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Irrigation
Irrigation
from Wikipedia
Irrigation of agricultural fields in Andalusia, Spain. Irrigation canal on the left.

Irrigation is the practice of applying controlled amounts of water to land to help grow crops, landscape plants, and lawns. Irrigation has been a key aspect of agriculture for over 5,000 years and has been developed by many cultures around the world. Irrigation helps to grow crops, maintain landscapes, and revegetate disturbed soils in dry areas and during times of below-average rainfall. In addition to these uses, irrigation is also employed to protect crops from frost,[1] suppress weed growth in grain fields, and prevent soil consolidation. It is also used to cool livestock, reduce dust, dispose of sewage, and support mining operations. Drainage, which involves the removal of surface and sub-surface water from a given location, is often studied in conjunction with irrigation.

Several methods of irrigation differ in how water is supplied to plants. Surface irrigation, also known as gravity irrigation, is the oldest form of irrigation and has been in use for thousands of years. In sprinkler irrigation, water is piped to one or more central locations within the field and distributed by overhead high-pressure water devices. Micro-irrigation is a system that distributes water under low pressure through a piped network and applies it as a small discharge to each plant. Micro-irrigation uses less pressure and water-flow than sprinkler irrigation. Drip irrigation delivers water directly to the root zone of plants. Subirrigation has been used in field crops in areas with high water tables for many years. It involves artificially raising the water table to moisten the soil below the root zone of plants.

Irrigation water can come from groundwater (extracted from springs or by using wells), from surface water (withdrawn from rivers, lakes or reservoirs) or from non-conventional sources like treated wastewater, desalinated water, drainage water, or fog collection. Irrigation can be supplementary to rainfall, which is common in many parts of the world as rainfed agriculture, or it can be full irrigation, where crops rarely rely on any contribution from rainfall. Full irrigation is less common and only occurs in arid landscapes with very low rainfall or when crops are grown in semi-arid areas outside of rainy seasons.

The environmental effects of irrigation relate to the changes in quantity and quality of soil and water as a result of irrigation and the subsequent effects on natural and social conditions in river basins and downstream of an irrigation scheme. The effects stem from the altered hydrological conditions caused by the installation and operation of the irrigation scheme. Amongst some of these problems is depletion of underground aquifers through overdrafting. Soil can be over-irrigated due to poor distribution uniformity or management wastes water, chemicals, and may lead to water pollution. Over-irrigation can cause deep drainage from rising water tables that can lead to problems of irrigation salinity requiring watertable control by some form of subsurface land drainage.

Extent

[edit]
Share of agricultural land which is irrigated (2021)
Area equipped For irrigation by region

In 2000, the total fertile land was 2,788,000 km2 (689 million acres), and it was equipped with irrigation infrastructure worldwide. Roughly 68% of this area is in Asia, 17% in the Americas, 9% in Europe, 5% in Africa and 1% in Oceania. The largest contiguous areas of high irrigation density are found in Northern and Eastern India and Pakistan along the Ganges and Indus rivers; in the Hai He, Huang He and Yangtze basins in China; along the Nile river in Egypt and Sudan; and in the Mississippi-Missouri river basin, the Southern Great Plains, and in parts of California in the United States. Smaller irrigation areas are spread across almost all populated parts of the world.[2]

By 2012, the area of irrigated land had increased to an estimated total of 3,242,917 km2 (801 million acres), which is nearly the size of India.[3] The irrigation of 20% of farming land accounts for the production of 40% of food production.[4][5]

Global overview

[edit]

The scale of irrigation increased dramatically over the 20th century. In 1800, 8 million hectares globally were irrigated, in 1950, 94 million hectares, and in 1990, 235 million hectares. By 1990, 30% of the global food production came from irrigated land.[6] Irrigation techniques across the globe include canals redirecting surface water,[7][8] groundwater pumping, and diverting water from dams. National governments lead most irrigation schemes within their borders, but private investors[9] and other nations,[8] especially the United States,[10] China,[11] and European countries like the United Kingdom,[12] also fund and organize some schemes within other nations.

By 2021 the global land area equipped for irrigation reached 352 million ha, an increase of 22% from the 289 million ha of 2000 and more than twice the 1960s land area equipped for irrigation. The vast majority is located in Asia (70%), where irrigation was a key component of the green revolution; the Americas account for 16% and Europe for 8% of the world total. India (76 million ha) and China (75 million ha) have the largest equipped area for irrigation, far ahead of the United States of America (27 million ha). China and India also have the largest net gains in equipped area between 2000 and 2020 (+21 million ha for China and +15 million ha for India). All the regions saw increases in the area equipped for irrigation, with Africa growing the fastest (+29%), followed by Asia (+25%), Oceania (+24%), the Americas (+19%) and Europe (+2%).[13]

Irrigation enables the production of more crops, especially commodity crops in areas which otherwise could not support them. Countries frequently invested in irrigation to increase wheat, rice, or cotton production, often with the overarching goal of increasing self-sufficiency.[12]

Example values for crops

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Approximate values of seasonal crop water needs[14]
Crop Crop water needs mm / total growing period
Sugarcane 1500–2500
Banana 1200–2200
Citrus 900–1200
Potato 500–700
Tomato 400–800
Barley/oats/wheat 450–650
Cabbage 350–500
Onions 350–550
Pea 350–500

Water sources

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Groundwater and surface water

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Traditional irrigation channel in Switzerland, collecting water from the high Alps
Irrigation is underway by pump-enabled extraction directly from the Gumti, seen in the background, in Comilla, Bangladesh.
Grapes in Petrolina, Brazil only made possible in this semi arid area by drip irrigation

Irrigation water can come from groundwater (extracted from springs or by using wells), from surface water (withdrawn from rivers, lakes or reservoirs) or from non-conventional sources like treated wastewater, desalinated water, drainage water, or fog collection.

While floodwater harvesting belongs to the accepted irrigation methods, rainwater harvesting is usually not considered as a form of irrigation. Rainwater harvesting is the collection of runoff water from roofs or unused land and the concentration of this.

Treated or untreated wastewater

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Irrigation with recycled municipal wastewater can also serve to fertilize plants if it contains nutrients, such as nitrogen, phosphorus and potassium. There are benefits of using recycled water for irrigation, including the lower cost compared to some other sources and consistency of supply regardless of season, climatic conditions and associated water restrictions. When reclaimed water is used for irrigation in agriculture, the nutrient (nitrogen and phosphorus) content of the treated wastewater has the benefit of acting as a fertilizer.[15] This can make the reuse of excreta contained in sewage attractive.[16]

The irrigation water can be used in different ways on different crops, such as for food crops to be eaten raw or for crops which are intended for human consumption to be eaten raw or unprocessed. For processed food crops: crops which are intended for human consumption not to be eaten raw but after food processing (i.e. cooked, industrially processed).[17] It can also be used on crops which are not intended for human consumption (e.g. pastures, forage, fiber, ornamental, seed, forest and turf crops).[18]

In developing countries, agriculture is increasingly using untreated municipal wastewater for irrigation – often in an unsafe manner. Cities provide lucrative markets for fresh produce, so they are attractive to farmers. However, because agriculture has to compete for increasingly scarce water resources with industry and municipal users, there is often no alternative for farmers but to use water polluted with urban waste directly to water their crops.

There can be significant health hazards related to using untreated wastewater in agriculture. Municipal wastewater can contain a mixture of chemical and biological pollutants. In low-income countries, there are often high levels of pathogens from excreta. In emerging nations, where industrial development is outpacing environmental regulation, there are increasing risks from inorganic and organic chemicals. The World Health Organization developed guidelines for safe use of wastewater in 2006,[16] advocating a 'multiple-barrier' approach wastewater use, for example by encouraging farmers to adopt various risk-reducing behaviors. These include ceasing irrigation a few days before harvesting to allow pathogens to die off in the sunlight; applying water carefully so it does not contaminate leaves likely to be eaten raw; cleaning vegetables with disinfectant; or allowing fecal sludge used in farming to dry before being used as a human manure.[15]

Drawbacks or risks often mentioned include the content of potentially harmful substances such as bacteria, heavy metals, or organic pollutants (including pharmaceuticals, personal care products and pesticides). Irrigation with wastewater can have both positive and negative effects on soil and plants, depending on the composition of the wastewater and on the soil or plant characteristics.[19]

Other sources

[edit]

Irrigation water can also come from non-conventional sources like treated wastewater,[20] desalinated water, drainage water, or fog collection.

In countries where humid air sweeps through at night, water can be obtained by condensation onto cold surfaces. This is practiced in the vineyards at Lanzarote using stones to condense water. Fog collectors are also made of canvas or foil sheets. Using condensate from air conditioning units as a water source is also becoming more popular in large urban areas.

As of November 2019 a Glasgow-based startup has helped a farmer in Scotland to establish edible saltmarsh crops irrigated with sea water. An acre of previously marginal land has been put under cultivation to grow samphire, sea blite, and sea aster; these plants yield a higher profit than potatoes. The land is flood irrigated twice a day to simulate tidal flooding; the water is pumped from the sea using wind power. Additional benefits are soil remediation and carbon sequestration.[21][22]

Competition for water resources

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Until the 1960s, there were fewer than half the number of people on the planet as of 2024. People were not as wealthy as today, consumed fewer calories and ate less meat, so less water was needed to produce their food. They required a third of the volume of water humans presently take from rivers. Today, the competition for water resources is much more intense, because there are now more than seven billion people on the planet, increasing the likelihood of overconsumption of food produced by water-thirsty animal agriculture and intensive farming practices. This creates increasing competition for water from industry, urbanisation and biofuel crops. Farmers will have to strive to increase productivity to meet growing demands for food, while industry and cities find ways to use water more efficiently.[23]

Successful agriculture is dependent upon farmers having sufficient access to water. However, water scarcity is already a critical constraint to farming in many parts of the world.

Irrigation methods

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There are several methods of irrigation. They vary in how the water is supplied to the plants. The goal is to apply the water to the plants as uniformly as possible, so that each plant has the amount of water it needs, neither too much nor too little. Irrigation can also be understood whether it is supplementary to rainfall, as happens in many parts of the world, or whether it is 'full irrigation, whereby crops rarely depend on any contribution from rainfall. Full irrigation is less common and only happens in arid landscapes experiencing very low rainfall or when crops are grown in semi-arid areas outside of any rainy seasons.

Surface irrigation

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Basin flood irrigation of wheat

Surface irrigation, also known as gravity irrigation, is the oldest form of irrigation and has been in use for thousands of years. In surface (furrow, flood, or level basin) irrigation systems, water moves across the surface of agricultural lands to wet it and infiltrate into the soil. Water moves by following gravity or the slope of the land. Surface irrigation can be subdivided into furrow, border strip or basin irrigation. It is often called flood irrigation when the irrigation results in flooding or near flooding of the cultivated land. Historically, surface irrigation is the most common method of irrigating agricultural land across most parts of the world. The water application efficiency of surface irrigation is typically lower than other forms of irrigation, due in part to the lack of control of applied depths. Surface irrigation involves a significantly lower capital cost and energy requirement than pressurized irrigation systems. Hence, it is often the irrigation choice for developing nations, for low-value crops and for large fields. Where water levels from the irrigation source permit, the levels are controlled by dikes (levees), usually plugged by soil. This is often seen in terraced rice fields (rice paddies), where the method is used to flood or control the level of water in each distinct field. In some cases, the water is pumped or lifted by human or animal power to the level of the land.

Residential flood irrigation in Phoenix, Arizona, US

Surface irrigation is even used to water urban gardens in certain areas, for example, in and around Phoenix, Arizona. The irrigated area is surrounded by a berm and the water is delivered according to a schedule set by a local irrigation district.[24]

A special form of irrigation using surface water is spate irrigation, also called floodwater harvesting. In case of a flood (spate), water is diverted to normally dry river beds (wadis) using a network of dams, gates and channels and spread over large areas. The moisture stored in the soil will be used thereafter to grow crops. Spate irrigation areas are in particular located in semi-arid or arid, mountainous regions.

Micro-irrigation

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Drip irrigation – a dripper in action

Micro-irrigation, sometimes called localized irrigation, low volume irrigation, or trickle irrigation is a system where water is distributed under low pressure through a piped network, in a pre-determined pattern, and applied as a small discharge to each plant or adjacent to it. Traditional drip irrigation use individual emitters, subsurface drip irrigation (SDI), micro-spray or micro-sprinklers, and mini-bubbler irrigation all belong to this category of irrigation methods.[25]

Drip irrigation

[edit]
Drip irrigation layout and its parts

Drip irrigation, also known as microirrigation or trickle irrigation, functions as its name suggests. In this system, water is delivered at or near the root zone of plants, one drop at a time. This method can be the most water-efficient method of irrigation,[26] if managed properly; evaporation and runoff are minimized. The field water efficiency of drip irrigation is typically in the range of 80 to 90% when managed correctly.

In modern agriculture, drip irrigation is often combined with plastic mulch, further reducing evaporation, and is also the means of delivery of fertilizer. The process is known as fertigation.

Deep percolation, where water moves below the root zone, can occur if a drip system is operated for too long or if the delivery rate is too high. Drip irrigation methods range from very high-tech and computerized to low-tech and labour-intensive. Lower water pressures are usually needed than for most other types of systems, except for low-energy center pivot systems and surface irrigation systems, and the system can be designed for uniformity throughout a field or for precise water delivery to individual plants in a landscape containing a mix of plant species. Although it is difficult to regulate pressure on steep slopes, pressure compensating emitters are available, so the field does not have to be level. High-tech solutions involve precisely calibrated emitters located along lines of tubing that extend from a computerized set of valves.[27]

Sprinkler irrigation

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Crop sprinklers near Rio Vista, California, US
A traveling sprinkler at Millets Farm Centre, Oxfordshire, United Kingdom

In sprinkler or overhead irrigation, water is piped to one or more central locations within the field and distributed by overhead high-pressure sprinklers or guns. A system using sprinklers, sprays, or guns mounted overhead on permanently installed risers is often referred to as a solid-set irrigation system. Higher pressure sprinklers that rotate are called rotors and are driven by a ball drive, gear drive, or impact mechanism. Rotors can be designed to rotate in a full or partial circle. Guns are similar to rotors, except that they generally operate at very high pressures of 275 to 900 kPa (39.9 to 130.5 psi) and flows of 3 to 76 L/s (50 to 1200 US gal/min), usually with nozzle diameters in the range of 10 to 50 mm (0.39 to 1.97 in). Guns are used not only for irrigation, but also for industrial applications such as dust suppression and logging.

Sprinklers can also be mounted on moving platforms connected to the water source by a hose. Automatically moving wheeled systems known as traveling sprinklers may irrigate areas such as small farms, sports fields, parks, pastures, and cemeteries unattended. Most of these use a length of polyethylene tubing wound on a steel drum. As the tubing is wound on the drum powered by the irrigation water or a small gas engine, the sprinkler is pulled across the field. When the sprinkler arrives back at the reel the system shuts off. This type of system is known to most people as a "water reel" travelling irrigation sprinkler, and they are used extensively for dust suppression, irrigation, and land application of wastewater.

Other travellers use a flat rubber hose that is dragged along behind while the sprinkler platform is pulled by a cable.

Center pivot

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Center pivot irrigation is a form of sprinkler irrigation utilising several segments of pipe (usually galvanized steel or aluminium) joined and supported by trusses, mounted on wheeled towers with sprinklers positioned along its length. The system moves in a circular pattern and is fed with water from the pivot point at the center of the arc. These systems are found and used in all parts of the world and allow irrigation of all types of terrain. Newer systems have drop sprinkler heads.[28]

As of 2017 most center pivot systems have drops hanging from a U-shaped pipe attached at the top of the pipe with sprinkler heads that are positioned a few feet (at most) above the crop, thus limiting evaporative losses. Drops can also be used with drag hoses or bubblers that deposit the water directly on the ground between crops. Crops are often planted in a circle to conform to the center pivot. This type of system is known as LEPA (Low Energy Precision Application). Originally, most center pivots were water-powered. These were replaced by hydraulic systems (T-L Irrigation) and electric-motor-driven systems (Reinke, Valley, Zimmatic). Many modern pivots feature GPS devices.[29]

Irrigation by lateral move (side roll, wheel line, wheelmove)

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A series of pipes, each with a wheel of about 1.5 m diameter permanently affixed to its midpoint, and sprinklers along its length, are coupled together. Water is supplied at one end using a large hose. After sufficient irrigation has been applied to one strip of the field, the hose is removed, the water drained from the system, and the assembly rolled either by hand or with a purpose-built mechanism, so that the sprinklers are moved to a different position across the field. The hose is reconnected. The process is repeated in a pattern until the whole field has been irrigated.[30][31]

This system is less expensive to install than a center pivot, but much more labor-intensive to operate – it does not travel automatically across the field: it applies water in a stationary strip, must be drained, and then rolled to a new strip. Most systems use 100 or 130 mm (3.9 or 5.1 in) diameter aluminum pipe. The pipe doubles both as water transport and as an axle for rotating all the wheels. A drive system (often found near the centre of the wheel line) rotates the clamped-together pipe sections as a single axle, rolling the whole wheel line. Manual adjustment of individual wheel positions may be necessary if the system becomes misaligned.[30][31]

Wheel line systems are limited in the amount of water they can carry, and limited in the height of crops that can be irrigated. One useful feature of a lateral move system is that it consists of sections that can be easily disconnected, adapting to field shape as the line is moved. They are most often used for small, rectilinear, or oddly-shaped fields, hilly or mountainous regions, or in regions where labor is inexpensive.[30][31]

Subirrigation

[edit]

Subirrigation has been used for many years in field crops in areas with high water tables. It is a method of artificially raising the water table to allow the soil to be moistened from below the plants' root zone. Often those systems are located on permanent grasslands in lowlands or river valleys and combined with drainage infrastructure. A system of pumping stations, canals, weirs and gates allows it to increase or decrease the water level in a network of ditches and thereby control the water table.

Subirrigation is also used in the commercial greenhouse production, usually for potted plants. Water is delivered from below, absorbed by upwards, and the excess collected for recycling. Typically, a solution of water and nutrients floods a container or flows through a trough for a short period, 10–20 minutes, and is then pumped back into a holding tank for reuse. Sub-irrigation in greenhouses requires fairly sophisticated, expensive equipment and management. Advantages are water and nutrient conservation, and labor savings through reduced system maintenance and automation. It is similar in principle and action to subsurface basin irrigation.

Another type of subirrigation is the self-watering container, also known as a sub-irrigated planter. This consists of a planter suspended over a reservoir with some type of wicking material, such as a polyester rope. The water is drawn up the wick through capillary action.[32][33] A similar technique is the wicking bed; this too uses capillary action.

Efficiency

[edit]

Modern irrigation methods are efficient enough to supply the entire field uniformly with water, so that each plant has the amount of water it needs, neither too much nor too little.[34] Water use efficiency in the field can be determined as follows:

  • Field Water Efficiency (%) = (Water Transpired by Crop ÷ Water Applied to Field) x 100

Increased irrigation efficiency has a number of positive outcomes for the farmer, the community and the wider environment. Low application efficiency infers that the amount of water applied to the field is in excess of the crop or field requirements. Increasing the application efficiency means that the amount of crop produced per unit of water increases. Improved efficiency may be achieved by applying less water to an existing field or by using water more wisely, thereby achieving higher yields in the same area of land. In some parts of the world, farmers are charged for irrigation water, hence over-application has a direct financial cost to the farmer. Irrigation often requires pumping energy (either electricity or fossil fuel) to deliver water to the field or supply the correct operating pressure. Hence, increased efficiency will reduce both the water cost and energy cost per unit of agricultural production. A reduction of water use on one field may mean that the farmer is able to irrigate a larger area of land, increasing total agricultural production. Low efficiency usually means that excess water is lost through seepage or runoff, both of which can result in loss of crop nutrients or pesticides with potential adverse impacts on the surrounding environment.

Improving the efficiency of irrigation is usually achieved in one of two ways: either by improving the system design or by optimizing the irrigation management. Improving system design includes conversion from one form of irrigation to another (e.g. from furrow to drip irrigation) and also through small changes in the current system (for example, changing flow rates and operating pressures). Irrigation management refers to the scheduling of irrigation events and decisions around how much water is applied.

Challenges

[edit]

Environmental impacts

[edit]
Within a long period of groundwater depletion in California's Central Valley, short periods of recovery have been mostly driven by extreme weather events that typically caused flooding and had negative social, environmental and economic consequences.[35]

Negative impacts frequently accompany extensive irrigation.[36] Some projects which diverted surface water for irrigation dried up the water sources, which led to a more extreme regional climate.[37] Projects that relied on groundwater and pumped too much from underground aquifers created subsidence and salinization. Salinization of irrigation water in turn damaged the crops and seeped into drinking water.[37] Pests and pathogens also thrived in the irrigation canals or ponds full of still water, which created regional outbreaks of diseases like malaria and schistosomiasis.[38][39][40] Governments also used irrigation schemes to encourage migration, especially of more desirable populations into an area.[41][42][43] Additionally, some of these large nationwide schemes failed to pay off at all, costing more than any benefit gained from increased crop yields.[44][45]

Overdrafting (depletion) of underground aquifers: In the mid-20th century, the advent of diesel and electric motors led to systems that could pump groundwater out of major aquifers faster than drainage basins could refill them. This can lead to permanent loss of aquifer capacity, decreased water quality, ground subsidence, and other problems. The future of food production in such areas as the North China Plain, the Punjab region in India and Pakistan, and the Great Plains of the US is threatened by this phenomenon.[46][47]

Technical challenges

[edit]
Overirrigation because of poor distribution uniformity in the furrows. Potato plants were oppressed and turned yellow

Irrigation schemes involve solving numerous engineering and economic problems while minimizing negative environmental consequences.[36] Such problems include:

  • Ground subsidence (e.g. New Orleans, Louisiana)
  • Underirrigation or irrigation giving only just enough water for the plant (e.g. in drip line irrigation) gives poor soil salinity control, which leads to increased soil salinity with consequent buildup of toxic salts on soil surface in areas with high evaporation. This requires either leaching to remove these salts and a method of drainage to carry the salts away. When using drip lines, the leaching is best done regularly at certain intervals (with only a slight excess of water), so that the salt is flushed back under the plant's roots.[48]
  • Overirrigation because of poor distribution uniformity or management wastes water, chemicals, and may lead to water pollution.[49]
  • Deep drainage (from over-irrigation) may result in rising water tables which in some instances will lead to problems of irrigation salinity requiring watertable control by some form of subsurface land drainage.[50][51] For example, in Australia, over-abstraction of fresh water for intensive irrigation activities has caused 33% of the land area to be at risk of salination.[52]
  • Drainage front instability, also known as viscous fingering, where an unstable drainage front results in a pattern of fingers and viscous entrapped saturated zones.
  • Irrigation with saline or high-sodium water may damage soil structure owing to the formation of alkaline soil.
  • Clogging of filters: algae can clog filters, drip installations, and nozzles. Chlorination, algaecide, UV and ultrasonic methods can be used for algae control in irrigation systems.
  • Complications in accurately measuring irrigation performance which changes over time and space using measures such as productivity, efficiency, equity and adequacy.[53]
  • Macro-irrigation, typical in intensive agriculture, where also are used agrochemicals, often causes eutrophication.

Social aspects

[edit]
  • Competition for surface water rights[54]
  • Assisting smallholders in sustainably and collectively managing irrigation technology and changes in technology.[55]

History

[edit]

Ancient history

[edit]
Animal-powered irrigation, Upper Egypt, ca. 1846

Archaeological investigation has found evidence of irrigation in areas lacking sufficient natural rainfall to support crops for rainfed agriculture. Some of the earliest known use of the technology dates to the 6th millennium BCE in Khuzistan in the south-west of Iran.[56][57] The site of Choga Mami, in present-day Iraq on the border with Iran, is believed to be the earliest to show the first canal irrigation in operation at about 6000 BCE.[58]

Irrigation was used as a means of manipulating water in the alluvial plains of the Indus valley civilization, the application of which is estimated to have begun around 4500 BCE and drastically increased the size and prosperity of their agricultural settlements.[59] The Indus Valley Civilization developed sophisticated irrigation and water-storage systems, including artificial reservoirs at Girnar dated to 3000 BCE, and an early canal irrigation system from c. 2600 BCE. Large-scale agriculture was practiced, with an extensive network of canals used for the purpose of irrigation.[59][60]

Farmers in the Mesopotamian plain used irrigation from at least the third-millennium BCE.[61] They developed perennial irrigation, regularly watering crops throughout the growing season by coaxing water through a matrix of small channels formed in the field.[62] Ancient Egyptians practiced basin irrigation using the flooding of the Nile to inundate land plots which had been surrounded by dikes. The flood water remained until the fertile sediment had settled before the engineers returned the surplus to the watercourse.[63] There is evidence of the ancient Egyptian pharaoh Amenemhet III in the twelfth dynasty (about 1800 BCE) using the natural lake of the Faiyum Oasis as a reservoir to store surpluses of water for use during dry seasons. The lake swelled annually from the flooding of the Nile.[64]

Young engineers restoring and developing the old Mughal irrigation system in 1847 during the reign of the Mughal Emperor Bahadur Shah II in Indian subcontinent

The Ancient Nubians developed a form of irrigation by using a waterwheel-like device called a sakia. Irrigation began in Nubia between the third and second millennia BCE.[65] It largely depended upon the flood waters that would flow through the Nile River and other rivers in what is now the Sudan.[66]

In sub-Saharan Africa, irrigation reached the Niger River region cultures and civilizations by the first or second millennium BCE and was based on wet-season flooding and water harvesting.[67][68]

Evidence of terrace irrigation occurs in pre-Columbian America, early Syria, India, and China.[63] In the Zana Valley of the Andes Mountains in Peru, archaeologists have found remains of three irrigation canals radiocarbon-dated from the 4th millennium BCE, the 3rd millennium BCE and the 9th century CE. These canals provide the earliest record of irrigation in the New World. Traces of a canal possibly dating from the 5th millennium BCE were found under the 4th-millennium canal.[69]

Ancient Persia (modern-day Iran) used irrigation as far back as the 6th millennium BCE to grow barley in areas with insufficient natural rainfall.[70][56] The Qanats, developed in ancient Persia about 800 BCE, are among the oldest known irrigation methods still in use today. They are now found in Asia, the Middle East, and North Africa. The system comprises a network of vertical wells and gently sloping tunnels driven into the sides of cliffs and steep hills to tap groundwater.[71] The noria, a water wheel with clay pots around the rim powered by the flow of the stream (or by animals where the water source was still), first came into use at about this time among Roman settlers in North Africa. By 150 BCE, the pots were fitted with valves to allow smoother filling as they were forced into the water.[72]

Sri Lanka

[edit]

The irrigation works of ancient Sri Lanka, the earliest dating from about 300 BCE in the reign of King Pandukabhaya, and under continuous development for the next thousand years, were one of the most complex irrigation systems of the ancient world. They included underground canals and artificial reservoirs to store water. These reservoirs and canal systems were used primarily to irrigate paddy fields, which require a lot of water to cultivate. Most of these irrigation systems still exist undamaged up to now, in Anuradhapura and Polonnaruwa, because of the advanced and precise engineering. The system was extensively restored and further extended during the reign of King Parakrama Bahu (1153–1186 CE).[73]

China

[edit]
Inside a karez tunnel at Turpan, Xinjiang, China

The oldest known hydraulic engineers of China were Sunshu Ao (6th century BCE) of the Spring and Autumn period and Ximen Bao (5th century BCE) of the Warring States period, both of whom worked on large irrigation projects. In the Sichuan region belonging to the state of Qin of ancient China, the Dujiangyan Irrigation System devised by the Qin Chinese hydrologist and irrigation engineer Li Bing was built in 256 BCE to irrigate a vast area of farmland that today still supplies water.[74] By the 2nd century CE, during the Han dynasty, the Chinese also used chain pumps which lifted water from a lower elevation to a higher one.[75] These were powered by manual foot-pedal, hydraulic waterwheels, or rotating mechanical wheels pulled by oxen.[76] The water was used for public works, providing water for urban residential quarters and palace gardens, but mostly for irrigation of farmland canals and channels in the fields.[77]

Korea

[edit]

Korea, Chang Yŏngsil, also known as Jang Yeong-sil, a Korean engineer of the Joseon dynasty, under the active direction of the king, Sejong the Great, invented the world's first rain gauge, uryanggye (Korean우량계) in 1441. It was installed in irrigation tanks as part of a nationwide system to measure and collect rainfall for agricultural applications. Planners and farmers could better use the information gathered in the[which?] survey with this instrument.[78]

North America

[edit]
A Cheugugi at Jang Yeong-sil Science Garden in Busan

The earliest agricultural irrigation canal system known in the area of the present-day United States dates to between 1200 BCE and 800 BCE and was discovered by Desert Archaeology, Inc. in Marana, Arizona (adjacent to Tucson) in 2009.[79] The irrigation-canal system predates the Hohokam culture by two thousand years and belongs to an unidentified culture. In North America, the Hohokam were the only culture known to rely on irrigation canals to water their crops, and their irrigation systems supported the largest population in the Southwest by CE 1300. The Hohokam constructed various simple canals combined with weirs in their various agricultural pursuits. Between the 7th and 14th centuries, they built and maintained extensive irrigation networks along the lower Salt and middle Gila Rivers that rivaled the complexity of those used in the ancient Near East, Egypt, and China. These were constructed using relatively simple excavation tools, without the benefit of advanced engineering technologies, and achieved drops of a few feet per mile, balancing erosion and siltation. The Hohokam cultivated cotton, tobacco, maize, beans, and squash varieties and harvested an assortment of wild plants. Late in the Hohokam Chronological Sequence, they used extensive dry-farming systems, primarily to grow agave for food and fiber. Their reliance on agricultural strategies based on canal irrigation, vital in their less-than-hospitable desert environment and arid climate, provided the basis for the aggregation of rural populations into stable urban centers.[80]

South America

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The oldest known irrigation canals in the Americas are in the desert of northern Peru in the Zaña Valley near the hamlet of Nanchoc. The canals have been radiocarbon dated to at least 3400 BCE and possibly as old as 4700 BCE. The canals at that time irrigated crops such as peanuts, squash, manioc, chenopods, a relative of Quinoa, and later maize.[69]

Modern history

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The scale of global irrigation increased dramatically over the 20th century. In 1800, 8 million hectares were irrigated; in 1950, 94 million hectares, and in 1990, 235 million hectares. By 1990, 30% of the global food production came from irrigated land.[6] Irrigation techniques across the globe included canals redirecting surface water,[7][8] groundwater pumping, and diverting water from dams. National governments led most irrigation schemes within their borders, but private investors[9] and other nations,[8] especially the United States,[10] China,[11] and European countries like the United Kingdom,[12] funded and organized some schemes within other nations. Irrigation enabled the production of more crops, especially commodity crops in areas that otherwise could not support them. Countries frequently invested in irrigation to increase wheat, rice, or cotton production, often with the overarching goal of increasing self-sufficiency.[12] In the 20th century, global anxiety, specifically about the American cotton monopoly, fueled many empirical irrigation projects: Britain began developing irrigation in India, the Ottomans in Egypt, the French in Algeria, the Portuguese in Angola, the Germans in Togo, and Soviets in Central Asia.[8]

Negative impacts frequently accompany extensive irrigation. Some projects that diverted surface water for irrigation dried up the water sources, which led to a more extreme regional climate.[37] Projects that relied on groundwater and pumped too much from underground aquifers created subsidence and salinization. Salinization of irrigation water damaged the crops and seeped into drinking water.[37] Pests and pathogens also thrived in the irrigation canals or ponds full of still water, which created regional outbreaks of diseases like malaria and schistosomiasis.[38][39][40] Governments also used irrigation schemes to encourage migration, especially of more desirable populations into an area.[41][42][43] Additionally, some of these large nationwide schemes failed to pay off at all, costing more than any benefit gained from increased crop yields.[44][45]

American West

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Irrigated land in the United States increased from 300,000 acres in 1880 to 4.1 million in 1890 to 7.3 million in 1900.[45] Two thirds of this irrigation sources from groundwater or small ponds and reservoirs, while the other one third comes from large dams.[81] One of the main attractions of irrigation in the West was its increased dependability compared to rainfall-watered agriculture in the East. Proponents argued that farmers with a dependable water supply could more easily get loans from bankers interested in this more predictable farming model.[82] Most irrigation in the Great Plains region derived from underground aquifers. Euro-American farmers who colonized the region in the 19th century tried to grow the commodity crops that they were used to, like wheat, corn, and alfalfa, but rainfall stifled their growing capacity. Between the late 1800s and the 1930s, farmers used wind-powered pumps to draw groundwater. These windpumps had limited power, but the development of gas-powered pumps in the mid-1930s pushed wells deep into the Ogallala Aquifer. Farmers irrigated fields by laying pipes across the field with sprinklers at intervals, a labor-intensive process, until the advent of the center-pivot sprinkler after World War II, which made irrigation significantly easier.[83] By the 1970s farmers drained the aquifer ten times faster than it could recharge, and by 1993 they had removed half of the accessible water.[84]

Large-scale federal funding and intervention pushed through the majority of irrigation projects in the West, especially in California, Colorado, Arizona, and Nevada. At first, plans to increase irrigated farmland, largely by giving land to farmers and asking them to find water, failed across the board. Congress passed the Desert Land Act in 1877 and the Carey Act in 1894, which only marginally increased irrigation.[85] Only in 1902 did Congress pass the National Reclamation Act, which channeled money from the sale of western public lands, in parcels up to 160 acres large, into irrigation projects on public or private land in the arid West.[86] The Congressmen who passed the law and their wealthy supporters supported Western irrigation because it would increase American exports, 'reclaim' the West, and push the Eastern poor out West for a better life.[87]

While the National Reclamation Act was the most successful piece of federal irrigation legislation, the implementation of the act did not go as planned. The Reclamation Service chose to push most of the Act's money toward construction rather than settlement, so the Service overwhelmingly prioritized building large dams like the Hoover Dam.[88] Over the 20th century, Congress and state governments grew more frustrated with the Reclamation Service and the irrigation schemes. Frederick Newell, head of the Reclamation Service, proving uncompromising and challenging to work with, falling crop prices, resistance to delay debt payments, and refusal to begin new projects until the completion of old ones all contributed.[89] The Reclamation Extension Act of 1914, transferring a significant amount of irrigation decision-making power regarding irrigation projects from the Reclamation Service to Congress, was in many ways a result of increasing political unpopularity of the Reclamation Service.[90]

In the lower Colorado Basin of Arizona, Colorado, and Nevada, the states derive irrigation water largely from rivers, especially the Colorado River, which irrigates more than 4.5 million acres of land, with a less significant amount coming from groundwater.[91] In the 1952 case Arizona v. California, Arizona sued California for increased access to the Colorado River, under the grounds that their groundwater supply could not sustain their almost entirely irrigation-based agricultural economy, which they won.[92] California, which began irrigating in earnest in the 1870s in San Joaquin Valley,[93] had passed the Wright Act of 1887 permitting agricultural communities to construct and operate needed irrigation works.[94] The Colorado River also irrigates large fields in California's Imperial Valley, fed by the National Reclamation Act-built All-American Canal.[95][96]

Soviet Central Asia

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When the Bolsheviks conquered Central Asia in 1917, the native Kazakhs, Uzbeks, and Turkmens used minimal irrigation. The Slavic immigrants pushed into the area by the Tsarist government[97] brought their irrigation methods, including waterwheels, the use of rice paddies to restore salted land, and underground irrigation channels. Russians dismissed these techniques as crude and inefficient. Despite this, tsarist officials maintained these systems through the late 19th century without other solutions.[98]

Before conquering the area, the Russian government accepted a 1911 American proposal to send hydraulic experts to Central Asia to investigate the potential for large-scale irrigation. A 1918 decree by Lenin then encouraged irrigation development in the region, which began in the 1930s. When it did, Stalin and other Soviet leaders prioritized large-scale, ambitious hydraulic projects, especially along the Volga River. The Soviet irrigation push stemmed mainly from their late 19th century fears of the American cotton monopoly and subsequent desire to achieve cotton self-sufficiency.[99] They had built up their textile manufacturing industry in the 19th century, requiring increased cotton and irrigation, as the region did not receive enough rainfall to support cotton farming.[98]

The Russians built dams on the Don and Kuban Rivers for irrigation, removing freshwater flow from the Sea of Azov and making it much saltier. Depletion and salinization scourged other areas of the Russian irrigation project. In the 1950s, Soviet officials began also diverting the Syr Darya and the Amu Darya, which fed the Aral Sea. Before diversion, the rivers delivered 55 cubic kilometres (13 cu mi) of water to the Aral Sea per year, but after, they only delivered 6 cubic kilometres (1.4 cu mi). Because of its reduced inflow, the Aral Sea covered less than half of its original seabed, which made the regional climate more extreme and created airborne salinization, lowering nearby crop yields.[100]

By 1975, the USSR used eight times as much water as they had in 1913, mostly for irrigation. Russia's expansion of irrigation began to decrease in the late 1980s, and irrigated hectares in Central Asia capped out at 7 million. Mikhail Gorbachev killed a proposed plan to reverse the Ob and Yenisei for irrigation in 1986, and the breakup of the USSR in 1991 ended Russian investment in Central Asian cotton irrigation.[101]

Africa

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Different irrigation schemes with various goals and success rates have been implemented across Africa in the 20th century but have all been influenced by colonial forces. The Tana River Irrigation Scheme in eastern Kenya, completed between 1948 and 1963, opened up new lands for agriculture. The Kenyan government attempted to resettle the area with detainees from the Mau Mau uprising.[102] Italian oil drillers discovered Libya's underground water resources during the Italian colonization of Libya. This water lay dormant until 1969, when Muammar al-Gaddafi and American Armand Hammer built the Great Man-Made River to deliver the Saharan water to the coast. The water largely contributed to irrigation but cost four to ten times more than the crops it produced were worth.[103]

In 1912, the Union of South Africa created an irrigation department and began investing in water storage infrastructure and irrigation. The government used irrigation and dam-building to further social goals like poverty relief by creating construction jobs for poor whites and irrigation schemes to increase white farming. One of their first significant irrigation projects was the Hartbeespoort Dam, begun in 1916 to elevate the living conditions of the 'poor whites' in the region and eventually completed as a 'whites only' employment opportunity.[104] The Pretoria irrigation scheme, Kammanassie project, and Buchuberg irrigation scheme on the Orange River all followed in the same vein in the 1920s and 30s.[42]

In Egypt, modern irrigation began with Muhammad Ali Pasha in the mid-1800s, who sought to achieve Egyptian independence from the Ottomans through increased trade with Europe—specifically cotton exportation.[105] His administration proposed replacing the traditional Nile basin irrigation, which took advantage of the annual ebb and flow of the Nile, with irrigation barrages in the lower Nile, which better suited cotton production. Egypt devoted 105,000 ha to cotton in 1861, which increased fivefold by 1865. Most of their exports were shipped to England, and the United States Civil War-induced cotton scarcity in the 1860s cemented Egypt as England's cotton producer.[106] As the Egyptian economy became more dependent on cotton in the 20th century, controlling even small Nile floods became more important. Cotton production was more at risk of destruction than more common crops like barley or wheat.[107] After the British occupation of Egypt in 1882, the British intensified the conversion to perennial irrigation with the construction of the Delta Barrage, the Assiut Barrage, and the first Aswan Dam. Perennial irrigation decreased local control over water and made traditional subsistence farming or the farming of other crops incredibly difficult, eventually contributing to widespread peasant bankruptcy and the 1879-1882 'Urabi revolt.[108]

Examples by country

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See also

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References

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Sources

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 This article incorporates text from a free content work. Licensed under CC BY-SA IGO 3.0 (license statement/permission). Text taken from World Food and Agriculture – Statistical Yearbook 2023​, FAO, FAO.

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from Grokipedia
Irrigation is the controlled application of to for the purpose of supplying moisture essential for plant growth, particularly in regions with inadequate rainfall or during dry seasons. This practice enables the cultivation of crops beyond natural precipitation limits, supporting higher yields and multiple harvests per year compared to . Originating around 6000 BCE in ancient Mesopotamia, where Sumerians constructed canals to divert water from the Tigris and Euphrates rivers, irrigation facilitated surplus food production that underpinned the rise of early urban civilizations. Similar systems emerged independently in ancient Egypt along the Nile, the Indus Valley, and China, demonstrating its foundational role in human agricultural advancement. In the contemporary era, irrigation equips approximately 343 million hectares of land worldwide as of , representing about 20% of global cultivated area yet accounting for roughly 40% of total food production due to enhanced . Common methods encompass , which uses to spread across fields and dominates globally; sprinkler irrigation, simulating rainfall through overhead distribution; and , which minimizes by delivering directly to . Despite these benefits, irrigation's intensive water use has precipitated , including depletion, salinization from salt accumulation in zones, and waterlogging, which degrade land productivity and necessitate careful management to avert long-term unsustainability.

Fundamentals

Definition and Principles

Irrigation constitutes the controlled application of water to soil or land surfaces to fulfill the water demands of crops, compensating for precipitation shortfalls that would otherwise limit growth. This process targets deficits in natural rainfall, particularly in arid, semi-arid, or seasonally variable climates, where insufficient moisture hinders plant development and yield potential. Unlike dependence on sporadic rain, irrigation delivers water via engineered systems to sustain hydrological balance, enabling cultivation on lands marginal for rain-fed agriculture by directly addressing evaporative losses and root-zone depletion. Core principles derive from agronomic and hydrological fundamentals, centering on evapotranspiration (ETc)—the combined from and by —as the primary measure of water need. ETc quantifies daily or seasonal losses, typically expressed in millimeters, and is computed as reference evapotranspiration (), based on meteorological variables like , , , and solar , multiplied by dimensionless coefficients (Kc) tailored to species, growth stage, and canopy cover. For instance, Kc values range from 0.15–1.2 across major like or , per standardized FAO methodologies, ensuring irrigation volumes align with empirical demands rather than approximations. Irrigation maintains within viable thresholds to avert physiological stress: above the permanent point (typically 25–50% depletion of available water, varying by ) but below saturation to prevent anaerobiosis and nutrient leaching. represents the upper limit post-gravitational drainage, holding 10–35% water by volume depending on clay or content, while allowable depletion guides scheduling to optimize access without excess. This causal intervention—replenishing vadose zone reserves—directly enhances photosynthetic rates, accumulation, and harvest indices in water-limited scenarios, distinct from passive wetting by rain.

Importance to Agriculture and Society

Irrigation sustains roughly 40% of global food production on approximately 20% of cropland, demonstrating its outsized role in enhancing agricultural output efficiency. This productivity stems from irrigated yields that exceed rainfed counterparts by 50% to 100%, especially for staples like rice and wheat where water availability directly limits growth in arid or semi-arid regions. Without irrigation, staple crop yields would decline by 50-70% in many key production areas, underscoring its causal necessity for maintaining food supplies amid variable rainfall. By enabling consistent harvests and surpluses, irrigation has historically underpinned population expansion and , transforming agrarian societies from subsistence to surplus-based economies capable of supporting non-agricultural labor. In modern contexts, it bolsters by mitigating risks, averting widespread famines that plagued pre-irrigation eras, and facilitating the agricultural revolutions that correlated with global from under 1 billion in 1800 to over 8 billion today. Economically, irrigation elevates GDP contributions from in developing nations, where it generates stable incomes for rural and expands in farming and related sectors. Studies attribute reductions to these effects, as higher outputs lower and increase household assets, with irrigation investments yielding returns through enhanced rural livelihoods and reduced vulnerability to variability. Furthermore, it supports by enabling "virtual water" exports embedded in irrigated commodities, sustaining global supply chains for food and fiber.

History

Ancient Origins

The earliest archaeological evidence of systematic irrigation dates to approximately 6000 BCE in the Fertile Crescent of Mesopotamia, where rudimentary channels diverted seasonal floodwaters from the Tigris and Euphrates rivers to fields, enabling controlled flooding for crop cultivation and silt deposition. Recent excavations in southern Mesopotamia have uncovered networks of over 200 canals dating to around 4000 BCE, oriented to harness tidal influences and river flows for agriculture, indicating early engineering to mitigate arid conditions and support barley and wheat yields exceeding rain-fed farming by factors of 2-3 times based on soil and sediment analysis. In the Nile Valley, basin irrigation emerged concurrently around 5000-6000 BCE, relying on the river's predictable annual inundation from July to November to flood enclosed fields, depositing nutrient-rich silt and allowing multi-crop cycles without mechanical pumping. Farmers constructed earthen dikes and basins to retain water for 2-3 months post-flood, yielding surpluses estimated at 5-10 times subsistence needs per hectare through emmer wheat and flax production, as inferred from predynastic settlement densities and tool assemblages. This method's simplicity—leveraging gravitational flow and natural cycles—facilitated population growth from villages to proto-urban centers by 4000 BCE. By 3000 BCE, the Indus Valley Civilization developed grid-planned canal systems at sites like and , channeling monsoon and river waters over distances up to 10 kilometers to irrigate , , and on alluvial plains, with evidence from sediment cores showing reduced flood variability through diversion structures. These innovations supported urban populations of 20,000-40,000 per city, enabling craft specialization as agricultural output stabilized at 1-2 tons per annually. In Sri Lanka's Dry Zone, reservoir-based systems appeared by the 3rd century BCE under King Pandukabhaya, with the Abhaya Wewa tank near Anuradhapura storing up to 80 million cubic meters for dry-season rice paddies via sluice gates and anicuts, sustaining yields that underpinned monastic and royal complexes. Across these regions, irrigation's causal role in surplus production—verified through comparative yield models and settlement hierarchies—fostered labor specialization, administrative hierarchies, and early states, as non-farmers comprised up to 20-30% of populations in irrigated cores versus near-zero in rain-dependent areas.

Major Historical Developments

One of the most enduring engineering achievements in ancient irrigation was the Dujiangyan system in China, constructed around 256 BCE during the Qin dynasty by local administrator Li Bing. This gravity-fed network diverted the Min River through a series of weirs, channels, and spillways, harnessing sediment deposition to maintain channel depth while distributing water across the Chengdu Plain without relying on dams that could silt up. The system simultaneously mitigated annual floods and supplied irrigation, enabling year-round cultivation of rice and other crops on expansive floodplains. By the early 21st century, it continued to irrigate approximately 5,300 square kilometers of farmland, demonstrating its scalability and long-term efficacy in boosting productivity through precise water control. In Persia, the development of qanats—horizontal underground aqueducts tapping aquifers via gently sloping tunnels—emerged around 1000 BCE, providing a low-evaporation method to convey over distances up to 50 kilometers to surface outlets for distribution. These structures, often exceeding 100 meters in depth at access shafts, minimized surface exposure in hyper-arid environments, sustaining oasis agriculture and urban centers by reliably accessing reserves without pumping. Qanats spread via and conquest to regions including the Islamic world, , and , where they irrigated date palms, grains, and orchards on marginal lands, fundamentally altering settlement patterns in water-scarce zones. Pre-Columbian North American societies, such as the culture in present-day , engineered extensive canal networks from around 300 CE, drawing from the Salt and Gila Rivers to irrigate maize, beans, and squash in the . These earthen channels, some reaching 15 meters wide and spanning hundreds of kilometers, incorporated gates and diversions for seasonal flood management, supporting population densities up to 10 times higher than non-irrigated areas through intensified dry-season farming. Similarly, in ancient Korea during the period (57 BCE–668 CE), state-directed irrigation expanded paddy fields via reservoirs and canalized streams, facilitating wet-rice cultivation that scaled agricultural output amid variable monsoons. In the Andes, the Inca Empire (c. 1438–1533 CE) constructed tiered terraces (andenes) coupled with aqueducts and canals to reclaim steep slopes, channeling snowmelt and rainfall while preventing erosion through stone retaining walls and integrated drainage. These systems created microclimates by capturing solar heat and moisture, permitting diverse crops like potatoes and quinoa across elevations from 2,000 to 4,000 meters, thereby expanding arable land in a rugged terrain prone to landslides and drought. Overall, such pre-modern innovations causally amplified cultivable acreage and yields—often by orders of magnitude in arid contexts—by engineering reliable water delivery, as evidenced by sustained demographic growth and surplus production in these civilizations.

Modern Expansion

The global extent of irrigated land expanded substantially during the , growing from approximately 50 million hectares in 1900 to around 270 million hectares by the early 2000s, driven primarily by state-sponsored projects that harnessed rivers for large-scale . This tripling in equipped area facilitated yield revolutions, particularly through reliable for staple and cash crops, enabling food production to keep pace with rapid in developing regions. In , the Reclamation Act of authorized federal funding for dams, reservoirs, and canals to irrigate arid lands, ultimately reclaiming over 10 million acres across multiple projects by mid-century. The , completed in 1936 as part of the Boulder Canyon Project, stored water to support irrigation for more than 2 million acres in downstream valleys, fostering high-value cash crops such as and boosting regional economic output through enhanced agricultural productivity. Soviet efforts in Central Asia during the 1950s and 1960s prioritized cotton monoculture via massive canal networks, expanding irrigated area in Uzbekistan by 33% from 1960 to 1985 and achieving annual fiber production of 2.2 to 2.5 million tons by the 1970s–1990s. While these systems induced salinization and waterlogging, reducing long-term soil fertility on some lands, the overall output surges provided net benefits by establishing the region as a key exporter and supporting industrial raw material needs. Post-independence dam constructions in developing nations amplified these trends; Egypt's Aswan High , filled by 1970, controlled floods and perennialized irrigation, doubling national food production through expanded cultivable area and multi-cropping. In , the Bhakra Nangal Dam complex, operational from 1963, irrigated 1.35 million acres in and neighboring states, driving a 1.7-fold rise in yields from 1963–1964 to 1968–1969 and underpinning the Green Revolution's yield gains that sustained demographic expansion.

Water Sources

Surface and Groundwater

Surface water, primarily from rivers and lakes, constitutes the dominant source for irrigation, accounting for approximately 75% of global irrigation water use. Diversion structures such as , weirs, and canals extract water by altering flow dynamics, relying on and channel gradients to transport it to fields without excessive energy input. Major river basins exemplify this: the Basin diverts water to irrigate about 5.5 million acres of farmland, with consuming 56-80% of the basin's allocated flow, often exceeding natural replenishment during dry periods due to upstream storage in reservoirs like . Similarly, the River supports extensive basin irrigation in and , where annual diversions harness seasonal floods and regulated releases from the High Dam to irrigate over 3 million hectares, constrained by the river's mean flow of about 84 km³ per year minus evaporation losses. Global surface water withdrawals for irrigation contribute to roughly 2,000 km³ annually, part of total agricultural withdrawals nearing 2,700 km³, with sustainability hinging on basin inflows that vary with and upstream demands. Groundwater, sourced from aquifers via wells and pumps, supplies the remaining 25% of irrigation water worldwide, extracted through mechanical lifting that overcomes hydrostatic pressure via centrifugal or submersible pumps, creating drawdown cones that can induce lateral flow from adjacent areas. Aquifers like the Ogallala in the U.S. , spanning eight states, have seen saturated volumes decline by an estimated 9-30% since 1950 due to pumping rates exceeding average recharge of 21 mm per year, though wetter cycles partially offset losses in northern portions with higher infiltration. Pumping lowers water tables, increasing energy costs proportional to lift depth per analogs, and risks salinization or if overexploited beyond recharge from , typically 1-5% of storage volume annually in semi-arid regions. Global abstraction for irrigation totals around 650 km³ per year, with dominating 80-90% of use, underscoring limits where extraction surpasses natural replenishment rates derived from isotopic tracing and hydrogeologic models. Competition between surface and groundwater intensifies in conjunctive use systems, where river depletions from over-diversion prompt compensatory pumping, amplifying depletion risks; empirical metrics from UN assessments indicate total irrigation withdrawals strain renewable yields, with 40% of global cropland in water-scarce basins facing deficits when flows or recharge fall below 1,000 m³ annually. Balanced management requires monitoring extraction against recharge, as physics dictates unsustainable drawdown leads to irreversible storage loss in confined .

Alternative Sources

Treated , after advanced purification to remove pathogens and excess nutrients, serves as a viable non-potable source for irrigation, providing a nutrient-rich supplement that can reduce reliance on freshwater by urban effluents. In , approximately 90% of municipal undergoes treatment and primarily for agricultural purposes, enabling the irrigation of over 500 square kilometers of farmland and offsetting freshwater shortages in a . Economic analyses indicate that such yields net savings of $0.50 to $0.60 per cubic meter compared to discharging treated water into rivers, factoring in avoided treatment and costs while leveraging inherent fertilizers in the . Desalination, particularly reverse osmosis applied to seawater or brackish groundwater, expands irrigation supplies in coastal or saline-prone regions by converting otherwise unusable water into potable-quality resources suitable for agriculture. Saudi Arabia has scaled desalination capacity significantly since the 2010s, operating plants like Ras Al Khair that produce over 1 million cubic meters daily, with portions allocated to support irrigated agriculture amid groundwater depletion, though primary use remains municipal. Production costs have declined to $0.30–$0.40 per cubic meter in recent large-scale facilities, making it increasingly feasible for high-value crops where energy inputs are offset by reliable yields in water-scarce areas. Supplementary methods include , which captures rooftop or for storage and direct field application, and using mesh nets in hyper-arid coastal zones to condense atmospheric moisture. In Chile's , fog nets yield up to 5 liters per square meter daily during peak seasons, supporting small-scale irrigation of without ecological disruption when sited away from sensitive habitats. These alternatives collectively hold potential to augment global irrigation supplies by 10–20% in stressed basins, provided investments prioritize energy-efficient treatment and localized distribution to minimize transmission losses.

Water Rights and Allocation

Water rights regimes govern the allocation of water for irrigation, with two primary doctrines shaping systems in arid regions: riparian rights, predominant in the , and prior appropriation, dominant in the and . Riparian rights grant access to water proportional to land ownership adjacent to the source, emphasizing equitable sharing among users but often resulting in vague entitlements that discourage long-term investment in due to uncertainty over future availability. In contrast, prior appropriation assigns rights based on the principle of "first in time, first in right," where the earliest beneficial use establishes , and rights are quantified, transferable, and subject to forfeiture if not used, fostering clear property definitions that incentivize efficient utilization and market-based transfers to higher-value applications. Empirical analysis indicates that prior appropriation enhances economic outcomes in water-scarce environments by doubling irrigation infrastructure investment and increasing agricultural output value compared to riparian baselines, as voluntary adoption across 1.8 million square miles of the western U.S. demonstrated through county-level from to 1910. This promotes conservation by allowing holders to sell or lease entitlements, aligning incentives with signals rather than equal division, which can perpetuate under riparian sharing; for instance, transferable enable reallocation from low-productivity to high-yield uses, preserving overall supply while maximizing returns. In , a similar cap-and-trade in the Murray-Darling Basin, rooted in prior appropriation principles, has facilitated over AUD $13 billion in government buybacks for environmental flows while enabling private trades that respond to drought-induced , reducing overall extraction through voluntary upgrades. Chile's 1981 Water Code exemplifies market-oriented allocation, establishing tradable, perpetual water rights that have enabled transfers averaging 100-200 million cubic meters annually, reallocating supply from to urban and industrial sectors during shortages and yielding efficiency gains of up to 20-30% in traded volumes through reduced conveyance losses and optimized application. Conversely, regulatory approaches like flat-rate pricing distort incentives, as seen in where subsidized, uncapped electricity tariffs for pumps—often a fixed fee per horsepower—have driven overpumping, depleting aquifers at rates exceeding 15,000 rupees per hectare in social costs annually in arid northwest regions and necessitating repeated well deepening without curbing extraction. Such non-price mechanisms fail to internalize depletion costs, exacerbating compared to quantity-based that enforce via markets or seniority.

Irrigation Methods

Surface Methods

Surface irrigation methods distribute water across fields primarily through gravity flow, allowing it to spread over the surface and infiltrate by . These techniques rely on the natural of the land or prepared field gradients to advance water from an inlet point, minimizing energy inputs beyond initial conveyance. Common configurations include basin, furrow, and systems, which have been adapted for various crops and topographies since antiquity. Basin irrigation involves flooding enclosed level areas, often rectangular or square, bounded by low levees or dikes. Water enters through gates or siphons and fills the basin to a depth, promoting even infiltration suitable for crops like that tolerate . This method exploits hydrostatic pressure and soil for distribution, but requires precise land leveling to achieve uniformity; uneven surfaces lead to in low spots and dry patches elsewhere. Field application efficiencies typically range from 50% to 70%, with losses primarily from at the surface and deep beyond root zones. Furrow irrigation channels water into narrow, parallel ditches spaced between crop rows, advancing downslope via gravity while seeping laterally into the . It suits row crops such as , , and , where raised beds prevent direct wetting of foliage to reduce risk. Flow dynamics depend on inflow rate, furrow slope (ideally 0.2-0.5%), and ; sandy soils advance quickly but infiltrate deeply, yielding 40-60% due to tail-end runoff and breakthrough losses. Empirical studies show that longer furrows (up to 800 meters) can improve uniformity if managed with cutback flows, reducing excess application by runoff. Border irrigation, a variant for larger fields, uses long strips (borders) separated by earthen ridges on gently sloping land (0.1-0.3% grade). Water floods each strip sequentially, advancing as a sheet flow that infiltrates as it progresses. This method demands extensive land preparation for uniform slopes and soil tilth, achieving 60-80% efficiency on leveled fields through controlled inflow to minimize runoff. It predominates in wheat and forage production where broad uniformity suffices, though variations in infiltration rates across field lengths cause advance-phase losses of 20-40% via uneven wetting. Globally, surface methods encompass approximately 90% of irrigated acreage, reflecting their simplicity and low capital requirements despite inherent inefficiencies from gravitational nonuniformity.

Pressurized Systems

Pressurized irrigation systems utilize pumps to elevate water pressure within distribution networks, facilitating delivery through overhead sprinklers or low-volume emitters for targeted crop wetting. This approach decouples application from gravitational flow, permitting uniform distribution on varied terrains and reducing dependency on field leveling. Operating pressures typically range from 20-70 psi for sprinklers and 8-30 psi for drip systems, with dynamic pressure management via regulators ensuring consistent emitter performance despite friction losses in pipes. Overhead sprinkler systems, a primary category of pressurized methods, disperse water via nozzles mimicking rainfall to cover large areas. Center-pivot variants, rotating around a fixed central pivot, irrigate circular fields up to 500 meters in radius and account for approximately 18 million hectares worldwide. Invented by Frank Zybach and patented in 1952, these systems transformed agriculture in the U.S. starting in the , converting marginal dryland into productive cropland for monocultures like corn and soybeans by accessing groundwater, thereby boosting regional yields through reliable moisture supply. Lateral-move systems complement pivots by traversing rectangular fields linearly, achieving up to 98% coverage via self-propelled spans fed by ditches or hoses, ideal for non-circular layouts. Sprinkler efficiencies generally range from 70-85%, influenced by wind, evaporation, and droplet size, though they enable mechanized operation minimizing labor compared to surface methods. Drip and systems deliver water under low pressure directly to the zone via emitters spaced along tubing, achieving application efficiencies exceeding 90% by curtailing and runoff. This precision fosters deeper penetration and optimal uptake, with field studies demonstrating yield increases of 20-50% in water-limited crops due to consistent . By confining wetting to plant bases, drip suppresses germination in inter-row spaces and curtails foliar diseases, as dry canopies inhibit proliferation like mildews and blights. surged post-1960s innovations in emitter technology, particularly in arid regions for high-value row crops.

Subsurface and Emerging Methods

Subsurface drip irrigation (SDI) delivers water directly to the crop root zone through buried emitters or tubing, typically placed 15-60 cm below the surface, minimizing surface exposure and associated losses. This method achieves water application efficiencies of up to 95% by substantially reducing from surfaces and limiting deep percolation beyond the root zone. SDI also curbs germination by keeping inter-row areas dry, potentially decreasing needs, and avoids foliar wetting to lower disease incidence from pathogens like those causing leaf blights. Automation compatibility further trims labor requirements, as systems can operate without manual field attendance for application. Subirrigation raises the through subsurface conduits such as perforated or ditches, enabling water to ascend via to plant roots in the unsaturated zone above. This approach suits flat or gently sloping terrains with impermeable subsoils that retain elevated water levels, as seen in regions like the U.S. Midwest where networks originally for drainage are repurposed for controlled management. By promoting uniform wetting from below, subirrigation enhances infiltration in heavy-textured soils prone to surface crusting, though it demands precise monitoring to prevent waterlogging and root oxygen deficits. responses vary by capillary conductivity, with benefits including sustained moisture availability during dry spells without surface disruption. Emerging subsurface techniques build on these principles with innovations like automated ebb-and-flow systems and mat integrations for finer control in high-value or controlled settings. mats, often paired with raised beds or benches, draw upward through fabric wicks to supply passively, conserving up to 30% more than overhead methods in trials by curbing evaporation and enabling precise drainage reuse. Hybrid approaches, such as optimized subsurface emitters with variable depth placement, target infiltration variability in heterogeneous soils, as demonstrated in recent modeling for upland crops showing yield stability under deficit conditions. These methods prioritize root-zone precision to boost uptake efficiency while mitigating buildup from uneven leaching.

Efficiency and Technology

Measurement and Improvement

Irrigation is quantified through metrics such as overall use , defined as in kilograms per cubic meter of applied (kg/m³), which integrates delivery, application, and crop utilization. Conveyance measures the proportion of diverted reaching the farm gate, typically ranging from 60-90% depending on canal conditions, with losses primarily from seepage and . Application assesses stored in the root zone versus applied, while distribution uniformity (DU) evaluates evenness of application, calculated as DU = (average depth in the lowest 25% of observations / average depth across all observations) × 100, with benchmarks above 85% considered optimal for minimizing over- and under-irrigation. Global average irrigation efficiency stands at approximately 55%, with national figures between 40% and 65% when measured as water relative to total withdrawals, though surface systems often achieve only 30-70%. Conveyance losses can exceed 30% in unlined earthen canals due to seepage, which is mitigated by lining with materials like or clay, reducing losses by 75-80% in suitable soils. Basic optimizations, such as compacting canal beds or applying geomembranes, can elevate overall to 80% by curbing non-beneficial losses without advanced technology. Improvements in scheduling enhance uniformity by aligning applications with deficits, using tensiometers to measure matric potential in centibars, triggering irrigation when readings reach crop-specific thresholds like 20-40 cb for many to prevent stress while avoiding excess. Field evaluations of DU involve placing catch cans during a representative run and analyzing depth variations, guiding adjustments like leveling fields or modifying flow rates to exceed 80% uniformity, thereby optimizing water retention in the root zone. These metrics and interventions focus on empirical benchmarks rather than theoretical maxima, as higher uniformity correlates directly with reduced deep and runoff.

Precision and Smart Irrigation

Precision irrigation systems utilize sensor networks and data analytics to apply water variably across fields, matching application rates to spatially variable crop water demands derived from real-time environmental and soil conditions. These technologies form closed-loop feedback mechanisms, where inputs from on-site sensors adjust irrigation delivery dynamically, often through automated controllers linked to pressurized distribution networks like center pivots or drip lines. Core components include soil moisture probes, such as capacitive sensors that measure volumetric water content in the root zone, weather stations tracking parameters like temperature, humidity, and wind speed, and evapotranspiration (ET) models that estimate crop water loss based on reference ET adjusted for crop coefficients. Integration of geographic information systems (GIS) and global positioning systems (GPS) enables variable rate irrigation (VRI), allowing sectional control of water output within a single system. For instance, in center pivot setups, GPS-equipped towers position the system to follow prescription maps generated from , which delineate zones of differing variability or stress; this permits reduced application in uniformly moist areas while targeting deficits elsewhere. Field evaluations of such VRI implementations have demonstrated targeted water reductions without yield penalties, as application aligns closely with measured deficits from proximal sensors or indices like (NDVI). Empirical trials report water use efficiencies improving by 20-30% under smart irrigation regimes compared to uniform scheduling, attributable to avoidance of over-irrigation in heterogeneous fields and responsive adjustments to microclimatic shifts. These savings stem from causal mechanisms like precise ET-based scheduling, which replaces calendar-driven cycles with demand-responsive ones, thereby conserving energy for pumping and mitigating risks. in water-scarce regions, such as California's Central Valley, has shown compatibility with regulatory frameworks like the Sustainable Groundwater Management Act, where VRI supports compliance by optimizing extractions.

Global Extent

Irrigated Areas and Crop Examples

Approximately 329 million hectares of land were equipped for irrigation globally in 2015, representing about 20% of total cultivated land and enabling production on roughly 40% of the world's food supply despite occupying a minority of cropland. Asia dominates this extent, accounting for 68% or 222 million hectares, driven by intensive systems for densely populated regions. Projections indicate modest expansion, with the Food and Agriculture Organization estimating an increase of 32 million hectares in equipped area by 2050 to meet rising demand, though actual harvested irrigated land may grow faster due to improved utilization. Irrigation underpins staple crop production, particularly for rice and wheat, where water reliability is essential for high yields in variable climates. Irrigated lowland systems produce about 75% of global rice output from 93 million hectares, as rice's flooded paddy requirements make it predominantly dependent on controlled water supply rather than rainfall. For wheat, irrigated areas contribute approximately 36% of total production, with the remainder from rainfed systems that face greater yield volatility. These staples highlight irrigation's role in food security, as disruptions in irrigated systems could sharply reduce output given limited arable land alternatives. High-water-use crops further illustrate irrigation's specificity: and are largely reliant on it, with consuming substantial volumes—often the highest among crops—and requiring consistent for fiber quality in arid production zones like the U.S. Southwest and . Yield differentials underscore this dependency; irrigated achieves averages 22% higher than rainfed equivalents globally, while sees a 34% uplift from irrigation, with ratios reaching 2:1 in water-limited environments due to reduced stress and optimized growth cycles. Such gaps affirm irrigation's causal contribution to productivity, enabling cultivation beyond rainfed constraints.

Regional Variations

Asia accounts for approximately 68% of the world's equipped irrigation area, with and together irrigating over 130 million hectares primarily through extensive networks derived from major river systems. These methods, dominant in the region, have enabled intensive and production but suffer from high conveyance losses—often exceeding 40% in unlined canals—exacerbating in policy environments that prioritize expansion over maintenance. In the , comprising 17% of global irrigated land, mechanized systems like center-pivot sprinklers predominate and , covering millions of hectares for crops such as corn and soybeans with water application efficiencies up to 85%. This technological adoption reflects adaptive successes in large-scale farming, contrasting with smallholder basin irrigation in , where shared pivot systems in settlements like Brazil's Itamarati have boosted yields but face challenges from uneven investment. Africa and the Middle East, with only 4-5% of global irrigated area despite acute aridity, rely heavily on groundwater pumping for over 60% of supplies, leading to rapid aquifer depletion rates—such as in the Arabian Peninsula—due to fragmented infrastructure and inadequate regulatory enforcement. Efficiency remains low, with application losses often above 50% from outdated wells and distribution networks, underscoring policy failures in coordinated development compared to more integrated continental approaches elsewhere.

Economic Impacts

Benefits and Productivity Gains

Irrigation substantially enhances crop yields for staple commodities, with econometric evidence from canal infrastructure expansions in India demonstrating persistent increases in agricultural productivity and population density in treated areas, countering concerns over long-term dependency by fostering sustained output growth. In semi-arid regions, irrigated wheat yields have been observed to rise by 22.8% under optimized single-application regimes compared to rainfed conditions, while potato outputs increased by 45% on average with supplemental water. Globally, such yield multipliers—often reaching 2 to 3 times for rice and maize in water-limited environments—enable irrigated croplands, which constitute about 20% of total arable area, to generate approximately 34% of world calorie production through higher per-hectare efficiency. These productivity gains translate into broader economic contributions, as evidenced by the U.S. irrigation equipment and services sector, which exerted a total annual impact of $23.3 billion in the early , encompassing $9 billion in direct spending and supporting in , installation, and maintenance. Irrigated farms in the U.S. accounted for over 50% of the total value of sales in 2022, underscoring irrigation's role in elevating output value despite comprising a minority of farmland. Econometric assessments of irrigation investments, such as canal rehabilitations in Argentina's vineyards, quantify yield equivalents of 144 kg per via enhanced vegetation indices, affirming positive returns that bolster rural economies. By stabilizing production against rainfall variability, irrigation offsets drought-induced losses, with studies projecting that each additional 100 mm of applied water reduces maize heat sensitivity by 7.6%, potentially countering 26% of yield declines anticipated by the 2050s under high-emissions scenarios. In drought-prone contexts like Rwanda's dry seasons, irrigated plots yield 90% more than non-irrigated counterparts, adding approximately $435 per hectare in value and enabling resilience without proportional land expansion. Such adaptations affirm irrigation's net positive trajectory in econometric models, where benefits from output stabilization outweigh critiques of resource lock-in through mid-century horizons.

Costs and Investment Returns

Capital costs for installing irrigation systems typically range from $1,000 to $5,000 per , depending on the , scale, and site-specific factors such as and water source. systems, for example, incur initial expenses of $500 to $1,200 per acre (approximately $1,235 to $2,965 per ), while center-pivot systems range from $1,100 to $2,100 per acre (about $2,720 to $5,190 per ). These upfront investments cover like , pumps, and emitters, with higher costs associated with pressurized systems requiring or fuel-powered pumps. Operational expenses primarily encompass for , labor for system management and maintenance, and repairs, which can account for a substantial portion of annual outlays. often represents the largest , varying by type—such as or —and water lift requirements; for instance, U.S. irrigation collectively consumed 60.6 terawatt-hours of in 2018, with comprising 37.5 terawatt-hours. Labor demands include monitoring distribution uniformity and addressing clogs or leaks, adding to ongoing costs that must be weighed against revenue from expanded cultivation. In regions with reliable water access and suitable soils, irrigation investments frequently demonstrate positive net present value (NPV) and internal rates of return exceeding discount rates, driven by private incentives to capture yield premiums from higher productivity. Payback periods typically span 3 to 5 years, as increased crop outputs—often 20-50% above rainfed baselines—offset capital and operational expenses, yielding return on investment rates around 20% in efficient setups. For example, analyses of center-pivot, low-pressure, and low-energy precision application systems in the Texas High Plains confirm profitability under NPV frameworks, assuming realistic crop prices and input costs. Market-based water pricing further enhances returns by signaling scarcity, encouraging adoption only where marginal benefits exceed costs, though subsidies can sometimes distort these incentives by lowering effective prices.

Environmental Considerations

Positive Effects

Irrigation maintains levels that promote vegetative cover and systems, which bind particles and reduce rates relative to , where bare or intermittently wet soils are more vulnerable to wind and intense rainfall . Efficient methods such as further minimize , preventing nutrient-laden sediment loss and preserving integrity. Managed irrigated wetlands, including rice paddies, replicate natural aquatic habitats, supporting biodiversity by providing foraging grounds and refuge for wetland-dependent species. In California, rice fields sustain nearly 230 species of birds, mammals, fish, reptiles, and amphibians, with paddies serving as critical stopover sites for migratory shorebirds and waterfowl during non-growing seasons when fields retain floodwater. Irrigated systems enhance carbon sequestration in soils through elevated crop productivity and residue inputs, with a global meta-analysis of 1,680 observations showing an average 5.9% increase in soil organic carbon stocks compared to non-irrigated counterparts, particularly in surface layers where organic matter accumulates. This effect stems from sustained biomass production that exceeds decomposition rates under controlled water availability. By boosting water productivity—defined as per unit of consumed—irrigation enables higher agricultural output from limited resources, reducing pressure on unirrigated lands and allowing portions of sources to remain allocated to ecosystems. Field from optimized systems demonstrate improved water-holding capacity and resilience to precipitation variability, stabilizing local and mitigating drought-induced ecosystem stress.

Negative Impacts and Mitigation

Irrigation-induced soil salinization occurs when salts accumulate in the root zone due to evaporation of applied water, exacerbated by poor drainage and inefficient application methods that prevent adequate leaching. Globally, 20 to 50 percent of irrigated soils suffer from salinity issues, rendering them less productive for crops. Inefficient irrigation practices, such as flood methods, contribute by allowing salts to concentrate without sufficient percolation to flush them below the root zone, often worsened by inadequate subsurface drainage systems. Aquifer overdraft from excessive irrigation pumping depletes reserves, with approximately 20 percent of the world's experiencing overpumping, leading to falling water tables and increased energy costs for extraction. This depletion is particularly acute in regions like the High Plains in the United States, where irrigation accounts for a significant portion of withdrawals, causing long-term risks in affected basins. Policy incentives, such as subsidized electricity for pumps in parts of and , have driven overuse by making extraction artificially cheap, amplifying drawdown rates beyond natural recharge. Mitigation of salinization involves leaching salts through the application of 10-20 percent excess irrigation water to facilitate drainage, combined with improved subsurface systems to remove saline effluents. Switching to drip or technologies can reduce water application by 30-50 percent compared to traditional surface methods, minimizing salt buildup by targeting delivery and enhancing leaching efficiency during controlled applications. For depletion, adopting deficit irrigation and precision scheduling based on sensors curbs , while reforming subsidies to reflect true costs encourages conservation without inherent reliance on blanket restrictions, as evidenced by sustainable irrigation in well-managed basins where recharge matches withdrawals.

Challenges and Controversies

Technical and Operational Issues

Clogging of emitters and laterals represents a primary technical challenge in s, often resulting from , biological growth, or chemical precipitates in source , which reduce flow rates and compromise . In drip systems, particles entering laterals can exacerbate , with severity depending on , concentration, and emitter discharge; field experiments indicate that particles larger than emitter orifices cause partial or total blockages, lowering distribution uniformity below 80% in affected zones. Pump failures frequently stem from such clogs, which impose hydraulic stress and lead to overheating or mechanical , as evidenced by operational showing premature pump degradation without adequate . Soil variability further hinders irrigation uniformity, particularly in surface and sprinkler applications, where differences in infiltration rates, hydraulic conductivity, and topography create uneven wetting patterns. Field studies on level basins demonstrate that spatial heterogeneity in soil properties can reduce application efficiency by 10-20%, necessitating adjustments in inflow rates or leveling to achieve distribution uniformity (DU) exceeding 85%. In sprinkler systems, pressure fluctuations and wind further amplify these effects, with evaluations revealing DU values dropping to 70% or lower on variable terrains without compensatory measures like variable-rate nozzles. Operationally, manual irrigation systems face labor-intensive demands, including frequent checks for leaks and adjustments, which are exacerbated by shortages in skilled personnel in rural areas, leading to inconsistent scheduling and higher failure rates. constitutes a significant portion of ongoing expenses, typically 5% of initial annually for repairs and upkeep, though this rises with poor or deferred servicing. Inadequate programmer configuration or valve malfunctions compound these issues, as gradual drops signal underlying problems like emitter blockages or pump wear. Solutions include deploying multi-stage filtration systems with screens and media filters to capture particulates, which field trials show can maintain emitter flows within 5% of specifications and extend life by reducing stress. Using robust materials such as UV-resistant polymers for laterals and corrosion-resistant alloys for mitigates degradation from chemical exposure, while flushing or chlorination addresses biological . Operator training programs, emphasizing monitoring and uniformity audits via catch-can tests, have demonstrated improvements in DU from 75% to over 90% in managed fields, underscoring the value of empirical protocols over reactive fixes. Regular seasonal inspections, including flow verification at multiple points, prevent downtime, with data indicating that proactive halves repair frequency in drip installations.

Policy and Subsidy Debates

Federal subsidies for irrigation in the United States, including crop insurance premium subsidies covering over 60% of premiums, have been shown to increase irrigation water withdrawals, with a 1% rise in subsidy rates leading to approximately 0.446% higher withdrawals, equivalent to about 475,901 acre-feet annually in analyzed western states. These programs, projected to involve billions in expenditures such as $2.1 billion in drought-related payments to California farmers alone from 2012 to 2020, distort resource allocation by providing artificially low water costs, encouraging expansion of irrigated acreage and higher consumption rather than conservation. Empirical studies indicate that even targeted conservation subsidies often fail to reduce overall water use, as farmers reallocate "saved" water to additional crops or less efficient practices, embodying the Jevons paradox where efficiency gains rebound into 10-30% higher total consumption in agricultural settings. Critics argue that such subsidies exemplify central planning failures, prioritizing political allocations over price signals and individual incentives, which systematically undervalue and exacerbate depletion in basins like the . In contrast, reforms emphasizing full-cost and secure property rights in entitlements have demonstrated superior outcomes; for instance, tiered structures in agricultural regions can enhance technical by incentivizing precise application without subsidizing overuse. Australia's Murray-Darling Basin provides evidence for market-oriented alternatives, where tradable water rights since the 1990s have enabled voluntary exchanges that reallocate water to higher-value uses, reducing waste through competitive pricing and cutting overall inefficiencies by improving allocation across irrigators. Trading volumes exceeding 2,000 gigaliters annually have facilitated environmental flows while sustaining agricultural output, underscoring how defined property rights and market mechanisms outperform subsidy-driven approaches in promoting causal efficiency without unintended expansions in use. Proponents of these reforms contend that they align individual decisions with resource constraints, avoiding the moral hazard of subsidized waste inherent in command-and-control policies.

Water Scarcity and Conflicts

Irrigation demands exacerbate in transboundary basins, where competing agricultural needs strain shared resources and spark allocation disputes. In the , encompassing 11 countries and supporting irrigation for over 300 million people, conflicts have persisted since colonial-era treaties favored downstream users. relies on the for 97% of its freshwater, with irrigation consuming 80% of that supply to sustain producing 95% of its food; upstream , contributing 85% of the river's flow via the , has pursued dams like the Grand Ethiopian Renaissance Dam (GERD), initiated in 2011, to expand its irrigated area from 1.4 million hectares in 2020 to projected 2.5 million by 2030, prompting Egyptian threats of military action during GERD reservoir filling phases in 2020 and 2021. These tensions, rooted in the 1959 Nile Waters Agreement allocating 55.5 billion cubic meters annually to and 18.5 billion to while excluding upstream states, highlight how ambiguous multilateral pacts fail to enforce shares amid rising demands. Globally, irrigation accounts for approximately 70% of freshwater withdrawals, contributing to high stress—defined as exceeding 40% of supply—in regions producing 60% of irrigated crops by weight, yet outright scarcity-driven wars remain rare, comprising fewer than 3% of historical interstate conflicts. Projections of acute global shortages by 2030, often cited in UN reports, frequently overlook technological mitigations like precision irrigation, which can reduce consumption by 30-50% through targeted delivery, and expansions, as seen in Israel's shift to 70% non-conventional sources by 2023, averting predicted crises. Empirical indicate that reallocation from inefficient uses, such as irrigation on low-value crops, could alleviate stress in 20-25% of high-pressure agricultural zones without expanding supply. Clear property rights frameworks have historically outperformed vague multilateral arrangements in resolving such disputes by enabling market-based transfers and judicial enforcement. In the arid western United States, the prior appropriation doctrine, formalized in the 1850s amid California's Gold Rush and codified in state laws by the 1880s, assigns rights based on beneficial first use and chronological priority, fostering efficient allocation via tradable entitlements; this system, upheld in U.S. Supreme Court rulings like Wyoming v. Colorado (1922), has mediated interstate claims over rivers like the Colorado without violence, contrasting with the basin's pre-doctrine riparian chaos. Transboundary conflicts arise largely from undefined rights, as property ambiguity incentivizes holdouts and overexploitation, whereas secure, transferable claims—evident in U.S. water markets transferring 1-2% of supply annually for billions in value—facilitate voluntary reallocations from agriculture to higher urban or environmental priorities, minimizing coercion. Stakeholder viewpoints underscore these dynamics: farmers assert rights to historically developed irrigation , yielding gains like doubling yields in stressed areas, against urban expansion claims and environmental advocates prioritizing instream flows for ecosystems, often resolved via compensated buyouts rather than top-down redistribution. In the case, upstream farmers in demand equitable shares for poverty alleviation, while downstream irrigators invoke prior uses under outdated pacts, illustrating how property clarity could preempt escalation over diplomacy's stalemates. Such reallocations, grounded in verifiable efficiencies, demonstrate scarcity's mitigability without sacrificing output, challenging alarmist narratives that undervalue institutional fixes.

Recent Developments

Technological Innovations

In the 2020s, irrigation technology has advanced through the integration of (AI), (IoT) sensors, and unmanned aerial vehicles (UAVs), enabling predictive and variable-rate watering based on . These systems analyze , weather forecasts, and crop needs to optimize application, reducing over-irrigation while maintaining yields. Field trials of AI-driven platforms have demonstrated water savings of 20-40% compared to conventional methods, with corresponding reductions in energy costs for pumping. UAVs equipped with multispectral cameras provide high-resolution monitoring of (NDVI) and soil conditions, allowing farmers to detect variability across fields and adjust irrigation zones dynamically. Since 2020, adoption of these drones has accelerated , with studies showing up to 40% water reduction through targeted application informed by aerial imagery and ground sensors. IoT networks complement this by transmitting data from in-soil probes for automated adjustments, minimizing human intervention and enabling scalability in large operations. Automation advancements include interfaces and retrofit kits for existing infrastructure, with 2025 product lines featuring app-based oversight, , and . These upgrades convert legacy pivot or drip systems into smart networks without full replacement, supporting variable-rate delivery via valves and flow sensors. The global smart irrigation market, encompassing these technologies, is projected to reach $2.14 billion in 2025, reflecting upscaling in precision methods amid rising input costs.

Policy and Sustainability Efforts

In 2024, the U.S. Department of Agriculture allocated up to $400 million to irrigation districts in drought-prone western states, enabling farmers to adopt water-conserving practices while maintaining production, as part of voluntary programs emphasizing market-based incentives over regulatory mandates. These efforts, including payments for fallowing fields or improving conveyance efficiency, conserved an estimated 250,000 acre-feet annually in the Colorado River Basin by compensating irrigators directly for reductions, demonstrating higher adoption rates compared to top-down restrictions that often face legal and operational resistance from agricultural stakeholders. Similarly, a 2023 agreement with California's Imperial Irrigation District secured 100,000 acre-feet of annual savings through compensated infrastructure upgrades, highlighting the efficacy of targeted financial incentives in arid basins where historical subsidies for high-water crops have exacerbated depletion. Digital governance trends in 2024 have advanced irrigation by integrating platforms for , with geographic information systems (GIS) and enabling associations to optimize distributions and reduce waste by up to 20% in pilot regions, prioritizing voluntary tech adoption driven by cost savings rather than enforced quotas. reforms in areas, such as those critiqued for inflating payouts—totaling $5.6 billion in 2023 across states—aim to redirect funds toward efficiency, though analyses indicate persistent overuse where payments fail to internalize full scarcity costs, underscoring inefficiencies in non-market interventions. Sustainability projections indicate that expanded irrigation, guided by return-on-investment (ROI) assessments, will yield net benefits across expanded U.S. croplands by , with economic gains from yield increases in corn and soybeans outweighing pumping and costs even under scenarios, as modeled in assessments of variability. Farmers adopting such ROI-focused practices report positive financial outcomes, contrasting with mandate-driven approaches that correlate with lower compliance due to disrupted operational autonomy. Debates in the 2024 Farm Bill centered on balancing farmer incentives—like enhanced conservation cost-sharing under the Environmental Quality Incentives Program—with proposals for stricter mandates on water use, where proponents of voluntary models argue they achieve greater long-term efficiency by aligning economic self-interest with resource limits, while critics of subsidies highlight their role in perpetuating over-extraction absent pricing reforms. Empirical data from basin-wide payments reveal voluntary reductions averaging 10-15% without yield collapse, versus historical mandate failures marked by evasion and litigation, suggesting market-oriented reforms better mitigate scarcity by mid-century projections.

References

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