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Gravity
Gravity
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The shapes of two massive galaxies in this image evolved under the effects of gravity.

In physics, gravity (from Latin gravitas 'weight'[1]), also known as gravitation or a gravitational interaction,[2] is a fundamental interaction, which may be described as the effect of a field that is generated by a gravitational source such as mass.

The gravitational attraction between clouds of primordial hydrogen and clumps of dark matter in the early universe caused the hydrogen gas to coalesce, eventually condensing and fusing to form stars. At larger scales this resulted in galaxies and clusters, so gravity is a primary driver for the large-scale structures in the universe. Gravity has an infinite range, although its effects become weaker as objects get farther away.

Gravity is described by the general theory of relativity, proposed by Albert Einstein in 1915, which describes gravity in terms of the curvature of spacetime, caused by the uneven distribution of mass. The most extreme example of this curvature of spacetime is a black hole, from which nothing—not even light—can escape once past the black hole's event horizon.[3] However, for most applications, gravity is sufficiently well approximated by Newton's law of universal gravitation, which describes gravity as an attractive force between any two bodies that is proportional to the product of their masses and inversely proportional to the square of the distance between them.

Scientists are looking for a theory that describes gravity in the framework of quantum mechanics (quantum gravity),[4] which would unify gravity and the other known fundamental interactions of physics in a single mathematical framework (a theory of everything).[5]

On the surface of a planetary body such as on Earth, this leads to gravitational acceleration of all objects towards the body, modified by the centrifugal effects arising from the rotation of the body.[6] In this context, gravity gives weight to physical objects and is essential to understanding the mechanisms that are responsible for surface water waves, lunar tides and substantially contributes to weather patterns. Gravitational weight also has many important biological functions, helping to guide the growth of plants through the process of gravitropism and influencing the circulation of fluids in multicellular organisms.

Characterization

[edit]

Gravity is the word used to describe a physical law, a fundamental physical interaction that derives primarily from mass, and the observed consequences of that interaction on objects. Gravity is the law that every object with mass attracts every other object in the universe in proportion to each mass and inversely proportional to the square of the distance between them. The force of gravity, F is written using the gravitational constant, G, as[7] for two masses, m, and m separated by a distance r.

Gravity is considered to be one of four fundamental interactions. The electromagnetic force law is similar to the force law for gravity: both depend upon the square of the inverse distance between objects in typical interactions. The ratio of gravitational attraction of two electrons to their electrical repulsion is 1 to 4.17×1042.[7] As a result, gravity can generally be neglected at the level of subatomic particles.[8] Gravity becomes the most significant interaction between objects at the scale of astronomical bodies, and it determines the motion of satellites, planets, stars, galaxies, and even light. Gravity is also fundamental in another sense: the inertial mass that appears in Newton's second law is the same as the gravitational mass. This equivalence principle is a scientific hypothesis that has been tested experimentally to more than one part in a trillion.[9]

History

[edit]

Ancient world

[edit]

The nature and mechanism of gravity were explored by a wide range of ancient scholars. In Greece, Aristotle believed that objects fell towards the Earth because the Earth was the center of the Universe and attracted all of the mass in the Universe towards it. He also thought that the speed of a falling object should increase with its weight, a conclusion that was later shown to be false.[10] While Aristotle's view was widely accepted throughout Ancient Greece, there were other thinkers such as Plutarch who correctly predicted that the attraction of gravity was not unique to the Earth.[11]

Although he did not understand gravity as a force, the ancient Greek philosopher Archimedes discovered the center of gravity of a triangle.[12] He postulated that if two equal weights did not have the same center of gravity, the center of gravity of the two weights together would be in the middle of the line that joins their centers of gravity.[13] Two centuries later, the Roman engineer and architect Vitruvius contended in his De architectura that gravity is not dependent on a substance's weight but rather on its "nature".[14] In the 6th century CE, the Byzantine Alexandrian scholar John Philoponus proposed the theory of impetus, which modifies Aristotle's theory that "continuation of motion depends on continued action of a force" by incorporating a causative force that diminishes over time.[15]

In 628 CE, the Indian mathematician and astronomer Brahmagupta proposed the idea that gravity is an attractive force that draws objects to the Earth and used the term gurutvākarṣaṇ to describe it.[16]: 105 [17][18]

In the ancient Middle East, gravity was a topic of fierce debate. The Persian intellectual Al-Biruni believed that the force of gravity was not unique to the Earth, and he correctly assumed that other heavenly bodies should exert a gravitational attraction as well.[19] In contrast, Al-Khazini held the same position as Aristotle that all matter in the Universe is attracted to the center of the Earth.[20]

The Leaning Tower of Pisa, where according to legend Galileo performed an experiment about the speed of falling objects

Scientific Revolution

[edit]

In the mid-16th century, various European scientists experimentally disproved the Aristotelian notion that heavier objects fall at a faster rate.[21] In particular, the Spanish Dominican priest Domingo de Soto wrote in 1551 that bodies in free fall uniformly accelerate.[21] De Soto may have been influenced by earlier experiments conducted by other Dominican priests in Italy, including those by Benedetto Varchi, Francesco Beato, Luca Ghini, and Giovan Bellaso which contradicted Aristotle's teachings on the fall of bodies.[21]

The mid-16th century Italian physicist Giambattista Benedetti published papers claiming that, due to specific gravity, objects made of the same material but with different masses would fall at the same speed.[22] With the 1586 Delft tower experiment, the Flemish physicist Simon Stevin observed that two cannonballs of differing sizes and weights fell at the same rate when dropped from a tower.[23]

In the late 16th century, Galileo Galilei's careful measurements of balls rolling down inclines allowed him to firmly establish that gravitational acceleration is the same for all objects.[24][25]: 334  Galileo postulated that air resistance is the reason that objects with a low density and high surface area fall more slowly in an atmosphere. In his 1638 work Two New Sciences, Galileo proved that the distance traveled by a falling object is proportional to the square of the time elapsed. His method was a form of graphical numerical integration since concepts of algebra and calculus were unknown at the time.[26]: 4  This was later confirmed by Italian scientists Jesuits Grimaldi and Riccioli between 1640 and 1650. They also calculated the magnitude of the Earth's gravity by measuring the oscillations of a pendulum.[27]

Galileo also broke with incorrect ideas of Aristotelian philosophy by regarding inertia as persistence of motion, not a tendency to come to rest. By considering that the laws of physics appear identical on a moving ship to those on land, Galileo developed the concepts of reference frame and the principle of relativity.[28]: 5  These concepts would become central to Newton's mechanics, only to be transformed in Einstein's theory of gravity, the general theory of relativity.[29]: 17 

In last quarter of the 16th century Tycho Brahe created accurate tools for astrometry, providing careful observations of the planets. His assistant and successor, Johannes Kepler analyzed these data into three empirical laws of planetary motion. These laws were central to the development of a theory of gravity a hundred years later.[30] In his 1609 book Astronomia nova Kepler described gravity as a mutual attraction, claiming that if the Earth and Moon were not held apart by some force they would come together. He recognized that mechanical forces cause action, creating a kind of celestial machine. On the other hand Kepler viewed the force of the Sun on the planets as magnetic and acting tangential to their orbits and he assumed with Aristotle that inertia meant objects tend to come to rest.[31][32]: 846 

In 1666, Giovanni Alfonso Borelli avoided the key problems that limited Kepler. By Borelli's time the concept of inertia had its modern meaning as the tendency of objects to remain in uniform motion and he viewed the Sun as just another heavenly body. Borelli developed the idea of mechanical equilibrium, a balance between inertia and gravity. Newton cited Borelli's influence on his theory.[32]: 848 

In 1657, Robert Hooke published his Micrographia, in which he hypothesized that the Moon must have its own gravity.[33]: 57  In a communication to the Royal Society in 1666 and his 1674 Gresham lecture, An Attempt to prove the Annual Motion of the Earth, Hooke took the important step of combining related hypothesis and then forming predictions based on the hypothesis.[34] He wrote:

I will explain a system of the world very different from any yet received. It is founded on the following positions. 1. That all the heavenly bodies have not only a gravitation of their parts to their own proper centre, but that they also mutually attract each other within their spheres of action. 2. That all bodies having a simple motion, will continue to move in a straight line, unless continually deflected from it by some extraneous force, causing them to describe a circle, an ellipse, or some other curve. 3. That this attraction is so much the greater as the bodies are nearer. As to the proportion in which those forces diminish by an increase of distance, I own I have not discovered it....[35][36]

Hooke was an important communicator who helped reformulate the scientific enterprise.[37] He was one of the first professional scientists and worked as the then-new Royal Society's curator of experiments for 40 years.[38] However his valuable insights remained hypotheses and some of these were incorrect.[39] He was unable develop a mathematical theory of gravity and work out the consequences.[32]: 853  For this he turned to Newton, writing him a letter in 1679, outlining a model of planetary motion in a void or vacuum due to attractive action at a distance. This letter likely turned Newton's thinking in a new direction leading to his revolutionary work on gravity.[37] When Newton reported his results in 1686, Hooke claimed the inverse square law portion was his "notion".

Newton's theory of gravitation

[edit]
English physicist and mathematician, Sir Isaac Newton (1642–1727)

Before 1684, scientists including Christopher Wren, Robert Hooke and Edmund Halley determined that Kepler's third law, relating to planetary orbital periods, would prove the inverse square law if the orbits were circles. However the orbits were known to be ellipses. At Halley's suggestion, Newton tackled the problem and was able to prove that ellipses also proved the inverse square relation from Kepler's observations.[29]: 13  In 1684, Isaac Newton sent a manuscript to Edmond Halley titled De motu corporum in gyrum ('On the motion of bodies in an orbit'), which provided a physical justification for Kepler's laws of planetary motion.[40] Halley was impressed by the manuscript and urged Newton to expand on it, and a few years later Newton published a groundbreaking book called Philosophiæ Naturalis Principia Mathematica (Mathematical Principles of Natural Philosophy).

The revolutionary aspect of Newton's theory of gravity was the unification of Earth-bound observations of acceleration with celestial mechanics.[41]: 4  In his book, Newton described gravitation as a universal force, and claimed that it operated on objects "according to the quantity of solid matter which they contain and propagates on all sides to immense distances always at the inverse square of the distances".[42]: 546  This formulation had two important parts. First was equating inertial mass and gravitational mass. Newton's 2nd law defines force via for inertial mass, his law of gravitational force uses the same mass. Newton did experiments with pendulums to verify this concept as best he could.[29]: 11 

The second aspect of Newton's formulation was the inverse square of distance. This aspect was not new: the astronomer Ismaël Bullialdus proposed it around 1640. Seeking proof, Newton made quantitative analysis around 1665, considering the period and distance of the Moon's orbit and considering the timing of objects falling on Earth. Newton did not publish these results at the time because he could not prove that the Earth's gravity acts as if all its mass were concentrated at its center. That proof took him twenty years.[29]: 13 

Newton's Principia was well received by the scientific community, and his law of gravitation quickly spread across the European world.[43] More than a century later, in 1821, his theory of gravitation rose to even greater prominence when it was used to predict the existence of Neptune. In that year, the French astronomer Alexis Bouvard used this theory to create a table modeling the orbit of Uranus, which was shown to differ significantly from the planet's actual trajectory. In order to explain this discrepancy, many astronomers speculated that there might be a large object beyond the orbit of Uranus which was disrupting its orbit. In 1846, the astronomers John Couch Adams and Urbain Le Verrier independently used Newton's law to predict Neptune's location in the night sky, and the planet was discovered there within a day.[44][45]

Newton's formulation was later condensed into the inverse-square law:where F is the force, m1 and m2 are the masses of the objects interacting, r is the distance between the centers of the masses and G is the gravitational constant 6.674×10−11 m3⋅kg−1⋅s−2.[46] While G is also called Newton's constant, Newton did not use this constant or formula, he only discussed proportionality. But this allowed him to come to an astounding conclusion we take for granted today: the gravity of the Earth on the Moon is the same as the gravity of the Earth on an apple:Using the values known at the time, Newton was able to verify this form of his law. The value of G was eventually measured by Henry Cavendish in 1797.[47]: 31 

Einstein's general relativity

[edit]

Eventually, astronomers noticed an eccentricity in the orbit of the planet Mercury which could not be explained by Newton's theory: the perihelion of the orbit was increasing by about 42.98 arcseconds per century. The most obvious explanation for this discrepancy was an as-yet-undiscovered celestial body, such as a planet orbiting the Sun even closer than Mercury, but all efforts to find such a body turned out to be fruitless. In 1915, Albert Einstein developed a theory of general relativity which was able to accurately model Mercury's orbit.[48]

Einstein's theory brought two other ideas with independent histories into the physical theories of gravity: the principle of relativity and non-Euclidean geometry.

The principle of relativity, introduced by Galileo and used as a foundational principle by Newton, led to a long and fruitless search for a luminiferous aether after Maxwell's equations demonstrated that light propagated at a fixed speed independent of reference frame. In Newton's mechanics, velocities add: a cannon ball shot from a moving ship would travel with a trajectory which included the motion of the ship. Since light speed was fixed, it was assumed to travel in a fixed, absolute medium. Many experiments sought to reveal this medium but failed and in 1905 Einstein's special relativity theory showed the aether was not needed. Special relativity proposed that mechanics be reformulated to use the Lorentz transformation already applicable to light rather than the Galilean transformation adopted by Newton. Special relativity, as in special case, specifically did not cover gravity.[29]: 4 

While relativity was associated with mechanics and thus gravity, the idea of altering geometry only joined the story of gravity once mechanics required the Lorentz transformations. Geometry was an ancient science that gradually broke free of Euclidean limitations when Carl Gauss discovered in the 1800s that surfaces in any number of dimensions could be characterized by a metric, a distance measurement along the shortest path between two points that reduces to Euclidean distance at infinitesimal separation. Gauss' student Bernhard Riemann developed this into a complete geometry by 1854. These geometries are locally flat but have global curvature.[29]: 4 

In 1907, Einstein took his first step by using special relativity to create a new form of the equivalence principle. The equivalence of inertial mass and gravitational mass was a known empirical law. The m in Newton's first law, , has the same value as the m in Newton's law of gravity on Earth, . In what he later described as "the happiest thought of my life" Einstein realized this meant that in free-fall, an accelerated coordinate system exists with no local gravitational field.[49] Every description of gravity in any other coordinate system must transform to give no field in the free-fall case, a powerful invariance constraint on all theories of gravity.[29]: 20 

Einstein's description of gravity was accepted by the majority of physicists for two reasons. First, by 1910 his special relativity was accepted in German physics and was spreading to other countries. Second, his theory explained experimental results like the perihelion of Mercury and the bending of light around the Sun better than Newton's theory.[50]

In 1919, the British astrophysicist Arthur Eddington was able to confirm the predicted deflection of light during that year's solar eclipse.[51][52] Eddington measured starlight deflections twice those predicted by Newtonian corpuscular theory, in accordance with the predictions of general relativity. Although Eddington's analysis was later disputed, this experiment made Einstein famous almost overnight and caused general relativity to become widely accepted in the scientific community.[53]

In 1959, American physicists Robert Pound and Glen Rebka performed an experiment in which they used gamma rays to confirm the prediction of gravitational time dilation. By sending the rays down a 74-foot tower and measuring their frequency at the bottom, the scientists confirmed that light is Doppler shifted as it moves towards a source of gravity. The observed shift also supports the idea that time runs more slowly in the presence of a gravitational field (many more wave crests pass in a given interval). If light moves outward from a strong source of gravity it will be observed with a redshift.[54] The time delay of light passing close to a massive object was first identified by Irwin I. Shapiro in 1964 in interplanetary spacecraft signals.[55]

In 1971, scientists discovered the first-ever black hole in the galaxy Cygnus. The black hole was detected because it was emitting bursts of x-rays as it consumed a smaller star, and it came to be known as Cygnus X-1.[56] This discovery confirmed yet another prediction of general relativity, because Einstein's equations implied that light could not escape from a sufficiently large and compact object.[57]

Frame dragging, the idea that a rotating massive object should twist spacetime around it, was confirmed by Gravity Probe B results in 2011.[58][59] In 2015, the LIGO observatory detected faint gravitational waves, the existence of which had been predicted by general relativity. Scientists believe that the waves emanated from a black hole merger that occurred 1.5 billion light-years away.[60]

On Earth

[edit]
An initially-stationary object that is allowed to fall freely under gravity drops a distance that is proportional to the square of the elapsed time. This image spans half a second and was captured at 20 flashes per second.

Every planetary body (including the Earth) is surrounded by its own gravitational field, which can be conceptualized with Newtonian physics as exerting an attractive force on all objects. Assuming a spherically symmetrical planet, the strength of this field at any given point above the surface is proportional to the planetary body's mass and inversely proportional to the square of the distance from the center of the body.

If an object with comparable mass to that of the Earth were to fall towards it, then the corresponding acceleration of the Earth would be observable.

The strength of the gravitational field is numerically equal to the acceleration of objects under its influence.[61] The rate of acceleration of falling objects near the Earth's surface varies very slightly depending on latitude, surface features such as mountains and ridges, and perhaps unusually high or low sub-surface densities.[62] For purposes of weights and measures, a standard gravity value is defined by the International Bureau of Weights and Measures, under the International System of Units (SI).

The force of gravity experienced by objects on Earth's surface is the vector sum of two forces:[6] (a) The gravitational attraction in accordance with Newton's universal law of gravitation, and (b) the centrifugal force, which results from the choice of an earthbound, rotating frame of reference. The force of gravity is weakest at the equator because of the centrifugal force caused by the Earth's rotation and because points on the equator are farthest from the center of the Earth. The force of gravity varies with latitude, and the resultant acceleration increases from about 9.780 m/s2 at the Equator to about 9.832 m/s2 at the poles.[63][64]

Gravity wave

[edit]

Waves on oceans, lakes, and other bodies of water occur when the gravitational equilibrium at the surface of the water is disturbed by for example wind.[65] Similar effects occur in the atmosphere where equilibrium is disturbed by thermal weather fronts or mountain ranges.[66]

Orbits

[edit]

Planets orbit the Sun in an ellipse as a consequence of the law of gravity. Similarly the Moon and artificial satellites orbit the Earth. Conceptually two objects in orbit are both falling off of the curve they would travel in if the force of gravity were not pulling them together. Since the force of gravity is universal, all planets attract each other with the most massive and closest pair have the most mutual affect. This means orbits are more complex than simple ellipses.[7]

Astrophysics

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Stars and black holes

[edit]

During star formation, gravitational attraction in a cloud of hydrogen gas competes with thermal gas pressure. As the gas density increases, the temperature rises, then the gas radiates energy, allowing additional gravitational condensation. If the mass of gas in the region is low, the process continues until a brown dwarf or gas-giant planet is produced. If more mass is available, the additional gravitational energy allows the central region to reach pressures sufficient for nuclear fusion, forming a star. In a star, again the gravitational attraction competes, with thermal and radiation pressure in hydrostatic equilibrium until the star's atomic fuel runs out. The next phase depends upon the total mass of the star. Very low mass stars slowly cool as white dwarf stars with a small core balancing gravitational attraction with electron degeneracy pressure. Stars with masses similar to the Sun go through a red giant phase before becoming white dwarf stars. Higher mass stars have complex core structures that burn helium and high atomic number elements ultimately producing an iron core. As their fuel runs out, these stars become unstable producing a supernova. The result can be a neutron star where gravitational attraction balances neutron degeneracy pressure or, for even higher masses, a black hole where gravity operates alone with such intensity that even light cannot escape.[67]: 121 

Gravitational radiation

[edit]
LIGO Hanford Observatory
The LIGO Hanford Observatory located in Washington (state), United States, where gravitational waves were first observed in September 2015

General relativity predicts that energy can be transported out of a system through gravitational radiation also known as gravitational waves. The first indirect evidence for gravitational radiation was through measurements of the Hulse–Taylor binary in 1973. This system consists of a pulsar and neutron star in orbit around one another. Its orbital period has decreased since its initial discovery due to a loss of energy, which is consistent for the amount of energy loss due to gravitational radiation. This research was awarded the Nobel Prize in Physics in 1993.[68]

The first direct evidence for gravitational radiation was measured on 14 September 2015 by the LIGO detectors. The gravitational waves emitted during the collision of two black holes 1.3 billion light years from Earth were measured.[69][70] This observation confirms the theoretical predictions of Einstein and others that such waves exist. It also opens the way for practical observation and understanding of the nature of gravity and events in the Universe including the Big Bang.[71] Neutron star and black hole formation also create detectable amounts of gravitational radiation.[72] This research was awarded the Nobel Prize in Physics in 2017.[73]

Dark matter

[edit]

At the cosmological scale, gravity is a dominant player. About 5/6 of the total mass in the universe consists of dark matter which interacts through gravity but not through electromagnetic interactions. The gravitation of clumps of dark matter known as dark matter halos attract hydrogen gas leading to stars and galaxies.[74]

Gravitational lensing

[edit]
Einstein's Cross, four images of the same distant quasar around a foreground galaxy due to gravitational lensing – a single quasar is actually hidden behind a massive foreground object (a galaxy in this case)

Gravity acts on light and matter equally, meaning that a sufficiently massive object could warp light around it and create a gravitational lens. This phenomenon was first confirmed by observation in 1979 using the 2.1 meter telescope at Kitt Peak National Observatory in Arizona, which saw two mirror images of the same quasar whose light had been bent around the galaxy YGKOW G1.[75][76] Many subsequent observations of gravitational lensing provide additional evidence for substantial amounts of dark matter around galaxies. Gravitational lenses do not focus like eyeglass lenses, but rather lead to annular shapes called Einstein rings.[47]: 370 

Speed of gravity

[edit]

In October 2017, the LIGO and Virgo interferometer detectors received gravitational wave signals 2 seconds before gamma ray satellites and optical telescopes seeing signals from the same direction, from a source about 130 million light-years away. This confirmed that the speed of gravitational waves was the same as the speed of light.[77]

Anomalies and discrepancies

[edit]

There are some observations that are not adequately accounted for, which may point to the need for better theories of gravity or perhaps be explained in other ways.

Rotation curve of a typical spiral galaxy: predicted (A) and observed (B). The discrepancy between the curves is attributed to dark matter.

Models

[edit]

The physical models of gravity, like all physical models, are expressed mathematically. Physicists use several different models, depending on the problem to be solved or for the purpose of gaining physical intuition.[84]: 44 

Newtonian action-at-a-distance

[edit]

Newton's inverse square law models gravity as a force F between two objects proportional to their mass, m: This gravitational force causes the objects to accelerate towards each other unless balanced by other forces. The force is "nonlocal": it depends on the mass of an object at a distance.[84]: 44  Scientists from Newton onwards recognized that this action at a distance does not explain the root cause of the force, but nevertheless the model explains a vast number of physical effects including cannon ball trajectories, tidal motion and planetary orbits.[84]: 4  However, combining the concept of relativity with gravity is enormously complex using this Newtonian model.[84]: 48 

Gravitational field

[edit]

A second equivalent approach to model gravity uses fields.[84]: 44  In physics, a field represents a physical phenomenon using a mathematical entity associated with each point in a space. Different field theories use different entities and concepts of space. For classical field theories of gravity, the entities can be vectors associated with points in a 3-dimensional space. Each vector gives the force experienced by an insignificantly small test mass at that point in space. The force vector at each point can be computed as the direction of the highest rate of change in the gravitational potential, a single number at each point in space. The three-dimensional map of the potential or of the gravitational field provides a visual representation of the effect of the gravitational effect of all surrounding objects.[dubiousdiscuss] Field models are local: the field values on a sphere completely determine the effects of gravity with the sphere.[84]: 45 

Fields are also used in general relativity, but rather than vectors over Euclidean space, the entities are tensors over spacetime. The Einstein field equations relate the 10 independent values in the tensors to the distribution of mass and energy in space.[dubiousdiscuss]

Action principles

[edit]

A third completely different way to derive a model of gravity is based on action principles. This formulation represents the effects of gravity on a system in a mathematically abstract way. The state of the system, for example the position and velocity of every particle, is expressed as a single mathematical entity. Each state has an associated energy property called the Lagrangian; the physically allowed changes to the state of the system minimize the value of this property. The path of the state is not a path in physical space, but rather in a high-dimensional state space: each point along the path corresponds to a different position and or velocity collectively for all particles in the system. This formulation does not express the forces or fields of the individual particles.[84]: 46  Modern theories of physics rely on these action principles.[85]: 396  The Einstein field equation for gravitation can be derived from the Einstein–Hilbert action.[85]: 388 

General relativity

[edit]

In modern physics, general relativity is considered the most successful theory of gravitation.[86] Physicists continue to work to find solutions to the Einstein field equations that form the basis of general relativity and continue to test the theory, finding excellent agreement in all cases.[87][88][89]: p.9 

Constraints

[edit]

Any theory of gravity must conform to the requirements of special relativity and experimental observations. Newton's theory of gravity assumes action at a distance and therefore cannot be reconciled with special relativity. The simplest generalization of Newton's approach would be a scalar field theory with the gravitational potential represented by a single number in a 4-dimensional spacetime. However, this type of theory fails to predict gravitational redshift or the deviation of light by matter and gives values for the precession of Mercury which are incorrect. A vector field theory predicts negative energy gravitational waves so it also fails. Furthermore, no theory without curvature in spacetime can be consistent with special relativity. The simplest theory consistent with special relativity and the well-studied observations is general relativity.[90]

General characteristics

[edit]

Unlike Newton's formula with one parameter, G, force in general relativity is terms of 10 numbers formed in to a metric tensor.[29]: 70 In general relativity the effects of gravitation are described in different ways in different frames of reference. In a free-falling or co-moving coordinate system, an object travels in a straight line. In other coordinate systems, the object accelerates and thus is seen to move under a force. The path in spacetime (not 3D space) taken by a free-falling object is called a geodesic and the length of that path as measured by time in the objects frame is the shortest (or rarely the longest) one. Consequently the effect of gravity can be described as curving spacetime. In a weak stationary gravitational field, general relativity reduces to Newton's equations. The corrections introduced by general relativity on Earth are on the order of 1 part in a billion.[29]: 77 

Einstein field equations

[edit]

The Einstein field equations are a system of 10 partial differential equations which describe how matter affects the curvature of spacetime. The system is may be expressed in the form where Gμν is the Einstein tensor, gμν is the metric tensor, Tμν is the stress–energy tensor, Λ is the cosmological constant, is the Newtonian constant of gravitation and is the speed of light.[91] The constant is referred to as the Einstein gravitational constant.[92]

Solutions

[edit]

The non-linear second-order Einstein field equations are extremely complex and have been solved in only a few special cases.[93] These cases however have been transformational in our understanding of the cosmos. Several solutions are the basis for understanding black holes and for our modern model of the evolution of the universe since the Big Bang.[41]: 227 

Tests of general relativity

[edit]
The 1919 total solar eclipse provided one of the first opportunities to test the predictions of general relativity.

Testing the predictions of general relativity has historically been difficult, because they are almost identical to the predictions of Newtonian gravity for small energies and masses.[94] A wide range of experiments provided support of general relativity.[89]: 1–9 [95][96][97][98] Today, Einstein's theory of relativity is used for all gravitational calculations where absolute precision is desired, although Newton's inverse-square law is accurate enough for virtually all ordinary calculations.[89]: 79 [99]

Gravity and quantum mechanics

[edit]

Despite its success in predicting the effects of gravity at large scales, general relativity is ultimately incompatible with quantum mechanics. This is because general relativity describes gravity as a smooth, continuous distortion of spacetime, while quantum mechanics holds that all forces arise from the exchange of discrete particles known as quanta. This contradiction is especially vexing to physicists because the other three fundamental forces (strong force, weak force and electromagnetism) were reconciled with a quantum framework decades ago.[100] As a result, researchers have begun to search for a theory that could unite both gravity and quantum mechanics under a more general framework.[101]

One path is to describe gravity in the framework of quantum field theory (QFT), which has been successful to accurately describe the other fundamental interactions. The electromagnetic force arises from an exchange of virtual photons, where the QFT description of gravity is that there is an exchange of virtual gravitons.[102][103] This description reproduces general relativity in the classical limit. However, this approach fails at short distances of the order of the Planck length,[104] where a more complete theory of quantum gravity (or a new approach to quantum mechanics) is required.

Alternative theories

[edit]

General relativity has withstood many tests over a large range of mass and size scales.[105][106] When applied to interpret astronomical observations, cosmological models based on general relativity introduce two components to the universe,[107] dark matter[108] and dark energy,[109] the nature of which is currently an unsolved problem in physics. The many successful, high precision predictions of the standard model of cosmology has led astrophysicists to conclude it and thus general relativity will be the basis for future progress.[110][111] However, dark matter is not supported by the Standard Model of particle physics, physical models for dark energy do not match cosmological data, and some cosmological observations are inconsistent.[111] These issues have led to the study of alternative theories of gravity.[112]

See also

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References

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Further reading

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Gravity is a in that causes mutual attraction between all objects with or , acting as the weakest of the four fundamental forces yet dominating large-scale structures in the . This force pulls objects toward each other, keeping planets in orbit around stars and governing the motion of celestial bodies over vast distances. In everyday experience on , gravity manifests as the downward pull that gives weight to objects and enables phenomena like and atmospheric retention. The classical understanding of gravity stems from Sir Isaac Newton's law of universal gravitation, formulated in 1687, which states that every particle attracts every other particle with a force directly proportional to the product of their masses and inversely proportional to the square of the between their centers. Mathematically expressed as F=Gm1m2r2F = G \frac{m_1 m_2}{r^2}, where GG is the approximately equal to 6.67430×1011m3kg1s26.67430 \times 10^{-11} \, \mathrm{m^3 kg^{-1} s^{-2}}, this law successfully explains planetary motion, , and the falling of objects, unifying terrestrial and . Newton's framework treats gravity as an instantaneous force acting at a , revolutionizing physics by providing a predictive applicable throughout the . In the early 20th century, Albert Einstein's theory of , published in 1915, redefined gravity not as a force but as the curvature of caused by mass and energy, with objects following paths in this warped geometry. This geometric interpretation predicts phenomena such as the bending of light around massive bodies, in gravitational fields, and the of Mercury's orbit, all confirmed through observations like the 1919 expedition. also implies the existence of —ripples in generated by accelerating masses, such as merging black holes—which were directly detected in 2015, validating the theory's predictions. Gravity's influence extends to cosmology, shaping the , the formation of galaxies, and the behavior of black holes, where curvature becomes extreme. Despite its success, reconciling with remains a major challenge in theoretical physics, driving research into theories like and . On , precise measurements of gravity aid in , resource exploration, and understanding climate dynamics, underscoring its practical significance.

Characterization

Definition and Fundamental Role

Gravity is one of the four fundamental interactions in nature, alongside , the strong , and the weak . It acts as an attractive between any two objects that possess or , with no repulsive counterpart observed in this interaction. In contrast to , which can be either attractive or repulsive depending on charges, gravity consistently draws masses toward each other. This force manifests in everyday phenomena, such as causing objects to fall toward Earth's surface, and on cosmic scales, it maintains the stability of planetary orbits around by counterbalancing centrifugal tendencies. Gravity also plays a pivotal role in shaping the large-scale structure of the , clumping matter into galaxies, clusters, and vast filaments through its cumulative pull on distributed masses. Gravity possesses an infinite range, extending across the without diminishment by distance in principle, though its effects weaken with separation. It is the weakest of the fundamental forces by many orders of magnitude, yet it dominates on astronomical scales because the other forces tend to cancel out—such as in neutral cosmic plasmas—while gravity accumulates additively over vast assemblies of matter. In daily life, the sensation of weight represents the gravitational attraction exerted by on an object's mass, pulling it downward toward the planet's center.

Strength and Universal Constant

The , denoted as GG, is a fundamental that quantifies the strength of the gravitational attraction between two masses in , F=Gm1m2r2F = G \frac{m_1 m_2}{r^2}, where it serves as the proportionality factor scaling the force inversely with the square of the distance rr between the masses m1m_1 and m2m_2. Its currently accepted value, as recommended by the Committee on Data for Science and Technology (CODATA) in 2022, is G=6.67430×1011m3kg1s2G = 6.67430 \times 10^{-11} \, \mathrm{m}^3 \mathrm{kg}^{-1} \mathrm{s}^{-2}, with a relative standard uncertainty of 22 parts per million. This value enables the calculation of gravitational forces across scales, from planetary orbits to galactic structures, by incorporating the masses involved. Gravity is the weakest of the four fundamental forces, approximately 103810^{38} times weaker than the strong when compared via their dimensionless constants at typical interaction scales. The strong , which binds quarks into protons and neutrons and holds atomic nuclei together, has a near 1, while gravity's effective is around 103910^{-39}, rendering it negligible in subatomic interactions. This disparity arises because gravity couples universally to mass-energy but with an exceedingly small constant, whereas the strong force operates over short ranges (about 101510^{-15} m) with immense intensity. The influence of gravity exhibits strong scale dependence: at atomic and subatomic levels, where particle masses are on the order of 102710^{-27} kg or less and distances are femtometers, the gravitational force between particles is overwhelmed by electromagnetic and nuclear forces, becoming effectively undetectable and thus having no noticeable effect on subatomic particles or processes. Conversely, at planetary and galactic scales, where masses aggregate to 102410^{24} kg or more and distances span kilometers to light-years, gravity dominates due to its infinite range and cumulative nature, dictating the motion of celestial bodies and the large-scale structure of the . This scale hierarchy explains why gravity shapes cosmic evolution while playing no role in chemical bonds or nuclear reactions. Measuring GG has historically posed significant challenges owing to the minuscule forces involved, requiring exquisite sensitivity to detect deflections on the order of microradians. The first successful determination came from Henry Cavendish's 1797–1798 torsion balance experiment, in which he suspended a light rod with small lead spheres (0.73 kg each) from a thin wire and observed its torsional oscillation induced by attraction to larger stationary lead spheres (158 kg each), placed alternately on opposite sides; by measuring the equilibrium deflection and wire's , Cavendish inferred the Earth's density, from which GG was later calculated as approximately 6.74×1011m3kg1s26.74 \times 10^{-11} \, \mathrm{m}^3 \mathrm{kg}^{-1} \mathrm{s}^{-2}. Modern measurements continue to rely on refined torsion balances, achieving precisions of 10–20 ppm by minimizing environmental noise through cryogenic cooling and vacuum isolation, though discrepancies among results persist at the 50 ppm level. Complementary approaches, such as , use laser-cooled atoms (e.g., cesium) in to detect phase shifts from gravitational gradients, yielding values like G=6.693×1011m3kg1s2G = 6.693 \times 10^{-11} \, \mathrm{m}^3 \mathrm{kg}^{-1} \mathrm{s}^{-2} with uncertainties around 0.5%, and offer potential for further improvements by suppressing systematic errors in quantum regimes. These efforts highlight ongoing refinements in isolating the pure Newtonian interaction.

Historical Development

Ancient and Pre-Scientific Views

In , particularly in the work of , the phenomenon now known as gravity was understood through the lens of natural motion and the four elements theory. posited that the universe consists of four sublunary elements—, , air, and fire—each with a specific natural place toward which it tends to move. Heavy elements like naturally move downward toward the center of the , their natural place, while light elements like air and fire move upward. This downward tendency of heavy bodies was not viewed as a universal attractive force but as an intrinsic property driven by the elements' natures, with motion ceasing once the natural place is reached. 's framework, detailed in works like Physics and , dominated Western thought for centuries, explaining everyday observations such as falling objects without invoking quantitative laws. Ancient observations of falling bodies and celestial motions further shaped these views, integrating them into geocentric models. Everyday experiences of objects dropping to the ground reinforced the idea of a natural downward pull limited to the sublunary realm, while heavenly bodies were seen as composed of a fifth element, ether, moving eternally in perfect circles around the Earth. Ptolemy's geocentric system, developed in the 2nd century CE in his Almagest, formalized these observations by placing Earth at the universe's center, with planets and stars affixed to nested crystalline spheres that rotated uniformly. Although Ptolemy focused on astronomical predictions rather than sublunary motion, his model upheld Aristotelian distinctions, treating celestial spheres as immune to the downward tendencies observed on Earth. Cultural perspectives beyond the Greco-Roman tradition offered parallel qualitative understandings. Similarly, Islamic scholars like elaborated on Aristotelian heaviness in his Kitab al-Shifa (), attributing the downward motion of heavy bodies to an inherent gravitational tendency while distinguishing it from celestial rotations driven by a separate motive force. Ibn Sina emphasized that this heaviness accelerates as bodies approach their natural place, influencing medieval Islamic . Medieval European developments began to refine these ideas through impetus theory and graphical representations. Jean Buridan (c. 1300–1361), a French philosopher, introduced the concept of impetus—an impressed motive force imparted to projectiles—to explain sustained motion without continuous external agents, challenging Aristotle's reliance on surrounding media like air. Buridan extended this to falling bodies, suggesting that gravity imparts successive increments of impetus, causing toward the natural place. Building on this, (c. 1320–1382) pioneered graphical methods in his Tractatus de configurationibus qualitatum et motuum, using coordinate-like diagrams to visualize motion intensities over time, such as plotting against duration to depict uniform as triangular areas. These innovations provided qualitative tools for analyzing motion, paving the way for later quantitative approaches. A central misconception in these pre-scientific views was that gravity represented a tendency solely toward a "natural place" rather than a universal force acting between all masses. This elemental and teleological perspective, rooted in , portrayed downward motion as purposeful and realm-specific, contrasting with the eventual recognition of it as an omnipresent attraction. Such ideas persisted until the transition to experimental methods in the late .

Newtonian Revolution

In 1687, Isaac Newton published Philosophiæ Naturalis Principia Mathematica, a seminal work that synthesized Johannes Kepler's empirical laws of planetary motion with Galileo's principle of inertia, establishing a unified framework for understanding both terrestrial and celestial mechanics. This synthesis demonstrated that the same physical laws govern the fall of objects on Earth and the orbits of planets around the Sun, marking a profound shift toward a mathematical description of nature. Newton's approach integrated these ideas through rigorous geometric proofs, resolving longstanding questions about motion under a single set of principles. A popular anecdote, first recounted by in 1727 based on accounts from Newton's niece, describes Newton observing an apple falling from a at around 1666, prompting him to ponder why it fell straight down rather than sideways or upward. This led to a comparing the apple's descent to the 's orbit: if the same force causing the apple to accelerate toward acted continuously on the , it could explain the curvature of its path around instead of a straight line into space. These reflections, developed during Newton's isolation due to the Great Plague, formed the conceptual foundation for his later formalization of gravitational attraction. Newton's theory of universal gravitation posited that every particle of in the attracts every other particle with proportional to their masses and inversely related to the square of the between them, providing a comprehensive explanation for diverse phenomena including ocean , the trajectories of comets, and the regular motions of . This principle unified disparate observations, showing as resulting from differential gravitational pulls of the and Sun on Earth's oceans, comets as bodies following elliptical orbits under solar attraction, and planetary paths as ellipses determined by the same inverse-square . The development of these ideas was influenced by contemporaries such as , who in 1679 suggested an for gravity in correspondence with Newton, and , whose 1684 query about planetary orbits spurred Newton to revisit his calculations. Priority disputes arose, particularly with Hooke, who claimed precedence for the inverse-square concept; Newton acknowledged Hooke's role in early drafts but minimized it in later editions amid acrimonious exchanges. Halley, however, played a pivotal supportive role by funding the Principia's publication and verifying its predictions. One immediate application of Newton's theory was Halley's prediction of comet returns using gravitational orbits; analyzing historical sightings, he calculated that the bright comet of 1682 would reappear around 1758, a forecast confirmed when the comet—now known as —was observed on December 25, 1758, validating the periodic nature of cometary motion under universal gravitation. This success, achieved posthumously for Halley, demonstrated the predictive power of Newton's framework and extended its reach beyond planets to transient celestial objects.

Relativistic and Modern Advances

By the late , Newtonian gravity encountered significant anomalies that highlighted its limitations. Astronomers observed an unexplained in Mercury's perihelion, amounting to approximately 43 arcseconds per century beyond what planetary perturbations could account for; this discrepancy was first quantified by in 1859 through analysis of historical observations. Concurrently, the prevailing view that light propagated through a stationary luminiferous ether—a hypothetical medium filling —faced null results from the Michelson-Morley experiment in , which sought to detect Earth's orbital motion relative to this ether but found no variation in light speed. These unresolved issues spurred theoretical innovations, culminating in Albert Einstein's presentation of in November 1915 to the , where he reconceptualized gravity as the curvature of four-dimensional induced by and . Early experimental validations bolstered general relativity's credibility. During the total solar eclipse of May 29, 1919, expeditions led by in and Andrew Crommelin in Sobral, Brazil, measured the apparent deflection of starlight passing near the Sun, confirming Einstein's predicted value of 1.75 arcseconds to within observational error. Decades later, the Pound-Rebka experiment at Harvard in 1959 provided direct evidence for by detecting a fractional frequency shift of about 2.5 × 10^{-15} in Mössbauer gamma rays traversing a 22.5-meter height in Earth's gravity, aligning with 's prediction to 10-15% precision. These tests, along with Mercury's now fully explained by relativistic effects, established as the superior framework over Newtonian mechanics. In the post-1950 era, transformed cosmology by underpinning models of an expanding universe, as Edwin Hubble's 1929 observations of galactic redshifts were interpreted through Friedmann-Lemaître-Robertson-Walker metrics derived from Einstein's equations, leading to the theory's widespread acceptance after the 1965 discovery of the by Arno Penzias and Robert Wilson. A landmark direct confirmation came on September 14, 2015, when the observatories detected —ripples in —from the merger of two black holes 1.3 billion light-years away, matching 's waveform predictions and opening multimessenger astronomy; this achievement earned the 2017 for , , and . Modern advances continue to probe general relativity's predictions at extreme scales. The Event Horizon Telescope collaboration released the first image of a black hole's shadow in the galaxy M87 on , , revealing a dark central region encircled by a luminous ring consistent with curvature around a 6.5-billion-solar-mass object, as forecasted by . This was followed by the May 2022 image of Sagittarius A*, the at the Milky Way's center with 4 million solar masses, further validating the theory's description of event horizons despite the target's rapid variability. In June 2023, the North American Nanohertz Observatory for Gravitational Waves (NANOGrav) reported evidence for a gravitational-wave background at nanohertz frequencies, detected via correlated timing residuals in signals from 67 pulsars over 15 years, likely arising from a cosmic population of binaries and affirming 's applicability to low-frequency regimes. More recent detections in late 2024 of twin black hole collisions further tested in highly dynamic environments, with waveforms aligning closely with theoretical predictions.

Effects on Earth

Surface Gravity and Measurement

Surface gravity on is the local manifestation of , denoted as g, which pulls objects toward the planet's center. The standard value adopted for sea-level conditions is g₀ = 9.80665 m/s², representing the conventional used in various scientific and standards. This value varies with latitude due to Earth's spheroidal shape and rotational effects; at the , g is approximately 9.78 m/s², while at the poles it reaches about 9.83 m/s², a difference of roughly 0.05 m/s² or 6 milligals (mgal). Early measurements of surface gravity relied on pendulum experiments, pioneered by in the 17th century. Huygens developed the cycloidal and used its period to derive a precise estimate of g at , achieving an accuracy of about 9.81 m/s² through the relation between length and . Modern gravimeters have advanced this precision significantly. Relative gravimeters, such as spring-based instruments, measure changes in g by detecting deflections in a suspended on a sensitive spring, offering portability for field surveys with resolutions down to 0.01 mgal. Absolute gravimeters, like falling-corner types, determine g directly by tracking the free fall of a corner-cube reflector using laser interferometry in a , providing standalone measurements accurate to 0.002 mgal over short drops of about 0.2 m. Local variations in surface gravity arise from several factors. Altitude affects g through the inverse-square law and reduced mass attraction; the free-air correction is approximately -0.3086 mgal per meter of elevation, leading to a decrease of about 0.03 m/s² at 10 km height. Earth's rotation introduces a centrifugal effect that reduces effective g most at the equator, where it subtracts up to 0.034 m/s² (about 0.3% of total g), directed outward perpendicular to the axis. Geological features cause anomalies from density contrasts; mountains exhibit negative Bouguer anomalies (e.g., -50 to -100 mgal over the Himalayas) due to low-density crustal roots, while ocean trenches show uncompensated negative free-air anomalies up to -9 mgal from mass deficits. In microgravity environments, where effective g approaches zero, biological systems experience profound changes. On the (ISS), astronauts encounter continuous , leading to fluid shifts causing facial puffiness and reduced leg volume, as well as accelerated bone loss (1-2% per month) and due to lack of load-bearing stress. simulations on Earth, such as parabolic flights or drop towers, replicate these conditions for short durations (20-30 seconds), enabling studies of cellular responses like altered protein expression and 3D tissue formation without interference. Gravity measurements play a key role in for resource exploration and hazard assessment. High-resolution maps subsurface density variations to delineate ore bodies, such as massive sulfides in mining districts, by identifying anomalies from 1-10 mgal associated with mineral deposits. In efforts, microgravity surveys detect precursory changes in crustal strain, with temporal variations of 10-100 μgal signaling potential fault movements before seismic events.
FactorApproximate Effect on gExample Location/Value
Latitude (Equator to Poles)+0.05 m/s²Equator: 9.78 m/s²; Poles: 9.83 m/s²
Altitude (per km)-0.003 m/s²10 km: ~0.03 m/s² decrease
Centrifugal (Equator)-0.034 m/s²Reduces effective g by 0.3%
Geological (Mountains)-50 to -100 mgalHimalayas: negative
Geological (Trenches)several mgal (free-air)Mariana Trench: -9 mgal uncompensated

Tidal Forces and Variations

Tidal forces arise from the differential gravitational attraction exerted by celestial bodies such as the Moon and Sun across the extent of Earth, leading to stretching and compression of the planet's oceans, crust, and atmosphere. Unlike the uniform gravitational pull that governs overall orbital motion, these forces create gradients that cause one side of Earth to experience stronger attraction than the opposite side, resulting in two opposing bulges. The Moon's proximity makes it the dominant contributor, producing tidal bulges on the near and far sides of Earth, with the oceans rising to form high tides at these locations twice daily as Earth rotates. The Sun contributes a smaller but significant effect, about 46% of the Moon's tidal influence, due to its greater mass offset by its distance. When the Moon and Sun align during new and full moons, their gravitational pulls reinforce to produce spring tides, characterized by higher high tides and lower low tides, increasing the by approximately 20%. Conversely, during first and third quarter moons, their pulls act at right angles, partially canceling to form neap tides with reduced range, also by about 20%. These cycles repeat twice per synodic of 29.53 days, influencing global ocean levels and coastal ecosystems. The mathematical basis for tidal acceleration stems from the variation in gravitational force over Earth's radius. While the direct gravitational attraction follows an inverse-square law, the differential tidal force—responsible for the bulges—varies inversely with the cube of the distance between the attracting body and Earth's center. This arises because the tidal effect is proportional to the gradient of the gravitational field, yielding an acceleration approximately given by Δg±2GMRr3,\Delta g \approx \pm \frac{2 G M R}{r^3}, where GG is the gravitational constant, MM is the mass of the Moon or Sun, RR is Earth's radius, and rr is the distance to the attracting body; the Moon's closer proximity (r384,400r \approx 384,400 km) amplifies its effect over the Sun's (r149.6×106r \approx 149.6 \times 10^6 km). On Earth, these forces manifest as diurnal tides (one high and one low per lunar day, common in the Gulf of Mexico) or semidiurnal tides (two highs and two lows of similar height per lunar day, prevalent along the U.S. East Coast). Mixed semidiurnal patterns, with unequal highs and lows, dominate the West Coast. Coastal regions experience amplified effects, including erosion from strong tidal currents, flooding during high tides that exacerbates storm surges, and navigational challenges in shallow waters where tides can exceed 10 meters in range, as in the Bay of Fundy. Tidal interactions have also led to the Moon's , where its rotational period with its around (both approximately 27.3 days), ensuring the same hemisphere always faces . This resulted from gravitational torques dissipating as heat over billions of years, a process that continues to subtly slow by about 2.3 milliseconds per century. Beyond oceans, tidal forces deform the by up to 30 cm vertically, causing measurable crustal flexing known as , which influence and . Atmospheric tides, driven by solar heating and lunar gravity, produce global pressure waves with diurnal (24-hour) and semidiurnal (12-hour) components, affecting upper atmospheric winds and ionospheric electron densities up to altitudes of 100 km. Isaac Newton first outlined the gravitational basis of tides in his 1687 Philosophiæ Naturalis Principia Mathematica, attributing oceanic bulges to the Moon's and Sun's attractions, though his equilibrium model overlooked dynamic ocean responses. Pierre-Simon Laplace refined this in the late 18th century through his Mécanique Céleste, incorporating hydrodynamic equations and global basin effects to better predict tidal variations, establishing the foundation for . Modern predictions rely on satellite altimetry from missions such as TOPEX/ (1992–2006) and the ongoing Sentinel-6 series (as of 2025), which map global ocean tides with centimeter accuracy, enabling precise models of tidal dissipation and circulation that improve forecasting for .

Orbital and Celestial Mechanics

Keplerian Orbits

Keplerian orbits represent the idealized motion of a smaller body, such as a or , around a much more massive central body under the influence of Newtonian gravity, where the force follows an . This framework assumes a , reducing the relative motion to a conic section—typically an for bound orbits—with the primary body at one focus. These orbits provide the foundational model for understanding planetary and artificial paths in . Johannes Kepler derived three empirical laws of planetary motion from meticulous observations of Mars made by Tycho Brahe. The first law, published in Astronomia Nova in 1609, states that a planet's orbit is an ellipse with the Sun at one of the two foci, replacing earlier circular models with a more accurate geometric description. The second law, also from 1609, asserts that a line joining the planet to the Sun sweeps out equal areas in equal intervals of time, implying that the orbital speed varies such that the planet moves faster near perihelion and slower near aphelion. The third law, announced in Harmonices Mundi in 1619, relates the orbital period TT to the semi-major axis aa of the ellipse via T2a3T^2 \propto a^3, applicable to all planets around the Sun. Isaac Newton later demonstrated in his Principia (1687) that these laws arise naturally from a central gravitational force proportional to 1/r21/r^2, unifying Kepler's empirical findings with a theoretical basis. The encapsulates the speed in a Keplerian , derived from in the under Newtonian gravity. For a body of μ\mu orbiting a central MM with gravitational parameter GMGM, the is constant, leading to the relation between vv, radial rr, and semi-major axis aa: v2=GM(2r1a)v^2 = GM \left( \frac{2}{r} - \frac{1}{a} \right) This equation follows by combining the total mechanical energy E=12v2GMr=GM2aE = \frac{1}{2} v^2 - \frac{GM}{r} = -\frac{GM}{2a} (constant for elliptical orbits) and solving for v2v^2, highlighting how speed depends on position and orbit size without needing angular momentum details. It applies to elliptical, parabolic, and hyperbolic trajectories, with negative aa for unbound cases. A Keplerian orbit is fully specified by six independent orbital elements, which describe its size, shape, orientation, and the body's position within it. These include the semi-major axis aa (defining the orbit's scale), eccentricity ee (measuring deviation from a circle, where 0e<10 \leq e < 1 for ellipses), inclination ii (angle between the orbital plane and a reference plane, such as the ecliptic), longitude of the ascending node Ω\Omega (orientation of the orbital plane), argument of periapsis ω\omega (angle from the ascending node to the periapsis), and true anomaly ν\nu (angle from periapsis to the current position). These elements enable precise prediction of positions for applications like satellite tracking. Keplerian orbits underpin practical engineering in space missions, such as calculating trajectories for satellite launches to achieve desired altitudes and inclinations using rocket burns timed via the vis-viva equation. In the Global Positioning System (GPS), satellite orbits are modeled as Keplerian ellipses with semi-major axes around 26,560 km, but relativistic effects from general relativity require corrections of about 45 microseconds per day to maintain positional accuracy within meters. The two-body approximation yields exact, closed-form solutions for bound orbits, ensuring long-term stability in isolation, though real-world perturbations—such as from Earth's oblateness or atmospheric drag—must be accounted for using numerical methods to refine predictions over time.

Gravitational Binding in Systems

In multi-body gravitational systems, binding arises from the negative gravitational potential energy that counteracts the positive kinetic energy of the components, maintaining overall stability. For a simple two-body system consisting of masses MM and mm separated by distance rr, the binding energy UU is the gravitational potential energy required to separate them to infinity, given by U=GMmr,U = -\frac{G M m}{r}, where GG is the gravitational constant. This negative value indicates the energy released upon formation and the work needed for disassembly. For stable, self-gravitating systems such as star clusters, the virial theorem provides a key relation between average kinetic energy K\langle K \rangle and potential energy U\langle U \rangle. In Newtonian gravity, where forces scale as 1/r21/r^2, the theorem states 2K+U=02 \langle K \rangle + \langle U \rangle = 0 for systems in equilibrium with no net change in moment of inertia over long timescales, such as orbital periods. This balance implies that the total energy E=K+U=12UE = \langle K \rangle + \langle U \rangle = \frac{1}{2} \langle U \rangle is negative, confirming bound states, with kinetic energy roughly half the magnitude of the potential energy. In solar system dynamics, gravitational binding extends to three-body interactions, where stable configurations emerge at Lagrange points—equilibrium positions in the restricted three-body problem dominated by two massive bodies like the Sun and a planet. These points, particularly the stable L4 and L5 triangular locations ahead and behind the secondary body, host Trojan asteroids in the Sun-Jupiter system, illustrating how binding enables long-term co-orbital stability through balanced gravitational and centrifugal forces. However, the three-body problem introduces chaos, as small perturbations in initial conditions lead to exponentially diverging trajectories; in the inner solar system, resonant interactions like the 2:1 Earth-Mars resonance drive chaotic zones with maximum Lyapunov exponents around (5×106yr)1(5 \times 10^6 \, \mathrm{yr})^{-1}, limiting long-term predictability despite overall binding. A related concept is escape velocity, the minimum speed vescv_\mathrm{esc} needed for a particle to escape a body's gravitational binding to infinity without further propulsion. For a spherical mass MM at radius rr, conservation of energy yields vesc=2GMr.v_\mathrm{esc} = \sqrt{\frac{2 G M}{r}}.
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