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Illuminance
Illuminance
from Wikipedia
Illuminance
Common symbols
Ev
SI unitlux
Other units
phot, foot-candle
In SI base unitscd·sr·m−2
Dimension
Illuminance diagram with units and terminology.
Illuminance diagram with units and terminology

In photometry, illuminance is the total luminous flux incident on a surface, per unit area.[1] It is a measure of how much the incident light illuminates the surface, wavelength-weighted by the luminosity function to correlate with human brightness perception.[2] Similarly, luminous emittance is the luminous flux per unit area emitted from a surface. Luminous emittance is also known as luminous exitance.[3][4]

In SI units illuminance is measured in lux (lx), or equivalently in lumens per square metre (lm·m−2).[2] Luminous exitance is measured in lm·m−2 only, not lux.[4] In the CGS system, the unit of illuminance is the phot, which is equal to 10000 lux. The foot-candle is a non-metric unit of illuminance that is used in photography.[5]

Illuminance was formerly often called brightness, but this leads to confusion with other uses of the word, such as to mean luminance. "Brightness" should never be used for quantitative description, but only for nonquantitative references to physiological sensations and perceptions of light.

The human eye is capable of seeing somewhat more than a 2 trillion-fold range. The presence of white objects is somewhat discernible under starlight, at 5×10−5 lux (50 μlx), while at the bright end, it is possible to read large text at 108 lux (100 Mlx), or about 1000 times that of direct sunlight, although this can be very uncomfortable and cause long-lasting afterimages.[citation needed]

Common illuminance levels

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A lux meter for measuring illuminances in work environments
Lighting condition Foot-candles Lux
Sunlight 10,000 [6] 100,000
Shade on a sunny day 1,000 10,000
Overcast day 100 1,000
Very dark day 10 100
Twilight 1 10
Deep twilight 0.1 1
Full moon 0.01 0.1
Quarter moon 0.001 0.01
Starlight 0.0001 0.001
Overcast night 0.00001 0.0001

Astronomy

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In astronomy, the illuminance stars cast on the Earth's atmosphere is used as a measure of their brightness. The usual units are apparent magnitudes in the visible band.[7] V-magnitudes can be converted to lux using the formula[8] where Ev is the illuminance in lux, and mv is the apparent magnitude. The reverse conversion is

Relation to luminance

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Comparison of photometric and radiometric quantities

The luminance of a reflecting surface is related to the illuminance it receives: where the integral covers all the directions of emission ΩΣ, and

In the case of a perfectly diffuse reflector (also called a Lambertian reflector), the luminance is isotropic, per Lambert's cosine law. Then the relationship is simply

See also

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References

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Illuminance is a photometric that describes the total incident on a surface per unit area, serving as a measure of the intensity of illuminating that surface. It is distinct from , which refers to the emitted or reflected from a surface, and is fundamental in assessing how interacts with environments to enable visibility. The SI unit of illuminance is the (lx), defined as one lumen per square meter (lm/), where the lumen quantifies the weighted by human visual sensitivity. In and , illuminance plays a critical role in ensuring optimal visual performance, comfort, and safety across various settings, from workplaces to public spaces. Standards such as EN 12464 specify minimum illuminance levels for indoor environments, recommending at least 500 lx on work surfaces for general offices to support tasks like reading and computer use, while higher levels—up to 1000 lx or more—are required for precision work such as inspection or drawing. For residential areas, the Illuminating Engineering Society (IES) suggests 200–300 lx for living rooms and 300–800 lx for kitchens to balance functionality and energy efficiency. These recommendations account for factors like task demands and occupant well-being, with insufficient illuminance leading to and reduced productivity, and excessive levels contributing to or unnecessary . Illuminance is measured using devices called lux meters or illuminance meters, which detect light across the and provide readings in to guide installation and of systems. Its calculation often involves the for point sources, where illuminance decreases with the square of the distance from the light source, influencing applications in , , and . By standardizing illuminance targets, professionals can create environments that enhance human perception while complying with international guidelines from bodies like the IES and the (CIE).

Fundamentals

Definition

Illuminance is a fundamental photometric quantity that describes the total incident on a surface per unit area, where represents the measure of visible light weighted by the of the human visual system. This weighting accounts for the eye's varying response to different wavelengths, using the photopic V(λ) under normal daylight conditions or the scotopic function V'(λ) in low-light environments. As such, illuminance quantifies the density of visible light reaching a given point on a surface, irrespective of the light's direction of incidence or the emitting source. Mathematically, illuminance Ev is expressed as: Ev=ΦvAE_v = \frac{\Phi_v}{A} where Φv is the in lumens and A is the surface area in square meters. itself is the total quantity of light emitted or received, perceived by the . The origins of illuminance trace back to 19th-century photometric investigations into light measurement, which sought to standardize of brightness. The term and its formal definition were established in the 1920s by the (CIE), which introduced the standard spectral luminous efficiency functions to enable consistent photometric evaluations.

Units and Standards

The primary unit of illuminance in the (SI) is the lux (symbol: lx), defined as the illuminance produced by a luminous flux of one lumen (lm) uniformly distributed over a surface of one square meter (m²). This coherent derived unit ensures consistency in photometric measurements worldwide, with the lux adopted by the 11th General Conference on Weights and Measures (CGPM) in 1960. Historically, illuminance was measured using non-SI units such as the foot-candle (fc), which originated in the late 19th century as the illuminance from a standard candle at a distance of one foot, standardized by the Illuminating in for practical lighting applications in the United States. Another unit, the phot (ph), was coined in 1921 as part of the centimeter-gram-second (CGS) system, defined as one lumen per square centimeter (cm²), primarily used in scientific contexts before the widespread adoption of SI units. Both units have become obsolete in modern international standards due to the global shift to SI, though the foot-candle persists in some legacy engineering and photography practices in non-metric regions. Common conversions between these units are essential for transitioning measurements across systems. The table below summarizes key factors, based on exact definitions where 1 fc = 1 lm/ft² and 1 = 1 lm/cm².
UnitSymbolRelation to Lux (lx)
Luxlx1 lx
fc1 lx = 0.092903 fc
ph1 lx = 0.0001
These conversions derive from area equivalences, with 1 m² = 10.76391 ft² and 1 m² = 10,000 cm². The (CIE) plays a central role in standardizing illuminance through its definition of the spectral luminous efficiency function V(λ), which weights for human and underpins precise calculations. In the 1980s, the CIE updated this function with the 1988 2° spectral luminous efficiency function for , providing official recognition of refined data from vision research to better account for foveal sensitivity across wavelengths. Following the 2019 revision of the SI by the 26th CGPM, non-SI units like the and phot were further deprecated for formal use, as the updated SI Brochure explicitly limits accepted non-SI units to a select list excluding photometric ones, reinforcing the exclusive adoption of the in scientific and international contexts.

Measurement

Instruments

Illuminance meters, commonly referred to as meters, are the primary instruments for measuring illuminance, the density of luminous flux incident on a surface. These devices typically utilize photodiodes as detectors, paired with V(λ) correction filters to closely replicate the of the under photopic conditions, as defined by the CIE 1924 luminosity function. The photodiode generates a proportional to the illuminance, which is then amplified and processed to provide readings in . Common types include handheld digital illuminance meters, which offer portability and ease of use for field applications, featuring digital displays such as LCDs for direct readout of illuminance values. For scenarios requiring uniform illumination measurement, integrating spheres are employed to create a homogeneous field, facilitating accurate and testing of illuminance meters by distributing light evenly across the detector surface. Calibration of illuminance meters is essential for and accuracy, with standards provided by organizations such as the National Institute of Standards and Technology (NIST) and the International Commission on Illumination (CIE). These calibrations involve direct substitution against reference photometers under controlled conditions, ensuring compliance with SI units, and manufacturers typically recommend annual recalibration to account for potential drift in detector response. Advanced variants, such as spectroradiometers, enable measurement of illuminance by capturing the full of incident light, allowing computation of illuminance weighted by V(λ). These instruments gained prominence in the for detailed analysis of complex sources like LED , where spectral content affects perceived illuminance and color rendering.

Techniques

The basic procedure for measuring illuminance involves positioning the of an illuminance meter to the incident light rays to capture the total on a surface accurately. This orientation ensures that the measurement reflects the direct and diffuse components falling on the plane, with the placed flat against the surface rather than suspended above it. To account for variations in conditions, multiple readings are taken at the same location and averaged, typically over several minutes or across repeated sessions to minimize temporal fluctuations. Illuminance measurements can be planar, targeting light on a specific surface, or hemispherical, integrating light from the entire surrounding environment; for diffuse scenarios common in indoor or conditions, cosine correction is essential to adjust for the angular dependence of incidence according to the cosine law. This correction is achieved by attaching diffusers, such as opal glass or PTFE, to the meter sensor, which approximate an ideal cosine response and reduce errors from off-axis rays. Without proper cosine correction, readings can deviate significantly at oblique angles, particularly beyond 60 degrees from the normal. In field techniques, illuminance mapping in rooms or spaces employs systematic grid patterns or cross-sections to evaluate lighting uniformity, with sensors moved methodically across predefined points on horizontal and vertical surfaces. Post-2020 advancements have integrated software for logging and visualization, enabling automated collection via mobile devices or robotic systems that generate detailed illuminance maps for analysis. These methods facilitate comprehensive assessments, such as plotting contours of light distribution to identify hotspots or deficiencies. Common error sources in illuminance measurement include , which introduces unintended illumination from extraneous sources, and cosine errors from imperfect angular responses. can be mitigated by shielding the and conducting measurements in controlled environments, while cosine errors are quantified and corrected using quality indices like the directional response index (f₂) defined in ISO/CIE 19476. Adherence to ISO 17025 protocols for laboratories further ensures and reduces overall through standardized verification procedures.

Photometric Relations

Relation to Luminous Flux

Illuminance is fundamentally defined as the amount of incident on a surface per unit area. Mathematically, for a small differential area where the illumination can be considered uniform, illuminance EE is expressed as the ratio of the differential dΦd\Phi to the differential area dAdA: E=dΦdAE = \frac{d\Phi}{dA} This relation, with EE measured in (lx) or lumens per square meter (lm/m²), quantifies how the total visible power, weighted by human visual sensitivity, is distributed across the receiving surface. For extended surfaces experiencing non-uniform illumination, the direct relation extends to an integrated form. The total Φ\Phi incident on the entire surface is then calculated by integrating the illuminance over the area: Φ=SEdA\Phi = \int_S E \, dA where SS denotes the surface. This inverse operation allows designers to compute the overall light output required from sources to achieve specified illuminance distributions, ensuring efficient use of luminous energy. A practical derivation of this relation appears in the case of a , where illuminance decreases with the inverse square of the distance due to flux spreading over a spherical surface. For a point source with luminous intensity II (in , cd, defined as luminous flux per unit in lumens per , lm/sr), the illuminance EE at a perpendicular distance dd (in meters) is: E=Id2E = \frac{I}{d^2} This equation arises because the flux dΦ=IdΩd\Phi = I \, d\Omega through a small solid angle dΩ=dA/d2d\Omega = dA / d^2 yields E=dΦ/dA=I/d2E = d\Phi / dA = I / d^2. Luminous intensity itself incorporates the visibility factor V(λ)V(\lambda), the spectral luminous efficiency function that weights radiant power by eye sensitivity, but for broadband sources, it is embedded in the photometric units. This formula applies for normal incidence, where the surface is perpendicular to the line from the source. For oblique incidence, illuminance follows Lambert's cosine law, which reduces it by the cosine of the angle of incidence θ\theta (the angle between the surface normal and the direction to the source): E=Icosθr2E = \frac{I \cos \theta}{r^2} where rr is the distance from the source to the point on the surface. For a horizontal surface illuminated by an overhead source at vertical height hh, with horizontal distance dd to the point directly below the source, cosθ=h/r\cos \theta = h / r and r=h2+d2r = \sqrt{h^2 + d^2}
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