kelvin | |
Standard: | SI |
Quantity: | temperature |
Symbol: | K |
Namedafter: | William Thomson, 1st Baron Kelvin |
Convertfromx: | yes |
Units1: | Celsius |
Inunits1: | ( − 273.15) °C |
Units2: | Fahrenheit |
Inunits2: | (1.8  − 459.67) °F |
Units3: | Rankine |
Inunits3: | 1.8  °Ra |
Extralabel: | 2019 definition |
Extradata: | ≝ |
The kelvin, symbol K, is the base unit of measurement for temperature in the International System of Units (SI). The Kelvin scale is an absolute temperature scale that starts from 0 K, the lowest possible temperature (absolute zero), then rises by exactly 1 K for each 1 °C. The Kelvin scale was designed to be easily converted from the Celsius scale (symbol °C). Any temperature in degrees Celsius can be converted to kelvin by adding 273.15.
The 19th century British scientist Lord Kelvin first developed and proposed the scale. It was often called the "absolute Celsius" scale in the early 20th century. The kelvin was formally added to the International System of Units in 1954, defining 273.16 K to be the triple point of water. The Celsius, Fahrenheit, and Rankine scales were redefined in terms of the Kelvin scale using this definition. The 2019 redefinition of the SI base units now defines the kelvin in terms of energy by setting the Boltzmann constant to exactly joules per kelvin; every 1 K change of thermodynamic temperature corresponds to a thermal energy change of exactly .
During the 18th century, multiple temperature scales were developed,[1] notably Fahrenheit and centigrade (later Celsius). These scales predated much of the modern science of thermodynamics, including atomic theory and the kinetic theory of gases which underpin the concept of absolute zero. Instead, they chose defining points within the range of human experience that could be reproduced easily and with reasonable accuracy, but lacked any deep significance in thermal physics. In the case of the Celsius scale (and the long since defunct Newton scale and Réaumur scale) the melting point of ice served as such a starting point, with Celsius being defined (from the 1740s to the 1940s) by calibrating a thermometer such that:
This definition assumes pure water at a specific pressure chosen to approximate the natural air pressure at sea level. Thus, an increment of 1 °C equals of the temperature difference between the melting and boiling points. The same temperature interval was later used for the Kelvin scale.
From 1787 to 1802, it was determined by Jacques Charles (unpublished), John Dalton, and Joseph Louis Gay-Lussac that, at constant pressure, ideal gases expanded or contracted their volume linearly (Charles's law) by about 1/273 parts per degree Celsius of temperature's change up or down, between 0 °C and 100 °C. Extrapolation of this law suggested that a gas cooled to about −273 °C would occupy zero volume.
In 1848, William Thomson, who was later ennobled as Lord Kelvin, published a paper On an Absolute Thermometric Scale. The scale proposed in the paper turned out to be unsatisfactory, but the principles and formulas upon which the scale was based were correct.[2] For example, in a footnote, Thomson derived the value of −273 °C for absolute zero by calculating the negative reciprocal of 0.00366—the coefficient of thermal expansion of an ideal gas per degree Celsius relative to the ice point.[3] This derived value agrees with the currently accepted value of −273.15 °C, allowing for the precision and uncertainty involved in the calculation.
The scale was designed on the principle that "a unit of heat descending from a body at the temperature ° of this scale, to a body at the temperature, would give out the same mechanical effect, whatever be the number ." Specifically, Thomson expressed the amount of work necessary to produce a unit of heat (the thermal efficiency) as
\mu(t)(1+Et)/E
t
E
\mu(t)
T1848=f(T)
T
dT1848/dT
\mu
\mu(t)
J
T
Thomson understood that with Joule's proposed formula for
\mu
J
To explain this definition, consider a reversible Carnot cycle engine, where
QH
QC
W
QH-QC
tH
tC
\mu=W/QH/(tH-tC)
TH=J/\mu
TH=J x QH x (tH-tC)/W
TH-TC=J x (tH-tc)
QH/TH=QC/TC
This definition by itself is not sufficient. Thomson specified that the scale should have two properties:
These two properties would be featured in all future versions of the Kelvin scale, although it was not yet known by that name. In the early decades of the 20th century, the Kelvin scale was often called the "absolute Celsius" scale, indicating Celsius degrees counted from absolute zero rather than the freezing point of water, and using the same symbol for regular Celsius degrees, °C.[7]
In 1873, William Thomson's older brother James coined the term triple point[8] to describe the combination of temperature and pressure at which the solid, liquid, and gas phases of a substance were capable of coexisting in thermodynamic equilibrium. While any two phases could coexist along a range of temperature-pressure combinations (e.g. the boiling point of water can be affected quite dramatically by raising or lowering the pressure), the triple point condition for a given substance can occur only at a single pressure and only at a single temperature. By the 1940s, the triple point of water had been experimentally measured to be about 0.6% of standard atmospheric pressure and very close to 0.01 °C per the historical definition of Celsius then in use.
In 1948, the Celsius scale was recalibrated by assigning the triple point temperature of water the value of 0.01 °C exactly[9] and allowing the melting point at standard atmospheric pressure to have an empirically determined value (and the actual melting point at ambient pressure to have a fluctuating value) close to 0 °C. This was justified on the grounds that the triple point was judged to give a more accurately reproducible reference temperature than the melting point.[10] The triple point could be measured with ±0.0001 °C accuracy, while the melting point just to ±0.001 °C.
In 1954, with absolute zero having been experimentally determined to be about −273.15 °C per the definition of °C then in use, Resolution 3 of the 10th General Conference on Weights and Measures (CGPM) introduced a new internationally standardized Kelvin scale which defined the triple point as exactly 273.15 + 0.01 = 273.16 degrees Kelvin.[11] [12]
In 1967/1968, Resolution 3 of the 13th CGPM renamed the unit increment of thermodynamic temperature "kelvin", symbol K, replacing "degree Kelvin", symbol .[13] The 13th CGPM also held in Resolution 4 that "The kelvin, unit of thermodynamic temperature, is equal to the fraction of the thermodynamic temperature of the triple point of water."[14] [15]
After the 1983 redefinition of the metre, this left the kelvin, the second, and the kilogram as the only SI units not defined with reference to any other unit.
In 2005, noting that the triple point could be influenced by the isotopic ratio of the hydrogen and oxygen making up a water sample and that this was "now one of the major sources of the observed variability between different realizations of the water triple point", the International Committee for Weights and Measures (CIPM), a committee of the CGPM, affirmed that for the purposes of delineating the temperature of the triple point of water, the definition of the kelvin would refer to water having the isotopic composition specified for Vienna Standard Mean Ocean Water.[16] [17]
See main article: 2019 redefinition of the SI base units. In 2005, the CIPM began a programme to redefine the kelvin (along with other SI base units) using a more experimentally rigorous method. In particular, the committee proposed redefining the kelvin such that the Boltzmann constant would take the exact value .[18] The committee hoped the program would be completed in time for its adoption by the CGPM at its 2011 meeting, but at the 2011 meeting the decision was postponed to the 2014 meeting when it would be considered part of a larger program.[19] A challenge was to avoid degrading the accuracy of measurements close to the triple point. The redefinition was further postponed in 2014, pending more accurate measurements of the Boltzmann constant in terms of the current definition,[20] but was finally adopted at the 26th CGPM in late 2018, with a value of =
For scientific purposes, the redefinition's main advantage is in allowing more accurate measurements at very low and very high temperatures, as the techniques used depend on the Boltzmann constant. Independence from any particular substance or measurement is also a philosophical advantage. The kelvin now only depends on the Boltzmann constant and universal constants (see 2019 SI unit dependencies diagram), allowing the kelvin to be expressed exactly as:
1 kelvin = = .
For practical purposes, the redefinition was unnoticed; enough digits were used for the Boltzmann constant to ensure that 273.16 K has enough significant digits to contain the uncertainty of water's triple point and water still normally freezes at 0 °C[21] to a high degree of precision. But before the redefinition, the triple point of water was exact and the Boltzmann constant had a measured value of, with a relative standard uncertainty of .[22] Afterward, the Boltzmann constant is exact and the uncertainty is transferred to the triple point of water, which is now .
The new definition officially came into force on 20 May 2019, the 144th anniversary of the Metre Convention.[23]
See also: Stefan–Boltzmann constant. The kelvin is often used as a measure of the colour temperature of light sources. Colour temperature is based upon the principle that a black body radiator emits light with a frequency distribution characteristic of its temperature. Black bodies at temperatures below about appear reddish, whereas those above about appear bluish. Colour temperature is important in the fields of image projection and photography, where a colour temperature of approximately is required to match "daylight" film emulsions.
In astronomy, the stellar classification of stars and their place on the Hertzsprung–Russell diagram are based, in part, upon their surface temperature, known as effective temperature. The photosphere of the Sun, for instance, has an effective temperature of https://books.google.com/books?id=zT2HEAAAQBAJ&pg=PA216https://nssdc.gsfc.nasa.gov/planetary/factsheet/sunfact.htmlhttps://books.google.com/books?id=2QBBEAAAQBAJ&dq=5772+K&pg=PA51https://arxiv.org/pdf/1605.09788.pdf# as adopted by IAU 2015 Resolution B3.
Digital cameras and photographic software often use colour temperature in K in edit and setup menus. The simple guide is that higher colour temperature produces an image with enhanced white and blue hues. The reduction in colour temperature produces an image more dominated by reddish, "warmer" colours.
See main article: Noise figure. For electronics, the kelvin is used as an indicator of how noisy a circuit is in relation to an ultimate noise floor, i.e. the noise temperature. The Johnson–Nyquist noise of resistors (which produces an associated kTC noise when combined with capacitors) is a type of thermal noise derived from the Boltzmann constant and can be used to determine the noise temperature of a circuit using the Friis formulas for noise.
See main article: Orders of magnitude (temperature). The only SI derived unit with a special name derived from the kelvin is the degree Celsius. Like other SI units, the kelvin can also be modified by adding a metric prefix that multiplies it by a power of 10:
According to SI convention, the kelvin is never referred to nor written as a degree. The word "kelvin" is not capitalized when used as a unit. It may be in plural form as appropriate (for example, "it is 283 kelvins outside", as for "it is 50 degrees Fahrenheit" and "10 degrees Celsius").[24] [25] The unit's symbol K is a capital letter,[26] per the SI convention to capitalize symbols of units derived from the name of a person.[27] It is common convention to capitalize Kelvin when referring to Lord Kelvin or the Kelvin scale.[28]
The unit symbol K is encoded in Unicode at code point . However, this is a compatibility character provided for compatibility with legacy encodings. The Unicode standard recommends using instead; that is, a normal capital K. "Three letterlike symbols have been given canonical equivalence to regular letters:,, and . In all three instances, the regular letter should be used."[29]
"If we push the strict principle of graduation, stated above, sufficiently far, we should arrive at a point corresponding to the volume of air being reduced to nothing, which would be marked as −273° of the scale (−100/·366, if ·366 be the coefficient of expansion); and therefore −273° of the air-thermometer is a point which cannot be reached at any finite temperature, however low."
"The arbitrary points which coincide on the two scales are 0° and 100°"