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ITS90 : ウィキペディア英語版
International Temperature Scale of 1990
The International Temperature Scale of 1990 (ITS-90) published by the Consultative Committee for Thermometry (CCT) of the International Committee for Weights and Measures (CIPM) is an equipment calibration standard for making measurements on the Kelvin and Celsius temperature scales.
ITS–90 is an approximation of the thermodynamic temperature scale that facilitates the comparability and compatibility of temperature measurements internationally.
It offers defined calibration points ranging from 0.65 K to approximately 1358 K (−272.5 °C to 1085 °C) and is subdivided into multiple temperature ranges which overlap in some instances.
ITS-90 is the latest (as of 2014) of a series of International Temperature Scales adopted by CIPM since 1927.〔"Beginning in 1927, the CIPM, acting under the authority of the General Conference on Weights and
Measures (CGPM) and, since 1937, on the advice of its Consultative Committee for Thermometry
(CCT), has adopted a series of International Temperature Scales. Subsequent to the 1927 scale, new
scales have been adopted in 1948, 1968, and 1990, with occasional minor revisions in intervening years."〕
Adopted at the 1989 General Conference on Weights and Measures, it supersedes the International Practical Temperature Scale of 1968 (amended edition of 1975) and the 1976 "Provisional 0,5 K to 30 K Temperature Scale". CCT has also adopted a ''mise en pratique'' (practical instructions) in 2011.〔"In practice, primary thermometry is difficult and time consuming and not a practical means of disseminating the kelvin. As an alternative, the International Temperature Scale provides an internationally accepted recipe for realizing temperature in a practical way." Consultative Committee for Thermometry, "''Mise en pratique'' for the definition of the kelvin", 2011.〕
The lowest temperature covered by ITS-90 is 0.65 K. In 2000, the temperature scale was extended further, to 0.9 mK, by the adoption of a supplemental scale, known as the Provisional Low Temperature Scale of 2000 (PLTS-2000).〔"Considerable research has been conducted on establishing a temperature scale extending to temperatures lower than 0.65 K; the PLTS-2000 is the resulting outcome, defining temperature from 1 K down to
0.9 mK. The PLTS-2000 is explicitly a provisional scale, recognizing that the data sets comprising the
basis of the scale were somewhat inconsistent below 10 mK. In the temperature range 0.65 K to 1 K,
temperature may be defined on either the ITS-90 or the PLTS-2000. Either scale is acceptable; the choice
of scale typically is dictated by convenience or the attainable uncertainty of realization. In those rare
cases where use of either scale is convenient, ''T2000 is a better approximation of thermodynamic
temperature than T90 in the region of overlap." Consultative Committee for Thermometry, "''Mise en pratique'' for the definition of the kelvin", 2011.〕
== Details ==
CCT
ITS-90 is designed to represent the thermodynamic (absolute) temperature scale (referencing absolute zero) as closely as possible throughout its range. Many different thermometer designs are required to cover the entire range. These include helium vapor pressure thermometers, helium gas thermometers, standard platinum resistance thermometers (known as SPRTs, PRTs or Platinum RTDs) and monochromatic radiation thermometers.
Although the Kelvin and Celsius scales are defined using absolute zero (0 K) and the triple point of water (273.16 K and 0.01 °C), it is impractical to use this definition at temperatures that are very different from the triple point of water. Accordingly, ITS–90 uses numerous defined points, all of which are based on various thermodynamic equilibrium states of fourteen pure chemical elements and one compound (water). Most of the defined points are based on a phase transition; specifically the melting/freezing point of a pure chemical element. However, the deepest cryogenic points are based exclusively on the vapor pressure/temperature relationship of helium and its isotopes whereas the remainder of its cold points (those less than room temperature) are based on triple points. Examples of other defining points are the triple point of hydrogen (−259.3467 °C) and the freezing point of aluminum (660.323 °C).
Thermometers calibrated per ITS–90 use complex mathematical formulas to interpolate between its defined points. ITS–90 specifies rigorous control over variables to ensure reproducibility from lab to lab. For instance, the small effect that atmospheric pressure has upon the various melting points is compensated for (an effect that typically amounts to no more than half a millikelvin across the different altitudes and barometric pressures likely to be encountered). The standard even compensates for the pressure effect due to how deeply the temperature probe is immersed into the sample. ITS–90 also draws a distinction between “freezing” and “melting” points. The distinction depends on whether heat is going ''into'' (melting) or ''out of'' (freezing) the sample when the measurement is made. Only gallium is measured while melting, all the other metals are measured while the samples are freezing.
A practical effect of ITS–90 is the triple points and the freezing/melting points of its thirteen chemical elements are precisely known for all temperature measurements calibrated per ITS–90 since these thirteen values are fixed by its definition. Only the triple point of Vienna Standard Mean Ocean Water (VSMOW) is known with absolute precision—regardless of the calibration standard employed—because the very definitions of both the Kelvin and Celsius scales are fixed by international agreement based, in part, on this point.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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