Kelvin (unit): Difference between revisions
imported>Alexander Wiebel (citation) |
imported>Paul Wormer m (rm centigrade (is not exactly Celsius)) |
||
| Line 7: | Line 7: | ||
The CIPM has specified the isotopic composition of standard water, as the triple point of water varies depending on the isotopic composition of water. | The CIPM has specified the isotopic composition of standard water, as the triple point of water varies depending on the isotopic composition of water. | ||
The [[Celsius]] | The [[Celsius]] scale is related to the kelvin (absolute) scale by setting the temperature zero degrees Celsius (0°C) to be exactly 273.15 K, and the increment of one degrees Celsius to be equal to one kelvin<ref name=BIPM />. The older [[Fahrenheit]] scale has 32 degrees Fahrenheit (32°F) equal to 273.15 K, and the increment of 1.8°F equal to one kelvin; thus absolute zero is -459.67°F. | ||
== References == | == References == | ||
<references /> | <references /> | ||
Revision as of 19:00, 13 April 2008
The kelvin (symbol: K) is the SI unit increment of temperature and is one of the seven SI base units. The kelvin is defined as 1/273.16 of the thermodynamic temperature of the triple point of water[1]. Zero kelvin (0 K) is the thermodynamic absolute zero.
The kelvin is named after the Irish-born physicist and engineer William Thomson, 1st Baron Kelvin (1824 – 1907), who wrote of the need for an absolute thermometric scale.
The CIPM has specified the isotopic composition of standard water, as the triple point of water varies depending on the isotopic composition of water.
The Celsius scale is related to the kelvin (absolute) scale by setting the temperature zero degrees Celsius (0°C) to be exactly 273.15 K, and the increment of one degrees Celsius to be equal to one kelvin[1]. The older Fahrenheit scale has 32 degrees Fahrenheit (32°F) equal to 273.15 K, and the increment of 1.8°F equal to one kelvin; thus absolute zero is -459.67°F.