Rankine scale

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Rankine
Unit ofTemperature
Symbol°R, °Ra
Named afterW. J. M. Rankine
Conversions
491.67 °R in ...... corresponds to ...
   Kelvin scale   273.15 K
   Celsius scale   0.00 °C
   Fahrenheit   32.00 °F
A man with a beard and curly hair sitting at a table with an open book.
W.J. Rankine

The Rankine scale (/ˈræŋkɪn/ RANG-kin) is an absolute scale of thermodynamic temperature named after the University of Glasgow engineer and physicist W. J. M. Rankine, who proposed it in 1859.[1] Similar to the Kelvin scale, which was first proposed in 1848,[1] zero on the Rankine scale is absolute zero, but a temperature difference of one Rankine degree (°R or °Ra) is defined as equal to one Fahrenheit degree, rather than the Celsius degree used on the Kelvin scale. In converting from kelvin to degrees Rankine, 1 °R = 5/9 K or 1 K = 1.8 °R. A temperature of 0 K (−273.15 °C; −459.67 °F) is equal to 0 °R.[2][3]

Usage

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The Rankine scale is used in engineering systems where heat computations are done using degrees Fahrenheit.[4][better source needed]

The symbol for degrees Rankine is °R[2] (or °Ra if necessary to distinguish it from the Rømer and Réaumur scales). By analogy with the SI unit kelvin, some authors term the unit Rankine, omitting the degree symbol.[5][6]

Some temperatures relating the Rankine scale to other temperature scales are shown in the table below.

Scale
Kelvin Rankine Fahrenheit Celsius Réaumur
Temperature Absolute zero 0 K 0.00 °R −459.67 °F −273.15 °C −218.52 °Ré
Freezing point of brine[a] 255.37 K 459.67 °R 0.00 °F −17.78 °C −14.22 °Ré
Freezing point of water[b] 273.15 K 491.67 °R 32.00 °F 0.00 °C 0 °Ré
Boiling point of water[c] 373.1339 K 671.641 °R 211.971 °F 99.9839 °C 79.9871 °Ré

See also

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Notes

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  1. ^ The freezing point of brine is the zero point of Fahrenheit scale, old definition.[7]
  2. ^ The ice point of purified water has been measured to be 0.00008910 degrees Celsius.[8]
  3. ^ For Vienna Standard Mean Ocean Water at one standard atmosphere (101.325 kPa) when calibrated solely per the two-point definition of thermodynamic temperature. Older definitions of the Celsius scale once defined the boiling point of water under one standard atmosphere as being precisely 100 °C. However, the current definition results in a boiling point that is actually 16.1 mK less. For more about the actual boiling point of water, see VSMOW in temperature measurement.[citation needed]

References

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