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Rankine scale

Absolute temperature scale using Fahrenheit degrees From Wikipedia, the free encyclopedia

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The Rankine scale (/ˈræŋkɪn/ RANG-kin) is an absolute scale of thermodynamic temperature named after the University of Glasgow engineer and physicist Macquorn Rankine, who proposed it in 1859.[1]

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History

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 K = 9/5 °Ra or 1 K = 1.8 °Ra. A temperature of 0 K (−273.15 °C; −459.67 °F) is equal to 0 °Ra.[2]

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Usage

The Rankine scale is used in engineering systems where heat computations are done using degrees Fahrenheit.[3]

The symbol for degrees Rankine is °R.[2] However, historical texts referring to "°R" are much more likely to mean the historically quite common Réaumur scale.[4] As there is also the Rømer scale, it is better to use °Ra to be unambiguous. 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.

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See also

Notes

  1. The freezing point of brine is the zero point of Fahrenheit scale, old definition, see: Grigull 1986
  2. The ice point of purified water has been measured to be 0.000089(10) degrees Celsius – see Magnum 1995
  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.
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References

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