Phasor: Difference between revisions

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Addition: In many 3 phase texts, -2 pi / 3 is preferred to 4pi / 3
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{{Orphan|date=February 2009}}
'''Relative thermal resistance''' is a measure of the [[energy]] required to mix water of two different temperatures (and thus different [[density|densities]]). Comparisons will be made against the differences in the density of water at 3.98°C and 5°C. <!-- Citation help is here http://www.google.com/search?&q=Wetzel+3.98+Density-of-water --> (Wetzel 1983) Since this is a relative measure, there are no units involved.
 
It is calculated at intervals of 1&nbsp;cm using the following equation:
<math>RTR= ((p_1-p_2) \times 10^{6})/ 8 </math>
where <math>p_2</math> is the density at the bottom of the stratum being considered
and <math>p_1</math> is the density at the top of the stratum being considered
 
==See also==
*[[Limnology]]
 
[[Category:Limnology]]
[[Category:Hydrography]]
[[Category:Lakes]]
 
{{Hydrology-stub}}

Revision as of 20:52, 27 December 2013

Template:Orphan Relative thermal resistance is a measure of the energy required to mix water of two different temperatures (and thus different densities). Comparisons will be made against the differences in the density of water at 3.98°C and 5°C. (Wetzel 1983) Since this is a relative measure, there are no units involved.

It is calculated at intervals of 1 cm using the following equation: RTR=((p1p2)×106)/8 where p2 is the density at the bottom of the stratum being considered and p1 is the density at the top of the stratum being considered

See also

Template:Hydrology-stub