"वाष्पीकरण" का संशोधनहरू बिचको अन्तर

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पङ्क्ति २४:
=== Evaporative equilibrium ===
 
[[Image:Water vapor pressure graph.jpg|thumb|240px|right|Vapor pressure of water vs. temperature. 760 [[Torr]] = 1 [[Atmosphere (unit)|atm]].]]
 
If evaporation takes place in a closed vessel, the escaping molecules accumulate as a [[vapor]] above the liquid. Many of the [[molecules]] return to the liquid, with returning molecules becoming more frequent as the [[density]] and [[pressure]] of the vapor increases. When the process of escape and return reaches an [[Thermodynamic equilibrium|equilibrium]],<ref name="Silberberg" /> the vapor is said to be "saturated," and no further change in either [[vapor pressure]] and density or liquid temperature will occur. For a system consisting of vapor and liquid of a pure substance, this equilibrium state is directly related to the vapor pressure of the substance, as given by the [[Clausius-Clapeyron relation]]:
पङ्क्ति ४८:
;[[Density]]: The higher the density the slower a liquid evaporates.
 
In the US, the National Weather Service measures the actual rate of evaporation from a standardized "pan" open water surface outdoors, at various locations nationwide. Others do likewise around the world. The US data is collected and compiled into an annual evaporation map.<ref>[http://www.grow.arizona.edu/Grow--GrowResources.php?ResourceId=208 Geotechnical, Rock and Water Resources Library - Grow Resource - Evaporation<!-- Bot generated title -->]</ref> The measurements range from under 30३० to over {{convert|120|in|mm}} per year.
 
== Applications ==
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