Absorption of vapors and gases by soils . Fig. 16.—Curve showing rate of evaporationPodimk soil. >f water from aLoc. cit. &Comp. rend.. !><). 741 (1880). cCameron and Gallagher, Bui. 50, Bureau

The figure shows the variation of specific heat capacity (C) of a solid as a of temperature (T). The temperature is increased continuously from 0 to 500 K at a constant rate.

Water vapor adsorption by dry soils: A potential link between the water and carbon cycles - ScienceDirect

Water vapor adsorption by dry soils: A potential link between the water and carbon cycles - ScienceDirect

Evaporation and Evapotranspiration: The Vapor Losses to the Atmosphere

Evaporation gases hi-res stock photography and images - Page 2 - Alamy

Analytical model for bare soil evaporation dynamics following wetting with concurrent internal drainage - ScienceDirect

Evaluation of radiative absorption effect to estimate mean radiant temperature in environments with high water vapor concentration such as in a sauna - ScienceDirect

Soil moisture–atmosphere feedback dominates land carbon uptake variability

Evaporation coefficient and condensation coefficient of vapor under high gas pressure conditions