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

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

Soil moisture–atmosphere feedback dominates land carbon uptake variability

Solved 50 Water Vapor grams per cubic meter) 40 20 20 40 Air

Movement of Water in Soil During Evaporation

Typical moisture uptake (in %) vs. time (in minutes) or water activity

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.

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

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

Evaluation of Soil-Gas Sampling Rate

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