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  1. 1 kwi 2019 · The vaporization plane forms if the water content of the surface soil reduces to the field water retention capacity, which is the natural water content in equilibrium with free drain condition. At that moment, the evaporation rate starts to decrease gradually.

  2. 3 lut 2017 · This enhancement is attributed to the change in surface tension that results from changes in soil water composition (ionic strength, concentration of organic surfactants) with temperature.

  3. Download scientific diagram | Relationship between soil moisture (W) and temperature (T) and the rates of soil temperature change with soil moisture at different periods.

  4. 6 lut 2008 · This study proposes an approach to model near-surface soil temperature profiles in a bare soil, using only a single temperature measurement, net radiation, and an estimate of the soil moisture content.

  5. 30 gru 1997 · Abstract. A modelling approach for predicting soil surface temperature and soil evaporation is presented. The procedure is based on the equations for heat flow at the soil surface and includes vapour diffusion and a semi-empirical correction function for the surface vapour pressure.

  6. 1 cze 2020 · To understand the water-vapor migration process and deformation of freezing unsaturated soils, we conducted a series of one-dimensional freezing tests to study the influences of the initial water content and cooling temperature on the water-vapor migration and deformation of unsaturated soils.

  7. Dr. Francis Hole, Soil Scientist (1913-2002) The soil is an important component of biometeorology. The soil surface is the lowest boundary of the biosphere-atmosphere system. Rules and tools learn so far for the atmosphere, need to be modified when applied to the soil. The soil environment contrasts