A model of unsaturated soil-water movement using a prediction model of basic physical soil properties for calculating correlation functions was developed using VADOSE/W. The reliability of the model was assessed by comparing the results with those of a soil-column test. Coefficients of determination, R2, between the simulated and the measured daily evaporation for sand-mulch thicknesses of 0 (control, CK), 1.7, 3.6 and 5.7 cm were 0.8270, 0.8214, 0.8589 and 0.9851, respectively. R2, between the simulated and measured cumulative evaporation for mulch thicknesses of 0, 1.7, 3.6 and 5.7 cm were 0.9755, 0.9994, 0.9997 and 0.9983, respectively. The fits were, thus, good, verifying the reliability of the model. The program accurately predicted th...
The quantification of soil evaporation and of soil water content dynamics near the soil surface are ...
Predicting the flow of water between the soil surface and the atmosphere is a critical issue which g...
The Penman equation, which calculates potential evaporation, was modified by Staple (1974, Soil Scie...
The soil water evaporation is a critical component of both the surface energy balance and water bala...
Soil evaporation can signifi cantly infl uence energy fl ux partitioning of partially vegetated surf...
Soil water evaporation plays a critical role in mass and energy exchanges across the land–atmosphere...
Evaporation of water from a saturated soil surface with ample free water is known as potential evapo...
Dry desert climate required search for the best ways to conserve water. The present study was conduc...
Multiannual data (2016–2018) from 12 weighed lysimeters (four soil types with textures ranging from ...
International audienceThe global warming and climate change have aroused increasing attention to the...
Bare soils and grasslands in arid and semi-arid conditions constitute a large portion of the earth s...
Bare soils and grasslands in arid and semi-arid conditions constitute a large portion of the earth s...
© 2018 Evaporation from unsaturated soil is characterized by vapor transfer in the upper part and li...
Evaporation from bare soils is a major component of the hydrologic cycle and needs to be estimated f...
effect of soil suction on evaporative fluxes from soil surfaces G.W. Wilson, D.G. Fredlund, and S.L....
The quantification of soil evaporation and of soil water content dynamics near the soil surface are ...
Predicting the flow of water between the soil surface and the atmosphere is a critical issue which g...
The Penman equation, which calculates potential evaporation, was modified by Staple (1974, Soil Scie...
The soil water evaporation is a critical component of both the surface energy balance and water bala...
Soil evaporation can signifi cantly infl uence energy fl ux partitioning of partially vegetated surf...
Soil water evaporation plays a critical role in mass and energy exchanges across the land–atmosphere...
Evaporation of water from a saturated soil surface with ample free water is known as potential evapo...
Dry desert climate required search for the best ways to conserve water. The present study was conduc...
Multiannual data (2016–2018) from 12 weighed lysimeters (four soil types with textures ranging from ...
International audienceThe global warming and climate change have aroused increasing attention to the...
Bare soils and grasslands in arid and semi-arid conditions constitute a large portion of the earth s...
Bare soils and grasslands in arid and semi-arid conditions constitute a large portion of the earth s...
© 2018 Evaporation from unsaturated soil is characterized by vapor transfer in the upper part and li...
Evaporation from bare soils is a major component of the hydrologic cycle and needs to be estimated f...
effect of soil suction on evaporative fluxes from soil surfaces G.W. Wilson, D.G. Fredlund, and S.L....
The quantification of soil evaporation and of soil water content dynamics near the soil surface are ...
Predicting the flow of water between the soil surface and the atmosphere is a critical issue which g...
The Penman equation, which calculates potential evaporation, was modified by Staple (1974, Soil Scie...