A numerical model of water evaporation from cracked soil
Cracking is a common phenomenon in clayey soils under soil-atmosphere interaction. It
strongly promotes water evaporation and further affects thermo-hydro-mechanical behavior …
strongly promotes water evaporation and further affects thermo-hydro-mechanical behavior …
Modelling of water evaporation from cracked clayey soil
WK Song, YJ Cui - Engineering geology, 2020 - Elsevier
A model for predicting water evaporation from clayey soil with desiccation cracks was
developed based on a general suction-related model. The effect of desiccation cracks was …
developed based on a general suction-related model. The effect of desiccation cracks was …
[HTML][HTML] Integral solutions to transient nonlinear heat (mass) diffusion with a power-law diffusivity: a semi-infinite medium with fixed boundary conditions
J Hristov - Heat and Mass Transfer, 2016 - Springer
Closed form approximate solutions to nonlinear heat (mass) diffusion equation with power-
law nonlinearity of the thermal (mass) diffusivity have been developed by the integral …
law nonlinearity of the thermal (mass) diffusivity have been developed by the integral …
An analytical model for evaporation from unsaturated soil
Evaporation from unsaturated soil is characterized by vapor transfer in the upper part and
liquid water transfer in the lower part of the soil. This study develops an analytical model for …
liquid water transfer in the lower part of the soil. This study develops an analytical model for …
An improved cracked soil evaporation model accounting for solar radiation and wind effect
Investigating the evaporation process and corresponding soil moisture redistribution in
cracked soils amidst intricate atmospheric conditions poses persistent challenges. In this …
cracked soils amidst intricate atmospheric conditions poses persistent challenges. In this …
An approximate analytical (integral-balance) solution to a nonlinear heat diffusion equation
J Hristov - Thermal Science, 2015 - doiserbia.nb.rs
The communication presents a closed form approximate solution of the nonlinear diffusion
equation of a power-law nonlinearity of the diffusivity developed by the heat-balance integral …
equation of a power-law nonlinearity of the diffusivity developed by the heat-balance integral …
Modelling water content redistribution during evaporation from sandy soil in the presence of water table
An analytical model based on Richards equation is presented to describe water content
redistribution during evaporation. Exponential functions are utilized to describe the relation …
redistribution during evaporation. Exponential functions are utilized to describe the relation …
Analytical solution to transient Richards' equation with realistic water profiles for vertical infiltration and parameter estimation
M Hayek - Water Resources Research, 2016 - Wiley Online Library
A general analytical model for one‐dimensional transient vertical infiltration is presented.
The model is based on a combination of the Brooks and Corey soil water retention function …
The model is based on a combination of the Brooks and Corey soil water retention function …
An approximate solution to one-dimensional upward infiltration in soils for a rapid estimation of soil hydraulic properties
S Wu, D Ma, Z Liu, J Zhang, L Chen, X Pan, L Chen - Journal of Hydrology, 2022 - Elsevier
Soil hydraulic properties quantify soil pore structure and are essential input parameters for
simulating soil hydrological processes in the vadose zone. Although methods have been …
simulating soil hydrological processes in the vadose zone. Although methods have been …
Functional extremum solution and parameter estimation for one‐dimensional vertical infiltration using the Brooks–Corey model
L Su, X Yang, Q Wang, X Qin, B Zhou… - Soil Science Society of …, 2018 - Wiley Online Library
Core Ideas Least action and variational principles were used to simulate unsaturated
vertical infiltration. A functional extremum explicit solution to Richards' equation was …
vertical infiltration. A functional extremum explicit solution to Richards' equation was …