Results 81 to 90 of about 166,663 (204)
Abstract Modeling unsaturated water transport in porous media traditionally relies on the Richards equation (RE) with hydraulic conductivity formulations to consider only capillary liquid water flow. However, this simplification neglects thin water films adsorbed onto particle surfaces, which can contribute significantly to flow under medium to dry ...
M. Kozyra, K. Lamorski, C. Sławiński
wiley +1 more source
A Novel Approach to Characterize and Model Drywell Infiltration Capacity
Abstract Drywells are vadose‐zone wells constructed for infiltration and recharge, typically positioned far above the water table. They provide for efficient infiltration, with high infiltration rates per land area, because the infiltration process is below the land surface.
Tamir Kamai
wiley +1 more source
Abstract Soil moisture dynamics in vertical profiles result from multiple interacting processes, generating complex temporal behavior and intricate connectivity patterns. However, accurately simulating multi‐depth soil moisture while diagnosing time‐varying vertical connectivity remains challenging.
Weiming Kang +4 more
wiley +1 more source
Simulation of Soil Temperature Dynamics with Models Using Different Concepts
This paper presents two soil temperature models with empirical and mechanistic concepts. At the test site (calcaric arenosol), meteorological parameters as well as soil moisture content and temperature at 5 different depths were measured in an experiment
Renáta Sándor, Nándor Fodor
doaj +1 more source
<p>batch HYDRUS-1D code for simulating RZSM and ET, with vegetation and test data</p ...
liao
core +1 more source
Modelling Climate Change Effects on Groundwater Recharge and Temperature for a Pre‐Alpine Lysimeter
Climate change is projected to increase winter groundwater recharge and extreme precipitation events in pre‐alpine regions. Groundwater temperatures will rise by up to 26%, primarily driven by air temperature. These trends pose challenges for future water availability and quality, requiring adaptive water resource management.
Christian Moeck +7 more
wiley +1 more source
Knowledge of the groundwater recharge rate determines whether aquifer use is sustainable. However, accurately measuring recharge globally presents significant challenges due to the complexity of subsurface processes and the lack of direct observational ...
M. E. Soylu, D. Entekhabi, R. L. Bras
doaj +1 more source
Sensitivity and uncertainty analysis of the HYDRUS-1D model for root water uptake in saline soils
A variance-based global sensitivity analysis (extended Fourier amplitude sensitivity test, EFAST) was applied to the Feddes module of the HYDRUS-1D model, and the sensitivity indices including both main and total effects of actual root water uptake ...
Wenzhi Zeng +5 more
core +1 more source
In this study, the performance of the modified soil moisture analytical relationship (MSMAR) in concurrent estimation of deep soil moisture (DSM), evapotranspiration (ET), and deep percolation (DP) derived from surface soil moisture (SSM) variations on a
Naghedifar S. M. +8 more
core +1 more source
[Objective] Precipitation is the main source of soil water in arid and semi-arid regions. By combining field observation and model simulation to study the regularity of rainfall infiltration, the soil water deficit can be mastered more systematically ...
LU Rui +7 more
doaj +1 more source

