Modeling Interactions and Dynamic Saturation Processes in Karst Media
Abstract The simulation of karst aquifers is highly challenging due to complex conduit‐matrix interactions. This study utilizes KarstFOAM, a high‐fidelity, physics‐based numerical model, to address these challenges. KarstFOAM integrates (a) a unified single‐domain Forchheimer–Darcy–Brinkman–Stokes (FDBS) formulation that transitions naturally across ...
F. Huang +5 more
wiley +1 more source
Effect of suction stress on the strength of rupture zone and stability of landslide. [PDF]
Wang J, Su A, Liu Q, Zou Z.
europepmc +1 more source
Abstract Evapotranspiration (ET) and groundwater recharge are fundamental components of the terrestrial water cycle, critical for understanding land–atmosphere interactions, ecosystem dynamics, and climate feedbacks. However, large‐scale mapping of these fluxes is hindered by sparse in situ observations and uncertainties in land surface models.
Asif Mahmood, Leila Farhadi
wiley +1 more source
Effects of wet-dry cycles on the bimodal soil-water characteristic curve and unsaturated permeability of granite residual soil. [PDF]
Zhang Y, Gu K, Dou H, Wu Y, Li L.
europepmc +1 more source
Evaporation‐Induced Hysteresis in Surface Water‐Groundwater Exchange in Wetlands
Abstract Evaporation is a major pathway of surface water loss in wetlands, yet its influence on subsurface feedbacks remains poorly understood. Using an integrated surface–subsurface hydrologic and solute transport model, we show that evaporation can induce hysteresis between evaporative demand and the upwelling of groundwater and solutes, with the ...
Chen Ding +4 more
wiley +1 more source
Mucilage facilitates root water uptake under edaphic stress: first evidence at the plant scale. [PDF]
Abdalla M, Carminati A, Cai G, Ahmed MA.
europepmc +1 more source
Soil Structure and Mixing Controls on Water‐Rock Contact: Implications for Enhanced Weathering
Abstract Enhanced weathering (EW), the addition of finely ground silicate rock powder (RP) to soil, has emerged as a promising carbon removal strategy. However, quantifying weathering rates in soils remains challenging, as most continuum‐scale EW models do not adequately account for the fraction of RP surface area (SA) that is wet at a given soil ...
Shashank Kumar Anand +3 more
wiley +1 more source
Simultaneous determination of soil-water characteristic and shrinkage curves of consolidated kaolin under continuous and discrete drying procedures. [PDF]
Liu H, Rahardjo H, Li Y.
europepmc +1 more source
Abstract Seepage boundary conditions are commonly used in groundwater simulations to allow groundwater to discharge at the upper surface of the model when groundwater head exceeds atmospheric pressure. However, the extent and transient behavior of the seepage zone are often unknown a priori and difficult to predict.
Young‐Jin Park +7 more
wiley +1 more source
Sustainable shear behavior of clayey sand reinforced with recycled PET strips under moisture variation. [PDF]
Zerarka M +7 more
europepmc +1 more source

