Core Ideas To determine the water retention curve from inverse modeling, θ and ψ need to
be monitored. δ18O ratios contained information to inversely estimate soil hydraulic …

Surface reactive phases of soils and aquifers, comprised of phyllosilicate and metal
oxohydroxide minerals along with humic substances, play a critical role in the regulation of …

Dispersivity (α) is a required input parameter in solute‐transport models based on the
advection‐dispersion equation (ADE). Normally α is obtained from miscible‐displacement …

Recently, significant advances have been made in the theory and application of acoustic
and electroacoustic spectroscopies for measuring the particle-size ( potential) of colloidal …

Bromide, Br−, adsorption behavior was investigated on amorphous Al and Fe oxide,
montmorillonite, kaolinite, and temperate and tropical soils. Bromide adsorption decreased …

The origin and residence time of brines in the Alberta Basin have been debated for more
than 40 years, with conflicting conclusions reported by geochemical and hydrogeologic …

The practitioner or researcher often faces complex alternatives when selecting a method to
characterize properties governing a soil process. After years of research and development …

Two subsurface samples representing highly weathered sediments of the Upper Coastal
Plain (Aiken, SC) that differed in Fe-oxide content (7.3 vs 35.9 g Fe kg-1) were evaluated in …

Dual‐permeability model simulations and sensitivity studies indicate that preferential solute
leaching in structured soil is intensified by a limited solute mass transfer between …

The hydrological and geochemical interactions between clay minerals and organic matter in
soils directly influence the reaction, behavior, and mobility of heavy metals in soils …