Jiri Simunek

TL;DR: Soil Solid Phase Introduction Soil Phases Soil Texture Soil Mineralogy Soil Structure Summary Derivations Problems Soil Water Content and Potential Introduction Energy and Work Properties of Bulk Water Properties of Water at Air and Solid Interfaces Soil water content Measuring SoIL Water Content SoIL water potential Measuring SOIL Water Potential Components The SoilWater Retention Curve RETC Program Summary Deriversations Problems Steady Water Flow in Soils Introduction Steady Flow in Saturated Soil Steady flow in Unsaturated Soils Measurements of Hydraulic Properties Summary Derivation

TL;DR: The results imply that AgNPs were largely irreversibly interacting in a primary minimum associated with microscopic heterogeneity.

TL;DR: Column experiments were conducted with undisturbed loamy sand soil under unsaturated conditions to investigate the retention of surfactant stabilized silver nanoparticles (AgNPs) with various input concentration, flow velocity, and ionic strength, and the remobilization of AgNPs by changing the cation type and IS.

TL;DR: In this paper, a mathematical model for colloid transport and retention in saturated porous media under unfavorable attachment conditions is presented, which is qualitatively consistent with observed trends for retention with colloid size and concentration, grain size, and velocity.

TL;DR: Results indicated that sorption of high explosives was rate limited, and use of parameters specific to formulations will improve fate and transport predictions.