Variations in saturated hydraulic conductivity and microstructural characteristics of loess, paleosol, and their contact zone under seepage conditions | Synapse
March 3, 2026
Variations in saturated hydraulic conductivity and microstructural characteristics of loess, paleosol, and their contact zone under seepage conditions
Key Points
Hydraulic conductivity varies significantly between soil types, affecting water movement.
The study notes distinct differences in microstructural characteristics at soil interfaces.
Comprehensive analysis was conducted under controlled seepage conditions to understand hydraulic behavior.
Understanding these variations may improve soil management practices and groundwater modeling.