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.