saturated mass water content and saturated hydraulic conductivity for different hulk densities were measured by the method of fixing bulk density of olefin. Effects of bulk density on the two parameters were analyzed. The results showed that saturated mass water content decreased with the increment of bulk density and was inverse to bulk density. Saturated hydraulic conductivity tended to diminish in power function when bulk density increased. The researches will provide appropriate function quantificetionally to build innovative frame on water movement theory for the soil with changing bulk density. It is helpful to utilize soil water resource reasonably.
Effect of Bulk Density on Soil Saturated Water Movement Parameters
Effects and Mechanisms of Vegetation Restoration Patterns on Soil Saturated Hydraulic Conductivity in Gully Catchment Areas of Loess Plateau
Response Characteristics of Soil Saturated Hydraulic Conductivity after Returning Orchard to Farmland on the Loess Plateau
Characteristics of Soil Saturated Hydraulic Conductivity and Its Influencing Factors at Different Landscape Positions in a Small Peak-Cluster Depression Watershed of the Karst Region
Effects of Biological Crust Development on Soil Saturated Hydraulic Conductivity in the Three Gorges Reservoir Area
Related Author
LU Dian-qing
SHAO Ming-an
LIU Chun-ping
XU Yin
YUAN Jiang
FU Suhua
LI Shuyi
YUAN Yaoyao
Related Institution
Faculty of Geographical Science, Beijing Normal University
State Key Laboratory of Earth Surface Processes and Hazards Risk Governance, Beijing Normal University
Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xian