Analysis of hydraulic conductivity characteristics of alluvial sequence in North China Plain

Hydraulic conductivity is a basic property of rocks and soil, and its estimation varies as a function of the scale and purpose of the study. This work combines geomorphological analysis, geological data, and groundwater investigations from literature to assess large-scale anisotropies in hydraulic conductivity in the North China Plain. The study area encompasses 144,000 km2 and represents the most important groundwater system of China, affected...