Bed form‐induced hyporheic exchange flux (qH) is increasingly viewed as a key process
controlling water fluxes and biogeochemical processes in river networks. Despite the fact …

Streambed hydraulic conductivity is one of the main factors controlling variability in surface
water‐groundwater interactions, but only few studies aim at quantifying its spatial and …

The change of vertical hydraulic conductivity (K^ sub v^) before and after a flood season is
crucial in understanding the long-term temporal variation of streambed permeability …

A detailed measurement of floodplain riverbank sediment hydraulic conductivity (K) is the
first step in analyzing the hydraulic relationship between streams and aquifers. Poyang Lake …

Spatial geostatistical interpolation of point measurements of streambed attributes in the
hyporheic zone may be constrained by the streambed anisotropy, and data density and …

This study focuses on the anisotropic hydraulic conductivity of a sandstone–mudstone
particle mixture. Permeameter tests were performed in the laboratory. The effects of the …

The hydraulic conductivity of intertidal sediments plays an important role in quantifying
seawater–groundwater interactions. However, its accurate and economical in situ evaluation …

Stream depletion is the reduction in flow rate in a stream due to pumping in an aquifer that is
hydraulically connected to the stream. We developed a semianalytical expression for stream …

剪切波速是反映土体动力学特性的重要参数之一. 受地质地貌和沉积环境的影响,
场地的近地表剪切波速可能存在明显的各向异性. 本研究利用克罗基特岩土台阵2 …

Prior to hydraulic engineering work, it is essential to know the geohydraulic properties of
river bed sediments as precisely as possible in order to predict and minimize potential …