This review evaluates research in the past 20 years focusing on groundwater nitrate removal
in the riparian zones of agricultural watersheds. Studies have reported a large range in the …

Infiltration rate affects slope stability by determining the rate of water transport to potential
failure planes. This note considers the influences of vegetation (grass and willow) …

Effects of plant growth on soil hydrological changes need to be considered for long-term
vegetation management of geotechnical infrastructure. Most existing studies focused on one …

Approximately 40% of total terrestrial precipitation transits the tiny volume of rhizosphere soil
around plant roots before being transpired, making it one of the most hydrologically active …

Wetland ecosystem, with their precious natural resources and important ecological
functions, is an integral part of the global ecosystem. Preferential flow is a form of water and …

How rainfall infiltration rate and soil hydrological characteristics develop over time under
forests of different ages in temperate regions is poorly understood. In this study, infiltration …

Macropores formed by roots are crucial channels for preferential flows in forest soils that are
largely responsible for water percolation and solute leaching. Using dual‐tracer experiments …

Saturated macropore flow is the dominant hydrological process in tropical and subtropical
hilly watersheds of northeast India. The process of infiltration into saturated macroporous …

Understanding and modeling both flow and solute transport within heterogeneous soils,
such as a macroporous soil, are of primary concern nowadays in tackling the problem of …

Macropores are subsurface connected void spaces caused by processes such as fracture of
soils, micro‐erosion, and fauna burrows. They are common near streams (eg hyporheic and …