This review discusses the causes and consequences of 'non‐equilibrium'water flow and
solute transport in large structural pores or macropores (root and earthworm channels …

In arable farming systems, the term 'subsoil'refers to the soil beneath the tilled or formerly
tilled soil horizon whereas the latter one is denoted as 'topsoil'. To date, most agronomic and …

Life on Earth is sustained by a small volume of soil surrounding roots, called the
rhizosphere. The soil is where most of the biodiversity on Earth exists, and the rhizosphere …

Soils are the product of the activities of plants, which supply organic matter and play a
pivotal role in weathering rocks and minerals. Many plant species have a distinct ecological …

In this research, we used the Revised Universal Soil Loss Equation (RUSLE) and
Geographical Information System (GIS) to predict the annual rate of soil loss in the District …

The rhizosphere differs from the bulk soil in a range of biochemical, chemical and physical
processes that occur as a consequence of root growth, water and nutrient uptake, respiration …

The disintegration of granite residual soil is especially affected by variations in physical and
chemical properties. Serious geologic hazards or engineering problems are closely related …

Experiments with plants in pots can be beset by several often-unrecognised artefacts. The
soil or other medium at the bottom of a freshly watered and drained pot is inevitably …

Soil function may be affected by crop** practices impacting the soil microbial community.
The effect of different phosphorus (P) fertilization rates (0, 20, or 40 kg P 2 O 5 ha− 1) on soil …

Soil ecosystems support a plethora of intertwined biophysical and biochemical processes.
Soil structure plays a central role in the formation and maintenance of soil biological activity …