Soil moisture (SM) is a key hydrologic state variable that is of significant importance for
numerous Earth and environmental science applications that directly impact the global …

Improving soil physical properties is important to soil conservation. Cover cropping can
improve soil physical properties and organic matter content which can reduce soil loss, and …

At the watershed scale, soil moisture is the major control for rainfall–runoff response,
especially where saturation excess runoff processes dominate. From the ecological point of …

Heat carried by ground water serves as a tracer to identify surface water infiltration, flow
through fractures, and flow patterns in ground water basins. Temperature measurements …

The HYDRUS numerical models are widely used for simulating water flow and solute
transport in variably saturated soils and groundwater. Applications involve a broad range of …

Vapor movement is often an important part in the total water flux in the vadose zone of arid
or semiarid regions because the soil moisture is relatively low. The two major objectives of …

We present a method for determining streambed seepage rates using time series thermal
data. The new method is based on quantifying changes in phase and amplitude of …

Significant spatial and temporal variability of water fluxes may exist at the river–groundwater
interface and the assessment of such variability may be important for appreciation of the …

Accurate and continuous measurements of soil thermal and hydraulic properties are
required for environmental, Earth and planetary science, and engineering applications, but …

The dynamic distribution of thermal conditions present in saturated near-surface sediments
have been widely utilised to quantify the flow of water. A rapidly increasing number of …