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 …

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 …

The completely revised and updated edition of the classic guide to soil physics The revised
edition of an environmental soil science classic, Soil Physics, Sixth Edition presents updated …

The thermal conductivity of soil under a given set of conditions is most important as it relates
to a soil's microclimate. The early growth and development of a crop may be determined to a …

Substantial advances in the measurement of water content and bulk soil electrical
conductivity (EC) using time domain reflectometry (TDR) have been made in the last two …

The soil thermal properties—heat capacity (C), thermal diffusivity (α), and thermal
conductivity (λ)—are important in many agricultural, engineering, and meteorological …

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

Frozen soil thermal conductivity (λ eff) is a critical thermo-physical property that is required
for environmental, earth science, geotechnical and geo-environmental applications and …

Soil thermal property data, especially as a function of water content, are currently not readily
available. Demand for these data is, however, on the increase because of improvements in …

Stream temperature has long been recognized as an important water quality parameter.
Temperature plays a key role in the health of a stream's aquatic life, both in the water column …