Research news on soil moisture

Soil moisture is the quantity of water contained within the unsaturated zone of soil, typically expressed as volumetric water content or gravimetric water content, and is a central variable in hydrology, agronomy, and land–atmosphere interaction studies. It governs soil hydraulic conductivity, matric potential, and the partitioning of precipitation into infiltration, runoff, and evapotranspiration. Soil moisture strongly regulates plant water availability, microbial activity, and biogeochemical cycling, and is measured using in situ sensors (e.g., time-domain reflectometry, capacitance probes), lysimeters, or remotely sensed estimates from microwave and thermal observations. It is a key state variable in land surface models, drought monitoring systems, and climate and weather prediction frameworks.

How cracks in dry soil impact moisture evaporation

Soils that are exposed to prolonged drought often develop desiccation cracks, which impact soil properties and exacerbate moisture loss through evapotranspiration. Now, a study from the University of Illinois Urbana-Champaign ...

Why forest loss is making our watersheds leak rain

It's a well-established fact that forests and water are deeply connected. For decades, paired-watershed experiments—a scientific method for evaluating land-use impacts on water quantity or quality—have shown that when we ...

Watering smarter, not more: A modern-day robotic divining rod

Advanced technology can help farmers get to the root of a growing problem—overwatering in an era of increasing drought and water scarcity. A new UC Riverside system can map soil moisture tree by tree, so growers water only ...

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