Key hydrological and biogeochemical processes in terrestrial systems are tightly coupled and controlled by soil properties. Process rates are especially large and dynamic at the interfaces between critical zone compartments, i.e., soil, groundwater, plants, and the atmosphere, where coupled processes and feedbacks result in nonlinear responses. However, the failure of scientists to work effectively across […]
AGU Chapman Conference on Soil-mediated Drivers of Coupled Biogeochemical and Hydrological Processes Across Scales
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