Reliable quantitative information on sediment sources to rivers is critical to mitigate
contamination and target conservation and restoration actions. However, for large-scale …

The time of concentration (Tc) is the main hydrological parameter used to characterize the
response of a given Hydrological Response Unit (HRU) to a precipitation event. Because of …

Nitrogen (N) contamination within agricultural‐karst landscapes and aquifers is widely
reported; however, the complex hydrological pathways of karst make N fate difficult to …

Excessive sediment loss degrades freshwater quality and is prone to further elevation and
variable source contributions due to the combined effect of extreme rainfall and differing …

The structural controls of sediment connectivity are poorly understood in low-gradient
watersheds and stream networks. We developed a field-and modeling-based framework to …

Carbon and nitrogen stable isotopic ratios are increasingly used in sediment fingerprinting
studies. However, questions remain regarding tracer conservativeness during sediment …

Hydrologic controls on the timing of sediment transport and sediment hysteresis patterns
remain an open area of investigation in hydrology, especially for low-gradient watersheds …

Coupling erosion formulae with sediment connectivity methods is one promising approach
to better represent structural and functional variability of sediment processes. To advance …

Soil organic matter (SOM) loss in agricultural watersheds driven by hydrology threatens the
aquatic environment, and increases the risk of greenhouse gas emissions from aquatic …

Soil runoff and sediment transport are considered as an important vector for particle-bound
contaminant transfer from source to receiving waters. Under changing climate conditions …