Weathering in the Ganga Alluvial Plain: Geochemical signatures linking of the Himalayan source and the Bay of Bengal sink (original) (raw)

This study investigates the geochemical signatures of river sediments in the Ganga Alluvial Plain, focusing on the Gomati River, which plays a crucial role in recycling Himalayan-derived sediments. Notably, the Gomati River has significantly elevated dissolved Sr and Se concentrations compared to average values, highlighting its impact on the Ganga River's geochemistry. The research emphasizes the need to consider monsoon-controlled hydro-geochemical processes in the Ganga Alluvial Plain to enhance understanding of the elemental mobility and cycling associated with the Ganga Fluvial system.