Development of global soil erosion research at the watershed scale: a bibliometric analysis of the past decade

At the watershed scale, soil erosion is a cascading system that includes detachment-transport-deposition processes while sediment yield is the net balance of detachment and deposition at the watershed outlet. Due to the temporal-spatial variations of rainfall and landscapes, the relationships between soil erosion and sediment yield are complex and non-linear. Soil erosion processes and sediment yield at the watershed scale have attracted widespread attention; however, few systematic studies have been performed. In this study, a bibliometric analysis and visualization are used to understand the global research status of soil erosion and sediment yield at the watershed scale and provide a reference for researchers to establish future research directions. The USA and China were the most active contributors and had the most publications and active institutions, while Jean Poesen, D.E. Walling, and Xingmin Mu were the top three lead authors in this field. A keyword evolution analysis showed that determining the relationship between soil erosion and the watershed landscape and identifying the sediment source and off-site environmental and ecological effects caused by soil erosion have attracted considerable research attention. Additionally, significant progress has been made in the study of connectivity, and future research should integrate connectivity and soil erosion models to explain the soil erosion, sediment transport, and deposition processes at the watershed scale.

Automated summary

At the watershed scale, the relationship between soil erosion and sediment yield is complex and nonlinear due to temporal-spatial variations of rainfall and landscapes. While there has been widespread attention to soil erosion processes and sediment yield, systematic studies in this field are lacking. The study highlights the need to integrate connectivity and soil erosion models for a better understanding of erosion and sediment processes at the watershed scale.