Geomorphic Control on Soil Erosion – a Case Study in the Subarnarekha Basin, India

Abstract

<p>Geomorphology depicts the qualitative and quantitative characteristics of both terrain and landscape features combined with the processes responsible for its evolution. Soil erosion by water involves processes, which removes soil particles and organic matter from the upper sheet of the soil surface, and then transports the eroded material to distant location under the action of water. Very few studies have been conducted on the nature and dynamics of soil erosion in the different geomorphologic features. In the present investigation, an attempt has been made to assess the control of geomorphologic features on the soil loss. Universal Soil Loss Equation (USLE) was used to determine soil loss from the various geomorphological landforms. Principal component analysis (PCA) was implemented on the USLE parameters to determine the degree of association between the individual principal components and the USLE-derived soil loss. Results obtained from the investigation signify the influence of the various landforms on soil erosion. PC5 is found to be significantly correlated with the USLE-derived soil loss. The results ascertained significant association between the soil loss and geomorphological landforms, and therefore, suitable strategies can be implemented to alleviate soil loss in the individual landforms.</p>

Soil Deformation after Water Drop Impact—A Review of the Measurement Methods

“…The nature of the erosion phenomena affects the way they are studied. Erosion research has been carried out on a large scale, including the study of mass transport and processes in entire catchments [ 18 , 19 , 20 , 21 , 22 ]. On the other hand, with the development of measurement techniques, the scope of possible micro-scale laboratory tests has also increased.…”