N.J. Sathe,
Y.V. Bachhav,
N.T. Rajput,
H.H. Ansari,
S.D. Yadav,
R.R. Kumbhar,
S.R. Vare,
S.B. Ghadage,
- Faculty, Department of Civil Engineering, Rajgad Dnyanpeeth Technical Campus, Shri Chhatrapati Shivajiraje College of Engineering, Dhangawadi, Bhor,Pune, Maharashtra, India
- Faculty, Department of Civil Engineering, Rajgad Dnyanpeeth Technical Campus, Shri Chhatrapati Shivajiraje College of Engineering, Dhangawadi, Bhor,Pune, Maharashtra, India
- Student, Department of Civil Engineering, Rajgad Dnyanpeeth Technical Campus, Shri Chhatrapati Shivajiraje College of Engineering, Dhangawadi, Bhor,Pune, Maharashtra, India
- Student, Department of Civil Engineering, Rajgad Dnyanpeeth Technical Campus, Shri Chhatrapati Shivajiraje College of Engineering, Dhangawadi, Bhor,Pune, Maharashtra, India
- Student, Department of Civil Engineering, Rajgad Dnyanpeeth Technical Campus, Shri Chhatrapati Shivajiraje College of Engineering, Dhangawadi, Bhor,Pune, Maharashtra, India
- Student, Department of Civil Engineering, Rajgad Dnyanpeeth Technical Campus, Shri Chhatrapati Shivajiraje College of Engineering, Dhangawadi, Bhor,Pune, Maharashtra, India
- Student, Department of Civil Engineering, Rajgad Dnyanpeeth Technical Campus, Shri Chhatrapati Shivajiraje College of Engineering, Dhangawadi, Bhor,Pune, Maharashtra, India
- Student, Department of Civil Engineering, Rajgad Dnyanpeeth Technical Campus, Shri Chhatrapati Shivajiraje College of Engineering, Dhangawadi, Bhor,Pune, Maharashtra, India
Abstract
The Varandha Ghats pans approximately 14.62 km 2 , where changes in temperature, vegetation, topography, and soil characteristics are causing continuous soil erosion. Catchment heterogeneity and climatic variations cause spatial variability in hydrological processes. Differences in land use, soil type, topography, and rainfall patterns influence how water moves and accumulates across regions, resulting in diverse hydrological responses. This complexity challenges accurate modeling and effective water resource management strategies across variable landscapes. This study applies Geographic Information System (GIS) techniques to divide the watershed into nearly uniform sub-regions for analysis. Soil erosion is evaluated using the Revised Universal Soil Loss Equation (RUSLE) model, which considers a number of variables, including crop cover (C), slope length (LS), rainfall erosivity (R), soil erodibility (K), and conservation practices (P). These parameters are extracted from various surface features, analyzed, and presented in raster format. The results highlight sediment distribution across the watershed and the sediment yield at the outlet.
Keywords: GIS, RUSLE, soil erosion, soil erodibility, slope length, spatial analysis
[This article belongs to Journal of Remote Sensing & GIS ]
N.J. Sathe, Y.V. Bachhav, N.T. Rajput, H.H. Ansari, S.D. Yadav, R.R. Kumbhar, S.R. Vare, S.B. Ghadage. Estimation of Soil Erosion Using GIS in Pune District, Maharashtra. Journal of Remote Sensing & GIS. 2025; 16(02):26-33.
N.J. Sathe, Y.V. Bachhav, N.T. Rajput, H.H. Ansari, S.D. Yadav, R.R. Kumbhar, S.R. Vare, S.B. Ghadage. Estimation of Soil Erosion Using GIS in Pune District, Maharashtra. Journal of Remote Sensing & GIS. 2025; 16(02):26-33. Available from: https://journals.stmjournals.com/jorsg/article=2025/view=223083
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Journal of Remote Sensing & GIS
| Volume | 16 |
| Issue | 02 |
| Received | 12/04/2025 |
| Accepted | 01/05/2025 |
| Published | 10/07/2025 |
| Publication Time | 89 Days |
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