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Analysis of the Relationship between Sediment Budget Components and Topographic Metrics at the Hillslope Scale in Control Sub-watershed of the Khamsan Representative-paired Watershed | ||
| پژوهش های آبخیزداری | ||
| Article 8, Volume 38, Issue 2 - Serial Number 147, July 2025, Pages 118-138 PDF (1.05 M) | ||
| Document Type: Research | ||
| DOI: 10.22092/wmrj.2025.367713.1602 | ||
| Authors | ||
| Reza Zarei1; Abdulvahed Khaledi Darvishan* 2; Mohamad Reza Zare3; Paolo Potro4 | ||
| 1Former Ph.D. Student, Department of Watershed Management, Faculty of Natural Resources, Tarbiat Modares University, Iran | ||
| 2Associate Professor, Department of Watershed Management, Faculty of Natural Resources, Tarbiat Modares University, Noor, Iran | ||
| 3Associate Professor, Department of Physics, Faculty of Sciences, University of Isfahan, Isfahan, Iran | ||
| 4Professor, Department of Agraria, University Mediterranea of Reggio Calabria, Italy | ||
| Abstract | ||
| Introduction and Goal Given the critical importance of soil and humanity's reliance on it for food production worldwide, especially in developing countries, one of the most important and fundamental problems today is soil erosion and degradation. The average soil erosion in the country is estimated to be around 16.5 tons per hectare, and soil erosion in Iran is approximately 2 to 2.5 times higher than the average in Asia and 5 to 6 times higher than the global average, predominantly occurring in slopes and hilly areas due to poor vegetation cover. Considering the advancements and development of erosion and sediment methods, along with the costs and lack of accuracy in traditional methods such as the use of erosion pins and plots, the use of radionuclides, especially 137Cs, for measuring the amount of erosion and deposition and sediment budget components is of great importance today. One of the important advantages of these methods, which has attracted the attention of researchers especially in recent decades, is the possibility of measuring soil redistribution due to water erosion in slopes and watersheds and even on the scale of laboratory plots. Accurately estimation of sediment budget components is essential for estimating erosion rates and planning effective soil conservation measures in any region. Therefore, this research aims to estimate the sediment budget components at the hillslope scale using topographic metrics. Materials and Methods Due to the possibility of using the results of previous researches and the availability of a digital elevation model with a spatial accuracy of one meter obtained from a drone photogrammetry, the present study was conducted in the control sub-watershed of the Khamsan representative paired watershed in Kurdistan province. To investigate the effect of the slope angle and curvature on erosion and sedimentation, soil sampling was done at 31 points in a 200-m grid with a systematic-random method and also at 48 points on six transects. After preparation of the soil samples including air and freeze drying and passing through a 63-micron sieve, 293 grams of soil were sent to the laboratory in special containers for the measurement of 137Cs. Also, distribution maps of topographic metrics were extracted using the digital elevation model in ArcGIS 10.8 software. Then, a distribution map of soil erosion/redistribution was prepared using the 137Cs inventory points and work unit approach. Additionally, the components of the sediment budget including total erosion, total sedimentation, net erosion and sediment delivery ratio were calculated for 14 hillslopes in the studied sub-watershed. Then, in order to check the normality of the data in the 14 studied hillslopes, the Kolmogorov Smirnov test was used, and according to the normality of the data, the correlation between the topographic metrics and the sediment budget components at the hillslope scale was checked using the Pearson correlation test. Finally, regression equations were presented to estimate the sediment budget components using topographic metrics. Results and Discussion According to the results of this study on the 14 studied hillslopes, specific total erosion ranged from 0.93 to 7.52 t ha-1yr-1, while the specific total deposition ranged from 0.03 to 0.51 t ha-1yr-1. These findings indicated that a significant percentage of erosion had been exported from the hillslopes. Specific net erosion was also calculated between 0.79 and 7.45 t ha-1 yr-1, which indicates the sediment delivery ratio between 0.84 and 1.00 for the investigated hillslopes. The results indicate that the correlation between erosion (total and net) and sediment delivery ratio with slope angle, topographic factor, and stream power index is significant and negative. These findings indicate the dominant effect of dryland farming on increased erosion in gentler slopes and downstream areas, in the upstream regions of the slopes, although the slope was steeper, erosion was minimal due to less soil disturbance and rangeland usage. Consequently, in this study, the interpretation of relationships and regression equations utilized the results of land use and its changes along the slope profile. Conclusion and Suggestions The inner area of the Khamsan watershed includes a low-slope plain with the predominant land use of rainfed agriculture, which continues to parts of the surrounding steep slopes, and similar conditions can be seen in the sub-watersheds, including the control sub-watershed. The conditions of land use changes from the upstream to the downstream of the hillslopes around the rainfed lands have relatively similar. Therefore, the regression equations presented in this study are applicable in the hillslopes of the Khamsan representative paired watershed and other similar watersheds. Finally, it is suggested to extract topographical metrics using digital height models with different spatial accuracies and use them in estimations. It is also recommended that a land management plan be developed for the studied area, taking into account the significant role of land use in erosion and sediment production, with adjustments and land use changes implemented based on the potential of each section. | ||
| Keywords | ||
| Net erosion; sediment delivery ratio; slope curvature; soil redistribution; topographic wetness index | ||
| References | ||
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