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Soil Erosion Rates Via 210 Pb ex , 137 Cs and Usle Model in El Rmel Watershed, NE Tunisia

Bibliographic Data

ID21648744
AuthorsLilia Ben Cheikha (0000-0002-9933-5008, National Centre for Nuclear Sciences and Technologies (CNSTN) Sidi Thabet Tunisia, corresponding author), Amina Mabrouk El Asmi (0000-0003-3255-369X, Laboratory of Sedimentary Basins and Petroleum Geology (BSGP‐FST) University of Tunis El Manar Tunis Tunisia), Boubaker Askri (0000-0001-9020-6288, National Centre for Nuclear Sciences and Technologies (CNSTN) Sidi Thabet Tunisia), Mansour Oueslati (National Centre for Nuclear Sciences and Technologies (CNSTN) Sidi Thabet Tunisia), F Gharbi (0000-0003-0653-0515, King Faisal University), Rafla Attia (DG/ACTA‐Ministry of Agriculture Tunis Tunisia), Thabet Aouedi (National Centre for Nuclear Sciences and Technologies (CNSTN) Sidi Thabet Tunisia)
Year2025
Volume36
Issue6
Pages2125-2143
Publication date2025-04-15
Open AccessYes
TypeARTICLE
VenueLand Degradation and Development (JOURNAL)
Journal identifiersISSN: 1085-3278 • E-ISSN: 1099-145X
PublisherWiley (PUBLISHER • GB)
DOI10.1002/ldr.5488
OpenAlexW4407081745
LanguageEN
Citations received2
References cited86

Soil erosion is a severe environmental and agricultural phenomenon which can be accelerated with climate change and land use, particularly in the Mediterranean region. In Tunisia, studies on the spatial distribution of erosion and deposition patterns can help to effectively implement soil and water conservation practices. Accordingly, the main objective of this research was to estimate soil erosion rates in two cultivated soils (SE1 and SE2), at El Rmel watershed of northeastern Tunisia. Three different time scales were observed via three tools, the 137 Cs, the 210 Pb ex radioisotopes and the USLE model. The FRN's conversion mass balance model 2 (MBM2) was used to convert activities into erosion rates. Based on the 137 Cs, 210 Pb ex , and USLE model, the mean erosion rates were, respectively, 37, 52, and 33 t ha −1 year −1 , at the cereal cultivated SE1 site and 4, 9, and 6 t ha −1 year −1 , at the olive tree cultivated SE2 site. It is supposed that the difference in time scale expressed by the three methods (100 years by 210 Pb ex , 60 years by 137 Cs, and 40 years by USLE), may have had a notable impact on the discrepancy in estimated erosion rates. The mean farm slope for SE1 and SE2 were, respectively, 14% and 8% and tillage was through three operations per year. Furthermore, the cereal crops site characterized by steep slopes show much higher erosion rates. Consequently, planting olive trees will be very helpful in reducing soil erosion and will be of great impact either environmentally and/or economically

Agronomy · Biology · Erosion · Geomorphology · Mediterranean climate · Soil water · Sowing · Tillage · Watershed · Aeolian processes and effects · Environmental Science · Hydrology and Watershed Management Studies · Soil erosion and sediment transport · Ecology · Geology · Soil Science

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Citations per year2
Citation span2026 - 2026 (1)
Highly citedNo

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