Using Beryllium-7 as a natural radionuclide for assessing short term soil erosion in arid agricultural land, Egypt. | ||||
| Arab Journal of Nuclear Sciences and Applications | ||||
| Article 10, Volume 55, Issue 2, April 2022, Page 94-103 PDF (876.7 K) | ||||
| Document Type: Original Article | ||||
| DOI: 10.21608/ajnsa.2021.91984.1505 | ||||
 View on SCiNiTO | ||||
| Authors | ||||
Mohamed Kassab   1; Ahmed Hegazi2; Mohamed Salem2; Moncef Benmansour3
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| 1Egyptian Atomic Energy Authority, Soils and water department, Nuclear Research Center, Cairo, Egypt. | ||||
| 2Department of Soils and Water Research, Nuclear Research Center, Egyptian Atomic Energy Authority, Cairo, Egypt. | ||||
| 3Water and Climate department, Centre National de l’Energie des Sciences et Techniques Nucléaires (CNESTEN), Rabat, Morocco | ||||
| Abstract | ||||
| The use of 7Be as a natural tracer for estimating soil erosion has been demonstrated as a promising tool. Erosion assessment was carried out using 7Be technique at an arid area of Egypt, located 35 km from Cairo upon a rain event of 54mm. The technique estimates soil erosion and deposition due to rainfall event by comparing 7Be activity concentration at a reference site and eroded or depositional sites. Soil samples were collected from three fields with different land uses, uncultivated, prickly pear field (Opuntia) and olives field (Olea europaea). The 7Be in the reference site was observed in the upper 14 mm of soil surface, the reference 7Be inventory value was 124 ±30 Bq.m-2. 7Be inventories of the uncultivated field was lower than the reference inventory and ranged from 59.9 to 122.5 ±30 Bq.m-2. The 7Be inventories in prickly pear field ranged from 89.5 to 296.6 ±30 Bq.m-2 showing erosion at upslope and deposition downslope each field, similar behavior was observed at olives field where 7Be inventories ranged from 73.9 to 263.6 ±30 Bq.m-2. Net soil erosion of 37, 4.1 and 17.9 (t. ha-1) were estimated for uncultivated soil, Prickly pear and olives, respectively. Combining these results with visual observations at the three fields, the main driving force of soil erosion and deposition processes by rain water was the hillslope topography. From the assumptions of applied technique, we can conclude that it gives robust evaluation of soil erosion due to rainfall. | ||||
| Keywords | ||||
| Soil erosion; Beryllium-7; Fallout radionuclide; Gamma spectrometry | ||||
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