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Impact of Flood Spreading on Infiltration Rate and Soil Properties in an Arid Environment

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  • Reza Ghazavi
  • Abbasali Vali
  • Saeid Eslamian

Abstract

Flood spreading (FS) is one of the suitable methods for flood management and water harvesting that increases the groundwater recharge, makes soil more fertile and increases nutrients in soil. It is also a method for reusing sediment, which is usually wasted. The purpose of this paper is to investigate the impact of flood spreading on physical and chemical soil properties (soil texture, infiltration rate, pH, EC, Na, P, K, Ca, Mg, Cl, HCO 3 , and SO 4 ). It is examined that the soil properties change in the flood spreading projection area (FSP). The physico-chemical properties of soil and infiltration rate were measured in different soil depths at both flood spreading and control area. For the 20 cm of top soil, the amount of clay increased after the flood spreading implementation especially in the first and second dikes. Increasing clay was accompanied by decreasing soil infiltration and sand percentage. The mean differences of the clay, sand and infiltration rate between FSP and the control area were statistically significant (P > 0.01). A significant difference was not observed in 20–30 cm of the depth. Soil pH, Mg, HCO 3 , Cl and SO 4 in different soil layers did not show any significant difference between the control and FSP. Soil EC in 0–20 cm depth of FSP and control area was showed a significant difference (P > 0.05) but no significant differences were found in deeper layers (P > 0.05). K, Na and Ca were remarkably different between 0 and 10 cm depths (P > 0.05) whereas no significant differences were found in deeper layers (P > 0.05). Comparison of the physico-chemical properties and infiltration rates between the dikes in the FSP shows that there are the significant differences between the medians of dike 1 with dikes 2, 3, 4 and 5, but the differences were not observed between dikes 3, 4 and 5. Our results show that the flood spreading operation can be influenced by the area that is under this operation. This study allowed us to investigate the mechanisms that regulate the infiltration rate and chemical soil properties throughout a seasonally flooded area. Copyright Springer Science+Business Media B.V. 2010

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  • Reza Ghazavi & Abbasali Vali & Saeid Eslamian, 2010. "Impact of Flood Spreading on Infiltration Rate and Soil Properties in an Arid Environment," Water Resources Management: An International Journal, Published for the European Water Resources Association (EWRA), Springer;European Water Resources Association (EWRA), vol. 24(11), pages 2781-2793, September.
    • Handle: RePEc:spr:waterr:v:24:y:2010:i:11:p:2781-2793
    DOI: 10.1007/s11269-010-9579-y
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    References listed on IDEAS

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    2. R. Ghazavi & A. Vali & S. Eslamian, 2012. "Impact of Flood Spreading on Groundwater Level Variation and Groundwater Quality in an Arid Environment," Water Resources Management: An International Journal, Published for the European Water Resources Association (EWRA), Springer;European Water Resources Association (EWRA), vol. 26(6), pages 1651-1663, April.
    3. Soha A. Mohamed & Mohamed E. El-Raey, 2020. "Vulnerability assessment for flash floods using GIS spatial modeling and remotely sensed data in El-Arish City, North Sinai, Egypt," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 102(2), pages 707-728, June.
    4. Hydar Ebrahimi & Reza Ghazavi & Haji Karimi, 2016. "Estimation of Groundwater Recharge from the Rainfall and Irrigation in an Arid Environment Using Inverse Modeling Approach and RS," Water Resources Management: An International Journal, Published for the European Water Resources Association (EWRA), Springer;European Water Resources Association (EWRA), vol. 30(6), pages 1939-1951, April.

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