利用现代技术对埃及西北沿海地区选定区域的水土资源进行了研究

E. Hussien, M. S. Ahmed, W. M. Omran
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引用次数: 0

摘要

研究区东起Minqar Alousran,西至Beer Qaaem,北至Marsa Matrouh,南至Jable Khaled。研究总面积约为345563.52 Fadden。选取了代表地貌单元的98个土壤剖面。土地评价采用定性方法。获得了水文和地貌特征。确定了4个主要地貌单元:滨海平原、北部高原、南部高原和利比亚高原。土壤从很浅到很深不等。主要的土壤质地介于砂质粘土壤土和砂土之间。这些土壤是中度至极钙化的。这些土壤呈微碱性到强碱性。研究的地貌单元土壤分为:石质单钙质、典型单钙质、典型钙质、石质单钙质、石质单钙质和氧水钙质。研究区土壤的土地评价。该研究还旨在预测年峰值流量和径流水量,以及20年、10年、5年、3年和2年的回归期。结果表明,El-Hraka盆地面积178.31km2,长33.70 km,周长132.8 km,缓坡0.012 m/m。研究流域的土地利用/土地覆盖类型有4种,分别为农用地、裸地、岩石区和城市,分别占盆地总面积的3.45%、92.98%、3.41%和0.16%。根据土壤质地的不同,研究流域分为A、C两个水文土壤类群。曲线数(CN)取决于土地利用/土地覆盖和水文土壤类型。El-Hraka盆地的平均值为73.67。年径流量10583.29 m3,补给地下水库。年入渗量为8195.01m3。重现期20年、10年、5年、3年和2年的洪峰流量分别为29.24、17.98、9.50、3.78和0.75 m3/s。研究流域20年、10年、5年、3年和2年回归期径流量分别为278万m3、171万m3、906,578.6、359,883和69,989.4 m3。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
EMPLOYING MODERN TECHNIQUES IN STUDYING SOIL AND WATER RESOURCES IN SELECTED AREA OF NORTH WESTERN COASTAL REGIONS, EGYPT
The study area is extending from Minqar Alousran at the east to Beer Qaaem at the west, Marsa Matrouh at the north to Jable Khaled at the south. The total studied area is about 345563.52 Fadden. Ninety eight soil profiles were selected representing the geomorphic units. The qualitative approach was used to land evaluation. Hydrological and morphometric characteristics have been obtained. Four main geomorphic units were identified: Coastal Plain, Northern Plateau, Southern Plateau and Lybian Plateau. The soils ranged from very shallow to very deep. The dominant soil texture is between sandy clay loam to sand. These soils are moderately to extremely calcareous. These soils are slightly to strongly alkaline. The studied soils in the geomorphic units are classified as follow:  Lithic Haplocalcids, Typic Haplocalcids, Typic Torriorthents, Gypsic Aquisalids, Typic Calcigypsids, Lithic Torriorthents and Oxyaquic Torripsamments. Land evaluation for the studied soils. The study aimed also to predict annual peak flow and runoff water volume, as well as the 20, 10, 5, 3, and 2year return periods. Results referred that El-Hraka basin characterized by an area of 178.31km2, basin length of 33.70 km, perimeter of 132.8 km, and gentle slope of 0.012 m/m. There are four types of land use/land cover in the study basin named: agriculture land, bare land, rocky areas and urban representing 3.45, 92.98, 3.41 and 0.16% of El Hraka basin, respectively. There are two hydrologic soil group of the study basin A and C depending on the soil texture. The Curve Number (CN) depending on the land use / land cover and the hydrologic soil groups. Its average values are 73.67 for El-Hraka basin. The annual runoff water volumes are 10583.29 m3 that recharge the groundwater reservoir. However, the annual infiltration volumes are 8195.01m3. The peak flow of the 20, 10, 5, 3 and 2 year return periods flash flood is 29.24, 17.98, 9.50, 3.78 and 0.75 m3/s respectively. The runoff volume of the 20, 10, 5, 3 and 2 year return-periods is 2.78 million, 1.71 million, 906,578.6, 359,883and 69,989.4 m3 respectively for the study basin.
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