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Application of Geographic Information System (GIS) to study the influence of the groundwater irrigation on salt accumulation in the soils of Sohag governorate

机译:应用地理信息系统(GIS)研究Sohag省的地下水灌溉对土壤盐分累积的影响

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Sohag governorate is located in Upper Egypt (about 467 Km south Cairo city) in a narrow long strip of cultivated area. The total maximum length of Sohag governorate is about 96 Km and the maximum width is about 25 Km. Sixteen transects were selected, crossing the Nile valley and extending from the eastern to the western desert covering the area understudy. Two locations on each side of the river from each transect whenever it is possible. Soil and water samples were selected to study physical and chemical properties of soils and water wells, to identify effect groundwater irrigation on salt accumulation in this area with a special reference to their taxonomic units. The obtained data reveal that the values of electrical conductivity, (ECw) varied from well to another. The ECw values of well waters range from 8020 μS/cm to 500 μS/cm. In soil samples, The ECe reached a maximum value of 8.23 dS/m and 10.85 dS/m for surface and subsurface soils respectively. However, the lowest value was 0.36 dS/m and 0.43 dS/m for surface and subsurface soils respectively. The salinity is increase with depth in most cases. The correlation coefficients between the electrical conductivity of the groundwater (ECw) and the saturated soil extract (ECe) are positive. The groundwater pH value ranges between 7.78 and 8.83. The pH values of the surface and subsurface soils samples are over than 8. The soluble potassium range from 0.05 to 0.62 meq/le in groundwater. But, in the soil samples the soluble potassium values ranged from 0.08 to 0.61 meq/le and from 0.09 to 0.65 meq/le for the surface and subsurface soil samples respectively. Sodium values in the groundwater had a range of 2.11 to 48.19 meq/l.It is ranged from 1.20 to 67.08 meq/le and 3.00 to 60.28 meq/le for the surface and subsurface soils samples respectively. Calcium values in the groundwater are varying from 0.86 to 10.60 meq/l. It is values ranged from 0.06 to 10.33 meq/le and 0.20 to 16.00 meq/le for the surface and subsurface soil samples respectively. Magnesium values in the groundwater ranged from 0.40 to 7.60 meq/l. Soluble magnesium values had a range of 0.20 to 10.40 meq/le and 0.20 to 8.79 meq/le for the surface and subsurface soil samples respectively. Chlorides values in the groundwater ranged from 1.19 to 45.00 meq/l. It is values ranged from 0.29 to 46.84 meq/le and 0.8 to 30.20 meq/le for the surface and subsurface soil samples respectively. Soluble sulphates values in the groundwater ranged from 0.92 to 16.20 meq/l. It is values ranged from 0.41 to 31.25 meq/le and 0.32 to 29.15 meq/le for the surface and subsurface soil samples respectively. Carbonates and bicarbonate values in the groundwater ranged from 1.33 to 15.60 meq/l. It is values ranged from 0.75 to 19.20 meq/le and 0.8 to 18.40 meq/le for the surface and subsurface soil samples respectively. SAR values in the groundwater ranged from 1.56 to 18.48. In the surface and subsurface soil samples, SAR values had a range of 1.16 to 48.09 and 2.73 to 51.15 respectively. RSC values in the groundwater reached high from 0.00 to 5.60. SSP values in groundwater ranged from 27.62 % to 83.43 %. In the surface and subsurface soil samples, SSP values had a range of 10.88 % to 95.16 % and 45.88 % to 95.64 % respectively. Calcium carbonate values in the surface and subsurface soil samples range between 0.04 to 37.39% and 0.09% to 29.57% respectively. The soil survey of area understudy identified medium to coarse textured soils .The soil under consideration were classified according to Soil Taxonomy as: Typic Torripsamments, Typic Torrorthents, Sodic Torrorthents, Typic Hplocalcids and Typic Natrargids.
机译:Sohag省位于上埃及(开罗市以南约467公里),耕地狭长。 Sohag省的总最大长度约为96 Km,最大宽度约为25 Km。选择了16个样带,这些样带穿过尼罗河谷,从东部到西部沙漠延伸,覆盖了被研究地区。只要有可能,每个横断面都在河流两边的两个位置。选择土壤和水样来研究土壤和水井的物理和化学特性,以特别参考其分类单位来确定地下水灌溉对该地区盐分累积的影响。所获得的数据表明,电导率(ECw)的值随井的不同而变化。井水的ECw值范围为8020μS/ cm至500μS/ cm。在土壤样品中,表层和地下土壤的ECe最大值分别达到8.23 dS / m和10.85 dS / m。然而,表层和地下土壤的最低值分别为0.36 dS / m和0.43 dS / m。在大多数情况下,盐度随深度增加。地下水(ECw)和饱和土壤提取物(ECe)的电导率之间的相关系数为正。地下水的pH值介于7.78和8.83之间。表层和地下土壤样品的pH值超过8。地下水中的可溶性钾含量在0.05到0.62 meq / le之间。但是,在土壤样品中,表层和地下土壤样品的可溶性钾值分别为0.08至0.61 meq / le和0.09至0.65 meq / le。地下水中的钠含量范围为2.11至48.19 meq / l,表层和地下土壤样品的钠含量范围分别为1.20至67.08 meq / le和3.00至60.28 meq / le。地下水中钙的含量从0.86到10.60 meq / l不等。表层和地下土壤样品的取值范围分别为0.06至10.33 meq / le和0.20至16.00 meq / le。地下水中的镁含量范围为0.40至7.60 meq / l。表层和地下土壤样品的可溶性镁值分别为0.20至10.40 meq / le和0.20至8.79 meq / le。地下水中的氯化物值范围为1.19至45.00 meq / l。表层和地下土壤样品的取值范围分别为0.29至46.84 meq / le和0.8至30.20 meq / le。地下水中的可溶性硫酸盐值为0.92至16.20 meq / l。表层和地下土壤样品的取值范围分别为0.41至31.25 meq / le和0.32至29.15 meq / le。地下水中的碳酸盐和碳酸氢盐值范围为1.33至15.60 meq / l。表层和地下土壤样品的取值范围分别为0.75至19.20 meq / le和0.8至18.40 meq / le。地下水的SAR值介于1.56至18.48之间。在表层和地下土壤样品中,SAR值分别在1.16至48.09和2.73至51.15之间。地下水中的RSC值从0.00升高到5.60。地下水中的SSP值介于27.62%至83.43%之间。在表层和地下土壤样品中,SSP值的范围分别为10.88%至95.16%和45.88%至95.64%。表层和地下土壤样品中的碳酸钙值分别在0.04至37.39%和0.09%至29.57%之间。待调查区域的土壤调查确定了中等至粗糙的纹理土壤。根据土壤分类法,所考虑的土壤分类为:典型龟甲,典型龟甲,南部龟甲,典型Hplocalcids和典型Natrargids。

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