首页> 外文期刊>Arabian journal of geosciences >The impact of the geologic setting on the Quaternary aquifer, El-Tur area, Southwest Sinai, Egypt
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The impact of the geologic setting on the Quaternary aquifer, El-Tur area, Southwest Sinai, Egypt

机译:地质环境对四季含水层,埃及西南埃尔树地区的影响

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The groundwater extracted from the unconfined Quaternary aquifer is the main source of water supply in El-Tur area. The area is bounded from the east by the elevated basement complex of Southern Sinai and from the west by El-Qabaliyat Ridge. The wadis dissecting these highlands form effective watersheds of the Quaternary aquifer. These wadis form areas of focused recharge. Recharge also occurs directly via the Quaternary sediments covering El-Qaa Plain. Subsurface lateral groundwater flow from the fractured basement contributes significant recharge to the aquifer as well. The aquifer sediment facies affect the type and quality of groundwater. In the eastern partwhere the aquifer is composed mainly of gravel and coarse sand with fragments of weathered basement, the Na-Cl-SO4 water dominates. In the west where the facies change is rapid and complex, many water types arise. The base exchange index (BEX) is positive in this part reflecting the role of clay minerals in changing the water types via cation exchange. In the east where clays are insignificant in the aquifer, the BEX is negative. In the western part next to El-Qabaliyat Ridge, the wells discharging from the calcareous sand zone have low groundwater salinities compared to the wells discharging from the alluvium. In general, the groundwater salinity increases in the direction of groundwater flow from the northeast to the southwest which reflects the dissolution of aquifer sediments. The concentration relationships between the major ions on one hand and chloride on the other reflect the dissolution of calcium carbonates, precipitation of K-and Mg-bearing minerals, and cation exchange of Ca for Na on clay minerals. The hydrochemical models support these reactions. In addition, they show that the effect of evaporation on the recharge water in the western catchment is about four times its effect on the eastern recharge water which reflects the rapid recharge through the wadis draining the fractured basement. Moreov
机译:从无束缚的第四纪含水层中提取的地下水是EL-Tur区域供水的主要来源。该地区由南北南部的地下室综合体和埃尔Qabaliyat山脊的地下室复合物界定。瓦迪斯解剖这些高地形成了四季含水层的有效分水岭。这些涉嫌形成的面积的重点充电。通过覆盖El-Qaa Plain的四季沉积物直接充电也会发生。来自裂缝地下室的地下横向地下水流量也为含水层带来了显着的补给。含水层沉积物相面积影响地下水的类型和质量。在东部的地方,含水层主要由砾石和粗砂组成,带有风化的地下室的碎片,Na-Cl-SO4水占主导地位。在方面改变快速且复杂的西方,出现了许多水类型。基础交换指数(BEX)在该部分中是阳性的,反映粘土矿物在通过阳离子交换改变水类型的作用。在东方粘土在含水层中微不足道的地方,Bex是消极的。在El-Qabaliyat Ridge旁边的西部,与钙砂区排出的井与从加油中排出的井有低的地下水盐度。通常,地下水盐度在地下水从东北到西南部的方向增加,这反映了含水层沉积物的溶解。一方面和氯化物上的主要离子之间的浓度关系反映了碳酸钙,K-和Mg承载矿物的溶解,对粘土矿物质的Na进行Ca的阳离子交换。水化学模型支持这些反应。此外,他们表明,蒸发对西部地区的充电水的影响是其对东方充电水影响的四倍,这反映了通过瓦迪排放裂缝地下室的快速充电。更多

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