基于地质和地电阻率测量的开罗东南部Tourah粘土采石场扩展段渗水源

A. A. El-Gawad
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引用次数: 2

摘要

水泥工业基本上依赖于粘土作为工业的主要原料之一。图拉粘土采石场是埃及最古老和最大的粘土采石场之一,位于开罗东南部。影响粘土采石场并可能导致其永久关闭的最大问题是,水到达采石场并导致从采石场提取原材料的困难,最终导致采石场关闭。在图拉粘土采石场扩建段的采矿作业和原料提取过程中,发现采石场底部出现漏水,积水开始增多,导致采石场设备进出困难。摘要对图拉粘土采石场扩展段内及周边地区进行了详细的野外地质研究和地电阻率调查,找出了采石场底部迅速增加的漏水的来源和原因。为了了解和解决上述问题,利用Wenner配置进行了13次垂直电测深和2次水平剖面的地电阻率测量。地电资料的解释显示了三个主要单元;表层由干燥的沙子、砾石和岩石碎片组成,其次是第二层松散的沙子和部分饱和的水,最后是粘土层,作为水泥工业的原料。据此,结合现场地质观测和地电阻率解释,认为粘土采石场底部可能的水源为第二松散的部分饱和砂单元,该区域水侵方向为东北方向。为了避免Tourah粘土采石场的关闭,建议采用水头补偿或井田脱水的方法在砂单元的水到达采石场底部之前将其抽出。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Water Seepage Source at the Extension of Tourah Clay Quarry, Southeastern Cairo Based on Geological and Geoelectrical Resistivity Measurements
The cement industry depends essentially on the clay as one of the main raw materials for the industry. The Tourah clay quarry is one of the oldest and largest quarries of clays in Egypt, which is located to the southeastern of Cairo. The biggest problems that affect the clay quarries and may cause them to be closed forever is that, the water reaches them and leads to the difficulty of extracting raw materials from the quarries and ultimately leads to their closure. During the mining operations and extraction of raw materials from the extension of Tourah clay quarry, a water leak was observed that reached the bottom of the quarry, and the water began to increase and led to the difficulty of entering and exiting the equipments from the quarry. A detailed geological field study and geoelectrical resistivity survey were conducted in and around the extension of Tourah clay quarry to find out the source and cause of the water leak, which was increasing rapidly on the bottom of quarry. A geoelectrical resistivity survey was performed in the form of thirteen vertical electrical soundings and two horizontal profiling were made using the Wenner configuration in order to understand and solve the formentioned problem. The interpretation of the geoelectrical data shows three main units; surface layer from dry sand, gravel and rock fragments followed by a second layer of loose sand and is partially saturated with water and finally a clay layer which is extracted as a raw material in cement industry. Accordingly, based on the field geological observations in addition to the geoelectrical resistivity interpretations, we can conclude that, the possible water source in the bottom of clay quarry is due to the second loose partially saturated sand unit and the direction of water invasion in this particular area comes from the northeastern direction. To save the extension of Tourah clay quarry from closure it is recommended to extract the water from the sand unit before it reached the quarry bottom either by water head compensation or dewatering of the well field area.
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