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Laboratory investigations of compatibility of the Kuwait Group aquifer, Kuwait, with possible injection waters

机译:实验室研究科威特科威特集团含水层与可能注入水的相容性

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A laboratory investigation of the compatibility of the Kuwait Group aquifer of Kuwait with desalinated seawater and reverse osmosis processed treated wastewater was carried out in anticipation of the artificial recharge of the aquifer in future. Even with the use of wax coating and freezing with liquid nitrogen, no core plugs could be extracted from the unconsolidated sections, and only the consolidated to semi-consolidated sections could be studied. The aquifer consists of silty and gravelly sand, and is often highly calcareous. The clay minerals present in the aquifer mostly belong to the montmorillonite and illite groups, with some palygorskite. Mercury injection porosimetry experiments on core plugs from the more cemented parts of the aquifer suggest that, to avoid significant clogging from suspended solids, particles down to a diameter of 8 mum should be filtered out of the injection water. Core flow experiments suggest that, for the samples examined, loss of permeability due to clay swelling is not very important. The blocking of pore throats by moving fines may be a more serious problem during injection. The geochemical simulation indicates that the possibility of scale formation when the injection waters come in contact with the Kuwait Group formation water is remote. Rather, there is a possibility of dissolution of carbonate minerals in the aquifer in contact with the injection waters. (C) 2003 Elsevier B.V. All rights reserved. [References: 23]
机译:对科威特科威特集团含水层与淡化海水和反渗透处理过的废水之间的相容性进行了实验室研究,以期将来可以对含水层进行人工补给。即使使用蜡涂层并用液氮冷冻,也无法从未固结段中抽出芯塞,而只能研究固结至半固结段。含水层由粉质和砾石质的沙子组成,通常是高度钙质的。含水层中存在的粘土矿物主要属于蒙脱石和伊利石组,还有一些坡缕石。对含水层中较胶结部分的岩心塞进行的汞注入孔隙率实验表明,为避免悬浮固体明显堵塞,应从注入水中滤出直径小于8毫米的颗粒。岩心流动实验表明,对于所检查的样品,由于粘土膨胀而导致的渗透性损失不是很重要。在注射过程中,通过移动细粉堵塞孔喉可能是一个更严重的问题。地球化学模拟表明,当注入水与科威特集团地层水接触时,形成水垢的可能性很小。相反,有可能在与注入水接触的含水层中溶解碳酸盐矿物。 (C)2003 Elsevier B.V.保留所有权利。 [参考:23]

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