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首页> 外文期刊>Acta Polytechnica >Modeling Water Pollution Of Soil
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Modeling Water Pollution Of Soil

机译:模拟土壤水污染

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The government of the Czech Republic decided that in the location to the west of Prague, capital city of the Czech Republic, some deep mines should be closed because of their low efficiency of coal mined i.e. small amounts and low quality of the coal extracted in the final stage of mining. The locations near Prague influenced the decision to do maintenance on the abandoned mines, as the thread of soil pollution was unacceptably high in the neighborhood of the capital city. Before the mines were closed it was necessary to separate existed extensive horizontal location of salt water below a clay layer in order not to deteriorate the upper fresh water. The salt water could not be allowed to pollute the upper layer with the fresh water, as many wells in villages in the neighborhood of the former mines would be contaminated. Two horizontal clay layers (an insulator and a semi-insulator) separated the two horizons containing salt water and fresh water. Before starting deep mining, vertical shafts had to be constructed with concrete linings to enable the miners to access the depths. The salt water was draining away throughout the existence of the mine. The drainage was designed very carefully to avoid possible infiltration of salt water into the upper horizon. Before the mines were abandoned it was necessary to prevent contact between the two kinds of waters in the shafts. Several options were put forward, the most efficient of which appeared to be one that proposed filling the shafts with spoil soil and creating a joint seal made of disparate material at the interface between the salt water and fresh water to create a reliable stopper. The material for the spoil soil was delivered from deposits located not far from the shafts. This material consisted of a variety of grains of sand, big boulders of slate, slaty clay, sandstone, etc.. Chemical admixtures were considered to improve the ftocculation of the filling material. The stopper was positioned at a depth of 220-300 m below the terrain. As an alternative, thinner stoppers were considered, but this option was discarded. The aim of this paper is to describe the design of the stoppers applied to separate the two types of water along the contact horizon using Demi's DSC theory (Distinct State Concept), and generalized plane strain in the m ultiphase problem of water flow in a porous medium. In addition, a comparison of some results from scale experimental models with numerical solutions was carried out. The intrinsic material properties of stoppers for numerical computations were obtained from physical and chemical laboratory tests. The models were evaluated for the complete underground work, particularly in its final stage of construction.
机译:捷克共和国政府决定,在捷克首都布拉格以西的位置,应关闭一些深部煤矿,因为这些煤矿开采的煤效率低,即开采的煤炭数量少且质量低。采矿的最后阶段。布拉格附近的地点影响了对废弃矿山进行维护的决定,因为首都附近的土壤污染状况令人难以接受。在关闭矿井之前,有必要在粘土层下面分离盐水的广泛存在的水平位置,以免使上部淡水变质。盐水不能被淡水污染上层,因为以前矿山附近村庄的许多井都将受到污染。两个水平的粘土层(绝缘体和半绝缘体)将包含盐水和淡水的两个层分开。在开始深层开采之前,必须使用混凝土衬砌构造竖井,以使矿工能够进入深处。整个矿山中的盐水都流失了。排水装置的设计非常谨慎,以避免盐水渗入上层地平线。在废弃地雷之前,有必要防止竖井中两种水之间的接触。提出了几种选择,其中最有效的选择似乎是建议用变质土填充竖井,并在盐水和淡水之间的界面处创建由不同材料制成的接头密封,以创建可靠的塞子。弃土的物料是从距离竖井不远的沉积物中输送的。这种材料由各种沙粒,板岩大块石,板岩粘土,砂岩等组成。人们认为使用化学外加剂可以改善填充材料的絮凝性。塞子位于地形下方220-300 m的深度。作为替代方案,考虑使用更薄的塞子,但该选项被放弃了。本文的目的是描述塞子的设计,该塞子的设计使用Demi的DSC理论(离散状态概念)沿接触层将两种类型的水分离,并在多孔水流的多相问题中推广广义平面应变介质。此外,还对规模实验模型的一些结果与数值解进行了比较。从物理和化学实验室测试中获得了用于数值计算的塞子的固有材料特性。对模型进行了完整的地下工程评估,尤其是在施工的最后阶段。

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