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STUDY ON ISOTOPE MODEL OF DYKE LEAKAGE

机译:堤坝渗漏同位素模型研究

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摘要

Applying the methods of stable isotopes and hydrochemistry to study the dyke is an effective way. And the theory of environmental isotope and hydrochemistry applied to leakage study is described. As natural tracers, environmental isotope and hydrochemistry mark groundwater, river water and precipitation. By contrast of the composition of environment isotope and water chemistry in water, the relation between them can be determined to distinguish the replenishment resource of groundwater, the position and range of leakage, the stratum formation and so on. Few coupled models of isotope field have been given so far. After making some assumptions and simplifications, the following models of the leakage of dyke are deduced based on basic law of hydraulics principle. And the model is used to predict the leakage velocity based on the data of the location. These models' building makes it possible to simulate the leakage of dyke quantitatively and gives it a help to interpret more objectively and more sufficiently the information that included in the leakage of dyke.
机译:应用稳定同位素和水化学方法研究堤坝是一种有效的方法。阐述了环境同位素和水化学理论在渗漏研究中的应用。作为天然示踪剂,环境同位素和水化学标志着地下水,河水和降水。通过比较水中环境同位素和水化学成分的组成,可以确定两者之间的关系,以区别地下水的补充资源,渗漏的位置和范围,地层的形成等。到目前为止,很少给出同位素场的耦合模型。在做出一些假设和简化之后,根据水力学原理的基本原理推导了堤防渗漏的以下模型。然后使用该模型根据位置数据预测泄漏速度。这些模型的建立使得可以定量地模拟堤防泄漏,并有助于更客观,更充分地解释堤防泄漏中包含的信息。

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