两层介质中地下水位变化的数值和数学模拟

Sherzod Daliev, N. Ravshanov
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摘要

本文讨论了在导电性好、导电性差的地层中预测地下水、压力水和盐浓度变化的过程。利用数学模型对这一过程进行研究和决策是一个迫切需要解决的问题。本文简要分析了对所研究对象进行数学和数值模拟的科学论文。为了对所考虑的过程进行全面研究,建立了基于有限差分法的模型和有效的数值算法。已有研究表明,与水位相关的地下水位和压力水位、过滤渗透率、失水系数和过滤速率的变化会对环境过程产生严重影响。通过计算实验分析可知,对地压水过滤和盐浓度影响较大的主要因素是层内过滤电导率、失水系数和层内过滤流速。并对所开发的数值算法的计算结果进行了分析。在引入新技术之前,建议使用有效的数值算法来预测水中盐分含量的变化
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Numerical and mathematical modeling of changes in groundwater levels in two-layer media
The process of predicting changes in the levels of groundwater and pressure water and salt concentration in layers with good and poor conductivity is discussed in the article. Research and decision-making on this process using mathematical modeling is an urgent problem. A brief analysis of scientific papers devoted to mathematical and numerical modeling of the object under study is presented. To conduct a comprehensive study of the process under consideration, a model and an efficient numerical algorithm based on the finite difference method were developed. It has been studied that changes in the level of ground and pressure water, filtration permeability, water loss coefficient and filtration rate associated with the water level can have a serious impact on the environmental process. As follows from the analysis of the computational experiments, the main factors that significantly affect the filtration of ground and pressure waters and salt concentration are filtration conductivity in the layers, water loss coefficient, and filtration flow velocity in the layers. The results obtained based on these developed numerical algorithms were analyzed. Before introducing new technologies, recommendations were developed to predict changes in salt content in water using an effective numerical algorithm
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