多含水层系统的研究及应用

APPLICATION AND RESEARCH FOR MULTI-AQUIFER SYSTEM

  • 摘要: 从平原地区的多含水层系统概念出发,建立了多含水层系统的数学模型,在此基础上进行了多含水层系统的流程设计,为解决此类地下水模型计算提供了一个良好的方法和思路。针对多含水层系统和多层、多结点,形成的矩阵方程组线形高度稀疏特点,给出了共轭梯度法和SSOR-共轭梯度法的两种比较解法,最后结合松辽盆地东部三层含水层系统的计算实例,对未来地下水开采引起的水位变化进行了预报,预测明水一段和二段在2005年将会各出现一个较大的降落漏斗,且二段漏斗的深度和范围明显大于一段。多含水层系统的研究具有较大的实用性和灵活性。

     

    Abstract: This paper introduces the establishment of multi-aquifer system's mathematical model, according to conception of multiaquifer system in plain area. Based on that mathematical model, the programming flowchart for multi-aquifer system is designed, providing an available method and idea for model calculation. In accordance with the characteristics, such as multi-layer, multi-node and highly spare linear matrix equation of multi-aquifer system, the solution of conjugate gradient method and SSOR-conjugate gradient method is presented for comparison. Taking the calculation of three layers in eastern Songliao Basin as example, the forecast for water level changes caused by further groundwater recovery is conducted. Based on that larger water cones will occurrence individually in Mingshi Interval No.1 and Interval No.2 in 2005, and the depth and scope of water cone in Inter-val No.2 is larger than that in Interval No.1. The research on multi-aquifer system, therefore, is of practicability and flexibility.

     

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