标题: 有限自由含水层中水平井抽水引起的地下水流解析模式
An Analytical Model for Groundwater Flow Induced by a Horizontal Well in a Finite Unconfined Aquifer
作者: 陈俊杰
Chen, Jyun-Jie
叶弘德
Yeh, Hund-Der
环境工程系所
关键字: 双重积分转换;拉普拉斯转换;敏感度分析;河川祛水率;河川入渗率;Robin边界条件;一阶自由液面方程式;double-integral transform;Laplace transform;sensitivity analysis;stream depletion rate;stream filtration rate;Robin boundary condition;first-order free surface equation
公开日期: 2015
摘要: 本研究建构一个数学模式,描述于自由含水层内因水平井抽水引起的三维地下水流。考虑含水层水平向四个边界呈现矩形,分别包含两条平行的河川和两个平行的不透水边界;而垂直向厚度有限,水层底部不透水、顶部为自由液面。模式包括代表井抽水的点沉项,自由液面由一阶方程式来描述其水位的变化,而河川有低渗透性河床,由Robin边界条件代表。应用双重积分转换、拉普拉斯转换、和余数定理,可求得模式的水头解析解;接着,从点沉项的位置,沿着水平井对水头解析解作积分,所得结果除以井长度,可获得水平井抽水引起的水头分布解析解。透过达西定律与水头解析解,可导出河川祛水率的解析解,以描述井抽水产生的河川渗流量。本研究也进行水头对参数改变的敏感度分析,参数包含水平与垂直向的水力传导系数、河床渗透性、比出水率、比产水率、及水平井的长度和深度。此外,我们提出一个量化条件,指出水层中水平井引起的三维和二维水流的适用范围。此外,针对河川祛水率,我们也提出另一个量化条件,以判断可忽略垂直流的情况。当满足上述两个条件时,过去的二维水流模式,即可用来估计地下水位变化和河川祛水率。
This study develops a mathematical model for describing three-dimensional (3-D) groundwater flow due to pumping at a horizontal well in a finite unconfined aquifer bounded by two parallel streams and two no-flow boundaries. The 3-D transient flow equation of the hydraulic head has a point sink term representing the pumping rate of the well. A first-order free surface equation is used to describe water table change, and the Robin boundary condition is chosen to represent the flow rate across the streambed. The point-sink solution of the model is obtained based on the methods of double-integral transform and Laplace transform. The solution of the head distribution is then developed by integrating the point-sink solution along the well and dividing the result by the well length. On the basis of Darcy’s law and the head distribution along the streams, the solution for the stream depletion rate (SDR) can also be developed. With the aid of the head solution, the sensitivity analysis can be then applied to explore the behavior of the hydraulic head in response to the change of a specific parameter such as horizontal and vertical hydraulic conductivities, streambed permeability, specific storage, specific yield, well length and well depth. A quantitative criterion is provided to identify the region where the groundwater flow is 3-D or 2-D without the vertical component. In addition, another criterion is also given to allow the neglect of the effect of vertical flow on the SDR. Conventional 2-D flow models are capable of predicting accurate head and SDR if satisfying these two criteria.
URI: http://140.113.39.130/cdrfb3/record/nctu/#GT070151703
http://hdl.handle.net/11536/125602
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