Non-Darcian flow to a partially penetrating well in a confined aquifer with a finite-thickness skin; [Ecoulement non-darcéen vers un puits pénétrant partiellement un aquifère captif avec un effet de peau d’épaisseur finie]; [Fluxo não Darciano em um poço parcialmente penetrante com uma película de espessura limitada em aquífero confinado]; [Flujo no darciano para un pozo parcialmente penetrante en un acuífero confinado con una película de espesor finito]

被引:0
|
作者
Feng Q. [1 ]
Wen Z. [2 ,3 ]
机构
[1] Department of Geotechnical Engineering, Tongji University, Shanghai
[2] School of Environmental Studies, China University of Geosciences, Wuhan, 430074, Hubei
[3] Laboratory of Basin Hydrology and Wetland Eco-restoration, China University of Geosciences, Wuhan, 430074, Hubei
基金
中国国家自然科学基金;
关键词
Analytical solutions; Groundwater flow; Izbash equation; Partially penetrating well; Skin effect;
D O I
10.1007/s10040-016-1389-8
中图分类号
学科分类号
摘要
Non-Darcian flow to a partially penetrating well in a confined aquifer with a finite-thickness skin was investigated. The Izbash equation is used to describe the non-Darcian flow in the horizontal direction, and the vertical flow is described as Darcian. The solution for the newly developed non-Darcian flow model can be obtained by applying the linearization procedure in conjunction with the Laplace transform and the finite Fourier cosine transform. The flow model combines the effects of the non-Darcian flow, partial penetration of the well, and the finite thickness of the well skin. The results show that the depression cone spread is larger for the Darcian flow than for the non-Darcian flow. The drawdowns within the skin zone for a fully penetrating well are smaller than those for the partially penetrating well. The skin type and skin thickness have great impact on the drawdown in the skin zone, while they have little influence on drawdown in the formation zone. The sensitivity analysis indicates that the drawdown in the formation zone is sensitive to the power index (n), the length of well screen (w), the apparent radial hydraulic conductivity of the formation zone (Kr2), and the specific storage of the formation zone (Ss2) at early times, and it is very sensitive to the parameters n, w and Kr2 at late times, especially to n, while it is not sensitive to the skin thickness (rs). © 2016, Springer-Verlag Berlin Heidelberg.
引用
收藏
页码:1287 / 1296
页数:9
相关论文
共 10 条