Volume 36 Issue 6
Jun.  2011
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WEN Zhang, HUANG Guan-hua, LIU Zhuang-tian, LI Jian, 2011. An Approximate Analytical Solution for Two-Region Non-Darcian Flow Toward a Well in a Leaky Aquifer. Earth Science, 36(6): 1165-1172. doi: 10.3799/dqkx.2011.123
Citation: WEN Zhang, HUANG Guan-hua, LIU Zhuang-tian, LI Jian, 2011. An Approximate Analytical Solution for Two-Region Non-Darcian Flow Toward a Well in a Leaky Aquifer. Earth Science, 36(6): 1165-1172. doi: 10.3799/dqkx.2011.123

An Approximate Analytical Solution for Two-Region Non-Darcian Flow Toward a Well in a Leaky Aquifer

doi: 10.3799/dqkx.2011.123
  • Received Date: 2011-05-08
    Available Online: 2021-11-10
  • Publish Date: 2011-06-15
  • In this paper, we propose a two-region non-Darcian flow model near a pumping well in a leaky aquifer. The flow near the pumping well is assumed to be non-Darcian, with the area nearby defined as non-Darcian flow region, while the flow far away from the pumping well can be regarded as Darcian flow. The critical distance distinguishing the non-Darcian flow region and Darcian flow region can be determined by the critical Renolds number. We have used a linearization procedure coupled with Laplace transform to solve such a two-region non-Darcian flow model. The drawdowns both in the non-Darcian flow region and Darcian flow region have been obtained by using the so-called Stefest numerical Laplace inversion method. We have compared our results with those for the one-region Darcian flow model and the one-region non-Darcian flow model. The results indicate that: (1) The drawdowns in the non-Darcian flow region of different critical distances approach the same asymptotic value at early stages, as well as the result for the one-region non-Darcian flow model; while at late stages, significant difference has been found between the drawdowns obtained in this study; (2) A larger "non-Darcian hydraulic conductivity" kD results in a greater drawdown in the entire aquifer at early stages, while leads to a smaller drawdown in the non-Darcian flow region at late stages and has little impact on the drawdowns in the Darcian flow region; (3) The leakage effect on the drawdown is similar to that for the Darcian flow case, and it only exists at late stages; (4) When the wellbore storage is considered, all the drawdowns inside the well for different kD and dimensionless leakage parameter BD values approach the same asymptotic value at early stages and are straight lines in double logarithmic paper at early stages.

     

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  • Camacho, V.R.G., Vásquez, C.M., 1992. Comment on "analytical solution incorporating nonlinear radial flow in confined aquifers" by Zekai Sen. Water Resources Research, 28(12): 3337-3338. doi: 10.1029/92WR01646
    Chang, A.D., Guo, J.Q., Wang, H.S., 2000. The analytical solution of unsteady well flow with two flow regimes. Journal of Hydraulic Engineering, 6: 49-53 (in Chinese with English abstract). doi: 10.1080/09715010.2000.10514679
    Hantush, M.S., Jacob, C.E., 1955. Non-steady radial flow in an infinite leaky aquifer. Transactions, American Geophysical Union, 36(1): 95-100. doi: 10.1029/TR036i001p00095
    Liu, Y.H., Chang, A.D., 2005. Research on unsteady well flow of the specific discharge of the nonlinear regime. Journal of Northwest Sci-Tech University of Agriculture and Forestry (Natural Science Edition), 33(8): 113-115 (in Chinese with English abstract). http://qikan.cqvip.com/Qikan/Article/Detail?id=20015341
    Liu, Y.H., Chang, A.D., Deng, Q.X., 2005. Drawdown of well flow in the co-existed linear and nonlinear exponents. Journal of Northwest Sci-Tech University of Agriculture and Forestry (Natural Science Edition), 33(3): 157-160 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XBNY200503026.htm
    Mathias, S.A., Butler, A.P., Zhan, H.B., 2008. Approximate solutions for forchheimer flow to a well. Journal of Hydraulic Engineering, 134(9): 1318-1325. doi: 10.1061/(ASCE)0733-9429(2000)134.9
    Sen, Z., 1987. Non-Darcian flow in fractured rocks with a linear flow pattern. Journal of Hydrology, 92(1-2): 43-57. doi: 10.1016/0022-1694(87)90088-6
    Sen, Z., 1988. Type curves for two-region well flow. Journal of Hydraulic Engineering, 114(12): 1461-1484. doi: 10.1061/(ASCE)0733-9429(1988)114.12
    Sen, Z., 1989. Nonlinear flow toward wells. Journal of Hydraulic Engineering, 115(2): 193-209. doi: 10.1061/(ASCE)0733-9429(1989)115.2(193)
    Sen, Z., 1990. Nonlinear radial flow in confined aquifers toward large-diameter wells. Water Resources Research, 26(5): 1103-1109. doi: 10.1029/WR026i005P01103
    Stehfest, H., Goethe-Univ, J.W., Germany, W., 1970a. Algorithm 368: numerical inversion of Laplace transforms. Communications of the ACM, 13(1): 47-49. doi: 10.1145/361953.361969
    Stehfest, H., Goethe-Univ, J.W., Germany, W., 1970b. Remark on algorithm 368: numerical inversion of Laplace transforms. Communications of the ACM, 13(10): 624-625. doi: 10.1145/355598.362787
    Wang, P.J., 1996. Theory for two-regime well flow in confined aquifers. Journal of Irrigation and Drainage, 15(4): 1-9 (in Chinese with English abstract).
    Wen, Z., Huang, G.H., Zhan, H.B., 2006. Non-Darcian flow in a single confined vertical fracture toward a well. Journal of Hydrology, 330(3-4): 698-708. doi: 10.1016/j.jhydrol.2006.05.001
    Wen, Z., Huang, G.H., Zhan, H.B., 2008a. Non-Darcian flow to a well in an aquifer-aquitard system. Advances in Water Resources, 31(12): 1754-1763. doi: 10.1016/j.advwatres.2008.09.002
    Wen, Z., Huang, G.H., Zhan, H.B., 2008b. An analytical solution for non-Darcian flow in a confined aquifer using the power law function. Advances in Water Resources, 31(1): 44-55.10.1016/j. advwatres. 2007.06.002 doi: 10.1016/j.advwatres.2007.06.002
    Wen, Z., Huang, G.H., Zhan, H.B., et al., 2008c. Two-region non-Darcian flow toward a well in a confined aquifer. Advances in Water Resources, 31(5): 818-827. doi: 10.1016/j.advwatres.2008.01.004
    Wen, Z., Huang, G.H., Li, J., et al., 2009a. A numerical solution of non-Darcian flow toward an extended well in a confined aquifer. Journal of Hydraulic Engineering, 40(4): 398-402 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SLXB200904004.htm
    Wen, Z., Huang, G.H., Li, J., et al., 2009b. A numerical solution for non-Darcian flow toward a well in a leaky aquifer. Chinese Journal of Hydrodynamics, 24(4): 448-454 (in Chinese with English abstract). http://www.researchgate.net/publication/287464153_A_numerical_solution_for_non-Darcian_flow_toward_a_well_in_a_leaky_aquifer
    Wu, Y.S., 2001. Non-darcy displacement of immiscibe fluids in porous media. Water Resources Research, 37(12): 2943-2950. doi: 10.1029/2001WR000389
    Wu, Y.S., 2002. Numerical simulation of single-phase and multiphase non-Darcy flow in porous and fractured reservoirs. Transport in Porous Media, 49(2): 209-240. doi: 10.1023/A:1016018020180
    常安定, 郭建青, 王洪胜, 2000. 两种流态区域条件下的井流问题的解析解. 水利学报, 6: 49-53. https://www.cnki.com.cn/Article/CJFDTOTAL-SLXB200006008.htm
    刘元会, 常安定, 2005. 非线性渗流区域井流问题渗流速度的分区研究. 西北农林科技大学学报(自然科学版), 33(8): 113-115. https://www.cnki.com.cn/Article/CJFDTOTAL-XBNY200508034.htm
    刘元会, 常安定, 邓秋霞, 2005. 线性非线性并存区域井流问题的水头降深研究. 西北农林科技大学学报(自然科学版), 33(3): 157-160. doi: 10.3321/j.issn:1671-9387.2005.03.037
    王鹏举, 1996. 考虑非达西流情况下地下水向集水建筑物运动的非稳定理论的研究. 灌溉排水, 15(4): 1-9. https://www.cnki.com.cn/Article/CJFDTOTAL-GGPS604.000.htm
    文章, 黄冠华, 李健, 等, 2009a. 承压含水层中扩展井附近非达西流数值解. 水利学报, 40(4): 398-402. https://www.cnki.com.cn/Article/CJFDTOTAL-SLXB200904004.htm
    文章, 黄冠华, 李健, 等, 2009b. 越流含水层中抽水井附近非达西流动模型的数值解. 水动力学研究与进展, 24(4): 448-454. https://www.cnki.com.cn/Article/CJFDTOTAL-SDLJ200904010.htm
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