Prof. Chongxi Chen's academic research contributions in the area of hydrogeology
-
摘要:
陈崇希教授长期坚持在水文地质领域从事课程教学、人才培养和科学研究, 取得了丰硕的学术研究成果。对陈崇希教授在水文地质领域的学术研究贡献进行了系统的总结评述, 主要包括3个方面: ①开展了地下水动力学的理论创新研究, 纠正了历史上"影响半径稳定井流"模型的错误, 提出了一系列特殊水文地质问题的解析模型, 改进和拓展了经典井流模型; ②持续探索水文地质模拟方法, 研究形成了一系列提高地下水模拟仿真水平的技术方法, 包括滨海区地下水的等效排泄边界、渗流-管流耦合模型、岩溶管道-裂隙-孔隙三重介质地下水线性-非线性流模型、地下水开采-地面沉降模型等, 研发了独具优势的地下水流模拟软件PGMS; ③提出地下水可持续开采量评价的补排增量理论, 完成我国多个典型区域的地下水模拟, 为科学评价地下水资源起到示范作用。陈崇希教授的创新研究对我国水文地质学的发展起到了重要的推动作用。
Abstract:Significance Prof. Chongxi Chen has long been engaged in teaching courses, personnel training and scientific research in the field of hydrogeology, working diligently and innovatively, and has achieved fruitful academic research results.
Progress This article makes a systematic review of Prof. Chongxi Chen's academic contributions in the field of hydrogeology, mainly including three aspects: ① Carrying out innovative and theoretical researchon groundwater hydraulics. He corrected the historical model error of "steady-state well flow within the influence radius", developed a series of analytical models for special hydrogeological problems, and improved and extended classical well flow models. ② Continuously exploring hydrogeological simulation methods. He proposed a number of techniques and methods to improve the emulational level of groundwater simulation, such as the equivalent submarine discharge boundary of coastal groundwater, the coupling seepage-pipe flow model, the linear-nonlinear flow model in triple Karst media of cave-fracture-porous and the groundwater withdrawal-land subsidence model, etc. He also developed a unique and advantageous software for groundwater flow simulation, PGMS. ③ Proposing a theory of recharge-discharge changes for the evaluation of the sustainable groundwater extraction. He completed groundwater modelling in several typical regions in China, which played a demonstration role for the scientific assessment of groundwater resources.
Conclusions and Prospects Prof. Chongxi Chen's innovative research has played an important role in promoting the development of hydrogeology in China.
-
[1] Dupuit A J E J. Etudestheoretiques et pratiques sur le mouvement des eaux[M]. Paris: Dunod, 1863(in Frence). [2] Каменский Г И. Основы Дина-мики Подземных Вод[M]. Госгеолиздат: Москва, 1943(in Russian). [3] Bear J. Dynamics of fluids in porous media[M]. New York: Amer Elsevier Publishing Company, 1972. [4] 陈崇希. 地下水动力学[Z]. 北京: 北京地质学院, 1966.Chen C X. Groundwaterhydraulics[Z]. Beijing: Beijing College of Geology, 1966(in Chinese). [5] 陈崇希. 地下水不稳定流计算[Z]. 山东莱芜: 山东省地质局第一地质大队, 1974.Chen C X. Computation oftransient groundwater flow[Z]. Laiwu Shandong: First Geological Brigade of Shandong Geological Bureau, 1974(in Chinese). [6] 陈崇希. 地下水不稳定井流计算方法[M]. 北京: 地质出版社, 1983.Chen C X. Computation method of transient groundwater flow to wells[M]. Beijing: Geological Publishing House, 1983(in Chinese). [7] 陈崇希. 影响半径稳定井流模型与可持续开采量: 地下水动力学一个基本理论问题的分歧: 与薛禹群院士商榷[J]. 水利学报, 2010, 41(8): 1003-1008. https://www.cnki.com.cn/Article/CJFDTOTAL-SLXB201502015.htmChen C X. Steady well flow model with influence radius and sustainable pumping rate: A dispute on a fundamental theoretical problem in groundwater hydraulics[J]. Journal of Hydraulic Engineering, 2010, 41(8): 1003-1008(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SLXB201502015.htm [8] 陈崇希. 影响半径稳定井流模型与可持续开采量: 地下水动力学一个基本理论问题的分歧再讨论: 对薛禹群院士讨论的答复[J]. 水利学报, 2014, 45(1): 117-121. https://www.cnki.com.cn/Article/CJFDTOTAL-SLXB201401017.htmChen C X. Steady well flow model with influence radius and sustainable pumping rate: A further dispute on a fundamental theoretical problem in groundwater hydraulics[J]. Journal of Hydraulic Engineering, 2014, 45(1): 117-121(in Chinese). https://www.cnki.com.cn/Article/CJFDTOTAL-SLXB201401017.htm [9] Theis C V. The relation between the lowering of the piezometric surface and the rate and duration of discharge of a well using groundwater storage[J]. Trans. Amer. Geophys. Union, 1935, 16: 519-524. doi: 10.1029/TR016i002p00519 [10] 陈崇希. 关于地下水开采引发地面沉降灾害的思考[J]. 水文地质工程地质, 2000, 27(1): 45-48. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG200001014.htmChen C X. Thinking about theland subsidence disaster induced by groundwater exploitation[J]. Hydrogeology & Engineering Geology, 2000, 27(1): 45-48(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG200001014.htm [11] 陈崇希. 对《水文地质调查规范(1∶50 000)》的若干讨论和建议[J]. 水文地质工程地质, 2018, 45(1): 173-174. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG201801026.htmChen C X. Discussions and suggestions on the specification for hydrogeology survey(1∶50 000)[J]. Hydrogeology & Engineering Geology, 2018, 45(1): 173-174(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG201801026.htm [12] 陈崇希. 层状非均质无压含水层中地下水不稳定井流的一种计算方法[J]. 地球科学: 武汉地质学院学报, 1981(1): 222-228.Chen C X. The calculation method of groundwater non-steady flowing to wells in an inhomogeneous stratified aquifer[J]. Earth Science: Journal of Wuhan College of Geology, 1981(1): 222-228(in Chinese with English abstract). [13] Hemker C J. Transient well flow in leaky multiple-aquifer systems[J]. Journal of Hydrology, 1985, 81: 111-126. doi: 10.1016/0022-1694(85)90170-2 [14] Bear J. Hydraulics of ground water[M]. Jerusalem: McGraw-Hill Inc, 1979. [15] 薛禹群, 吴吉春. 地下水动力学: 第3版[M]. 北京: 地质出版社, 2010.Xue Y Q, Wu J C. Groundwater hydraulics: The third Edition[M]. Beijing: Science Press, 2010(in Chinese). [16] 陈崇希. 地下水不稳定井流计算方法[Z]. 武汉: 武汉地质学院, 1975.Chen C X. Computation method of transient groundwater flow to wells[Z]. Wuhan: Wuhan College of Geology, 1975(in Chinese). [17] 陈崇希, 陈明佑, 陈爱光, 等. 矿坑涌水量计算方法研究[M]. 武汉: 武汉地质学院出版社, 1985.Chen C X, Chen M Y, Chen A G, et al. Computation method studies on water inflow in mining pits[M]. Wuhan: Wuhan College of Geology Press, 1985(in Chinese). [18] Chen C X, Hu L T, Wang X S. Analysis of steady ground water flow toward wells in a confined-unconfined aquifer[J]. Ground Water, 2006, 44(4): 609-612. doi: 10.1111/j.1745-6584.2006.00170.x [19] Hu L T, Chen C X. Analytical methods for transient flow to a well in a confined-unconfined aquifer[J]. Ground Water, 2008, 46(4): 642-646. doi: 10.1111/j.1745-6584.2008.00436.x [20] 陈崇希, 林敏, 成建梅. 地下水动力学: 第五版[M]. 北京: 地质出版社, 2011.Chen C X, Lin M, Cheng J M. Groundwater hydraulics: 5th Edition[M]. Beijing: Geological Publishing House, 2011(in Chinese). [21] Maillet E. Essais d'Hydraulique souterraine et fluviale[M]. Paris: Hermann, 1905(in French). [22] Lin M, Chen C X. Analysis models of groundwater flowing to spring in karst aquifer[C]//Anon. Proceedings of IAH 21st Congress, 1988, Gulin, China, Oct. 10-15.1988: 646-653. [23] McDonald M G, Harbaugh A W. A Modular three dimensional finite difference groundwater flow model[R]. Washington D.C. : U.S. Geological Survey, 1998. [24] 陈崇希. 地下水混合井流解析模型[J]. 水文地质工程地质, 2012, 39 (5): 1-7. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG201205000.htmChen C X. Analytical model of groundwater flow in multiaquifer wells[J]. Hydrogeology & Engineering Geology, 2012, 39 (5): 1-7(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG201205000.htm [25] 陈崇希. 地下水向集水建筑物的运动[Z]. 武汉: 武汉地质学院, 1981.Chen C X. Groundwater flow to collecting structures[Z]. Wuhan: Wuhan College of Geology, 1981(in Chinese). [26] 陈崇希, 林敏. 地下水动力学[M]. 武汉: 中国地质大学出版社, 1999.Chen C X, Lin M. Groundwater hydraulics[M]. Wuhan: China University of Geosciences Press, 1999(in Chinese). [27] 王旭升, 陈崇希. 改进的Theis井流模型及其解析解-考虑含水层顶板的挠曲作用[J]. 地球科学, 2002, 27(2): 199-202. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200202018.htmWang X S, Chen C X. Analysis of modified Theis model on well flow: Considering bending of the confining stratum[J]. Earth Science, 2002, 27(2): 199-202(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200202018.htm [28] 王旭升, 陈崇希, 焦赳赳. 承压含水层井流-盖层弯曲效应的解析理论[J]. 地球科学, 2003, 28(5): 545-550. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200305012.htmWang X S, Chen C X, Jiao J J. Theory on coupling of radial flow in a confined aquifer and bending of confining unit[J]. Earth Science, 2003, 28(5): 545-550(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200305012.htm [29] Hantush M S, Jacob C E. Non-steady radial flow in an infinite leaky aquifer[J]. Trans. Amer. Geophys. Union, 1955, 36: 95-100. [30] 陈崇希. Dupuit模型的改进: 具入渗补给[J]. 水文地质工程地质, 2020, 47(5): 1-4. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG202106001.htmChen C X. Improvement of Dupuit model: With infiltration recharge[J]. Hydrogeology & Engineering Geology, 2020, 47(5): 1-4(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG202106001.htm [31] 陈崇希, 唐仲华. Theis不稳定潜水井流模型的改进: 具入渗补给[J]. 水文地质工程地质, 2021, 48(6): 1-12. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG202106001.htmChen C X, Tang Z H. Improvement of the Theis unsteady well flow model with infiltration recharge in a phreatic aquifer[J]. Hydrogeology and Engineering Geology, 2021, 48(6): 1-12(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG202106001.htm [32] 陈崇希, 唐仲华, 谢永桦, 等. 有入渗补给的层状非均质含水层圆岛潜水井流模型[J]. 地质科技通报, 2023, 42(4): 15-26. doi: 10.19509/j.cnki.dzkq.tb20220723Chen C X, Tang Z H, Xie Y H, et al. A well flow model for a stratiform heterogenous unconfined aquifer in a round island with infiltration recharge[J]. Bulletin of Geological Science and Technology, 2023, 42(4): 15-26 (in Chinese with English abstract). doi: 10.19509/j.cnki.dzkq.tb20220723 [33] 陈崇希, 万军伟. 孔隙介质非Darcy流基本方程: Forchheimer等公式具通用性吗?[J]. 水利学报, 2011, 42(10): 1257-1259. https://www.cnki.com.cn/Article/CJFDTOTAL-SLXB201110016.htmChen C X, Wan J W. Basic equations for non-Darcy flow in porous media: Are formulas such as Forchheimer's equation universality[J]. Journal of Hydraulic Engineering, 2011, 42(10): 1257-1259(in Chinese). https://www.cnki.com.cn/Article/CJFDTOTAL-SLXB201110016.htm [34] 万军伟, 黄琨, 李银泉, 等. 尼古拉兹圆管沿程水流阻力实验的新发现[J]. 地质科技情报, 2012, 31(5): 157-161. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201205022.htmWan J W, Huang K, Li Y Q, et al. New discovery of Nikuradse's experiments on the law of friction resistance in pipes[J]. Geological Science and Technology Information, 2012, 31(5): 157-161(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201205022.htm [35] Huang K, Wan J W, Chen C X, et al. Experimental investigation on water flow in cubic arrays of spheres[J]. Journal of Hydrology, 2013, 492: 61-68. doi: 10.1016/j.jhydrol.2013.03.039 [36] Huang K, Wan J W, Chen C X, et al. Experiments investigation of the effects of surface roughness on laminar flow in macro tubes[J]. Experimental Thermal and Fluid Science, 2013, 45: 243-248. doi: 10.1016/j.expthermflusci.2012.10.022 [37] Huang K, Wan J W, Chen C X, et al. Experimental investigation on friction factor in pipes with large roughness[J]. Experimental Thermal and Fluid Science, 2013, 50: 147-153. [38] 陈崇希. "防止模拟失真, 提高仿真性"是数值模拟的核心[J]. 水文地质工程地质, 2003, 30(1): 1-5. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG200302001.htmChen C X. "To prevent model loss in reality and improve model accuracy"is the key of groundwater numerical modeling[J]. Hydrogeology & Engineering Geology, 2003, 30 (2): 1-5(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG200302001.htm [39] Nawang W M, Kishi Y. Modelling of salt-water movement in multilayered coastal aquifer at Tanjuang Mas, Malaysia[C]//Anon. Proc. Int. Conf. on calibration and reliability in groundwater modelling. 3–6 September 1990, The Hague, The Netherlands, 1990: 112-119. [40] 陈崇希, 蒋健民, 叶善士, 等. 滨海多层含水系统水资源评价及承压含水层海底等效边界研究: 以广西北海市禾塘水源地为例[R]. 南宁: 广西壮族自治区地质矿产局, 1989.Chen C X, Jiang J M, Ye S S, et al. Waterresources assessment for the coastal multi-aquifer system and studies on equivalent submarine boundary of confine aquifers: An example of the Hetang water head site in Guangxi Province, China[R]. Nanning: Guangxi Geology and Mineral Resources Bureau, 1989(in Chinese). [41] Chen C X, Lin M. Numericalsimulation of the coastal aquifer in Beihai City[C]//Karel K. Proceeding of international conference on calibration and reliability in groundwater modeling (ModelCARE'90), 1990: 67-74. [42] 陈崇希, 林敏, 舒本媛. 滨海承压含水层等效边界: 以北海禾塘水源地为例[J]. 水文地质工程地质, 1990, 17(4): 2-4. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG199004002.htmChen C X, Lin M, Shu B Y. The equivalent drainage boundary of a confined aquifer and its determination in coastal region: A case study in Hetang area of Beihai city, China[J]. Hydrogeology & Engineering Geology, 1990, 17(4): 2-4(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG199004002.htm [43] Chen C X, Lin M, Li G. Modeling of quasi 3-D ground water flow and studying of equivalent drainage boundary in Beihai Penisula, Guangxi[J]. Journal of China University of Geosciences, 1992, 31(1): 105-115. [44] 万军伟, 陈崇希. 海南省洋浦港滨海水源地最大开采量确定方法研究[J]. 勘察科学技术, 1996(6): 6-11. https://www.cnki.com.cn/Article/CJFDTOTAL-KCKX199606001.htmWan J W, Chen C X. The research for method in determining the most exploitation volume of seaside water resource area in Yangpu harbor in Hainan Province [J]. Site Investigation Science and Technology, 1996 (6): 6-11(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-KCKX199606001.htm [45] Cheng J M, Chen C X, Ji M R, Determination of aquifer roof extending under sea from variable-density flow modelling of groundwater response to tide loading: Case study of the Jahe River Basin, Shandong Province, China[J]. Hydrogeology Journal, 2004, 12(4): 408-423. [46] 成建梅, 陈崇希, 吉孟瑞, 等. 山东烟台夹河中、下游地区海水入侵三维水质数值模拟研究[J]. 地学前缘, 2001, 8(1): 179-184. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200101037.htmCheng J M, Chen C X, Ji M R, et al. Three-dimensional numerical study for salt water intrusion in multi-layered coastal aquifers in the Jahe River basin, Shandong province, China[J]. Earth Science Frontiers, 2001, 8(1): 179-184(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200101037.htm [47] 陈崇希, 蒋健民, 林敏, 等. 地下水不稳定混合抽水的渗流-管流耦合模型及其应用[R]. 武汉: 中国地质大学环境地质研究所, 1992.Chen C X, Jiang J M, Lin M, et al. Coupling model of seepage-pipe flow for unsteady groundwater flow in pumping tests with multi-layer wells and its applications[R]. Wuhan: Institute of Environmental Geology, China University of Geosciences, 1992(in Chinese). [48] 陈崇希, 林敏, 叶善士, 等. 地下水混合井流的理论及应用[M]. 武汉: 中国地质大学出版社, 1998.Chen C X, Lin M, Ye S S. Groundwater flow model for mixed wells and its application[M]. Wuhan: China University of Geosciences Press, 1998(in Chinese). [49] Chen C X, Jiao J J. Numerical simulation of pumping test in multilayer wells with non-Darcian flow in the wellbore[J]. Ground Water, 1999, 37(3): 465-474. [50] 陈崇希, 林敏, 叶善士. 郑州市黄河"九五"滩地水源地三个含水层地下水不稳定混合抽水试验确定分层水文地质参数[R]. 武汉: 中国地质大学环境地质研究所, 1995.Chen C X, Lin M, Ye S S. Estimation oflayered hydrogeological parameters from unsteady groundwater pumping tests with multi-layer wells in three aquifers at the water head site on the '95' flood land beside Yellow River, in the Zhengzhou City[R]. Wuhan: Institute of Environmental Geology, China University of Geosciences, 1995(in Chinese). [51] 陈崇希, 刘文波. 陕西渭北东部岩溶水资源数值模拟研究[R]. 武汉: 中国地质大学环境地质研究所, 2003.Chen C X, Liu W B. Numerical modeling study on karst water resources in the eastern part of northern bank of Wei River, Shaanxi Province[R]. Wuhan: Institute of Environmental Geology, China University of Geosciences, 2003(in Chinese). [52] 陈崇希, 黎明. 新疆渭干河流域地下水资源评价[R]. 武汉: 中国地质大学环境地质研究所, 2003.Chen C X, Li M. Groundwater resources assessment for the Weigan River basin[R]. Wuhan: Institute of Environmental Geology, China University of Geosciences, 2003(in Chinese). [53] 陈崇希, 胡立堂. 甘肃黑河干流中游地区地表水-地下水转化数值模拟研究[R]. 武汉: 中国地质大学环境地质研究所, 2004.Chen C X, Hu L T. Numerical modeling study on interaction between surface water and groundwater in the middle reaches area of Heihe River, Gansu Province[R]. Wuhan: Institute of Environmental Geology, China University of Geosciences, 2004(in Chinese). [54] 陈崇希, 韩巍. 甘肃疏勒河流域地下水资源合理配置研究[R]. 武汉: 中国地质大学环境地质研究所, 2005.Chen C X, Han W. Study on rational allocation of groundwater resources in the Shule River basin, Gansu Province[R]. Wuhan: Institute of Environmental Geology, China University of Geosciences, 2005(in Chinese). [55] 陈崇希. 三维地下水流中常规观测孔水位的形成机理及确定方法[J]. 地球科学, 2003, 28(5), 483-491. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200305002.htmChen C X. Forming mechanism and calculating methods of the water level in a conventional observation wellbore on the condition of three dimensional groundwater flow[J]. Earth Science, 2003, 28(5): 483-491(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200305002.htm [56] Hantush M S. Aquifer test on partially penetrating wells[J]. Proc. Am. Soc. Civil Engrs., 1961, 87(5): 171-195. [57] Бочевер Ф М, Веригин Н Н. Методическое пособие посчетам зксплуатащонных запасов подземных воддля Водоснабжения[M]. Москва: Игостроииздат, 1961(in Russian). [58] Neuman S P. Theory of flow in unconfined aquifers considering delayed response of the water table[J]. Water Resources Research, 1972, 18(4): 1031-1045. [59] 陈崇希, 万军伟. 地下水水平井流的模型及数值模拟方法: 考虑井管内不同流态[J]. 地球科学, 2002, 27(2): 135-140. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200202004.htmChen C X, Wan J W. A new model of groundwater flowing to horizontal well and the numerical simulation approach [J]. Earth Science, 2002, 27(2): 135-140(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200202004.htm [60] Chen C X, Wan J W, Zhan H B. Theoretical and experimental studies of coupled seepage-pipe flow to a horizontal well[J]. Journal of Hydrology, 2003, 281(1/2): 163-175. [61] Atkinson T C. Present and future directions in karst hydrogeology[J]. Annales de la Societe Gologique de Belgique, 1985, 108: 293-296. [62] Quinlan R F, Ewers R O. Ground water flow in limestone terrains: Strategy rational and procedure for reliable, efficient monitoring of groundwater quality in karst areas[C]//Anon. Proceedings of the 5th symposium of aquifer restoration and ground water monitoring, National Water Well Association, Columbus, 21-24 May 1985: 197-234. [63] 陈崇希. 岩溶管道-裂隙-空隙三重空隙介质地下水流模型及模拟方法研究[J]. 地球科学, 1995, 20(4): 361-366.Chen C X. Groundwater flow model and simulation method in triple medium of karst tube fissure-pore[J]. Earth Science, 1995, 20(4): 361-366(in Chinese with English abstract). [64] Cheng J M, Chen C X. Preliminary numerical study of karst groundwater flow in Beishan area[C]//Anon. Proceedings of 2nd International Conference of Future Groundwater at Risk. Changchun: 1998, July 13-17: 65-66. [65] Cheng J M, Chen C X. An integrated linear/non-linear flow model for the conduit-fissure-pore media in the Karst triple void aquifer system[J]. Environmental Geology, 2005, 47: 163-174. [66] Clemens T, Hueckinghaus D, Sauter M, et al. A combined continuum and discrete network reactive transport model for simulation of karst development[C]//Anon. Proceedings of the ModelCARE'96 Conference, Golden, CO, USA, 1996: 309-318. [67] Liedl R, Sauter M, Huckinghaus D, et al. Simulation of the development of Karst aquifers using a coupled continuum pipe flow model[J]. Water Resources Research, 2003, 39(3): 1057-1068. [68] Shoemaker W B, Kuniansky E L, Birk S, et al. Documentation of a conduit flow process (CFP) for MODFLOW-2005[R]. U.S. Geol. Surv. Tech. Methods, 6-A24, 2008. [69] 陈崇希, 裴顺平. 地下水开采-地面沉降数值模拟及防治对策研究: 以江苏省苏州市为例[M]. 武汉: 中国地质大学出版社, 2001.Chen C X, Pei S P. Investigations on numerical modeling of groundwater exploitation-land subsidence and control measures: A case study in the Suzhou City, Jiangsu Province[M]. Wuhan: China University of Geosciences Press, 2001(in Chinese). [70] 比利时地质调查所. 长江三角洲上海地区第四纪地质、水文地质、工程地质及地面沉降数学模型研究[R]. 上海: 原上海经济区地质中心, 1989.Belgian Geological Survey. Study on Quaternary geology, hydrogelogy and engineering geology and mathematical model of land subsidence in the Shanghai District, Yangtze River Delta[R]. Shanghai: Former Geological Center of Shanghai Economic Zone, 1989(in Chinese). [71] 陈崇希, 裴顺平. 地下水开采-地面沉降模型研究[J]. 水文地质工程地质, 2001, 28(2): 5-8. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG200102001.htmChen C X, Pei S P. The research on the model of groundwater withdrawal with land subsidence[J]. Hydrogeology & Engineering Geology, 2001, 28(2): 5-8(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG200102001.htm [72] Chen C X, Pei S P, Jiao J J. Land subsidence caused by groundwater exploitation in Suzhou City, China[J]. Hydrogeology Journal, 2003, 11(2): 275-287. [73] 陈崇希, 胡立堂, 王旭升. 地下水流模拟系统PGMS(1.0版)简介[J]. 水文地质工程地质, 2007, 34(6): I-IIChen C X, Hu L T, Wang X S. An introduction to a groundwater flow modeling system, PGMS (version 1.0)[J]. Hydrogeology & Engineering Geology, 2007, 34(6): I-II(in Chinese). [74] 陈崇希, 唐仲华, 胡立堂. 地下水流数值模拟理论方法及模型设计[M]. 北京: 地质出版社, 2014.Chen C X, Tang Z H, Hu L T. Theoretical method and model design for numerical modeling of groundwater flow[M]. Beijing: Geological Publishing House, 2014(in Chinese). [75] 陈崇希. 山东龙口地下水开采-海水入侵问题水文地质模型设计若干问题: 与薛禹群院士商榷[J]. 水利学报, 2015, 46(2): 248-252. https://www.cnki.com.cn/Article/CJFDTOTAL-SLXB201502015.htmChen C X. On problems in hydrgeological model design for sea water intrusion induced by groundwater pumping at the site of Longkou, Shandong Province[J]. Journal of Hydraulic Engineering, 2015, 46(2): 248-252(in Chinese). https://www.cnki.com.cn/Article/CJFDTOTAL-SLXB201502015.htm [76] 陈崇希. 用数值-解析法预测毛里塔尼亚伊迪尼水源地的地下水开采动态[J]. 水文地质工程地质, 1980, 7(4): 8-13.Chen C X. Using analytical-numerical method to predict the groundwater exploited dynamics in the Yi Dini water resource field of Mao Li Tania [J]. Hydrogeology & Engineering Geology, 1980, 7(4): 8-13(in Chinese with English abstract). [77] 陈崇希, 林敏, 方淑镇, 等. 河南省宜阳县韩城勘探区供水水源初步勘探报告第五章: 地下水资源评价[R]. 武汉: 中国地质大学环境地质研究所, 1989.Chen C X, Lin M, Fang S Z, et al. Preliminary investigation report of supply water sources in the Hancheng exploration area, Yiyang County, Henan Province, Chapter 5: Groundwater resources assessment[R]. Wuhan: Institute of Environmental Geology, China University of Geosciences, 1989(in Chinese). [78] 陈崇希, 林敏, 朱伟武, 等. 山西省运城市地下水资源预报与管理模型研究[R]. 武汉: 中国地质大学环境地质研究所, 1991.Chen C X, Lin M, Zhu W W, et al. Study onprediction and management model of groundwater resources in the Yunchen City, Shanxi Province[R]. Wuhan: Institute of Environmental Geology, China University of Geosciences, 1991(in Chinese). [79] 陈崇希, 方淑镇, 林敏. 大同市文英湖地区湖周地下水排水优化管理模型[R]. 武汉: 中国地质大学环境地质研究所, 1992.Chen C X, Fang S Z, Lin M. Optimization management model of groundwater drainage surrounding lakes in the Wenying Lake area, Datong City[R]. Wuhan: Institute of Environmental Geology, China University of Geosciences, 1992(in Chinese). [80] 陈崇希. 湖北省孝感市第四系地下水流模型[R]. 武汉: 中国地质大学环境地质研究所, 1993.Chen C X. Model of groundwater flow in Quaternary sediments in the Xiaogan City, Hubei Province[R]. Wuhan: Institute of Environmental Geology, China University of Geosciences, 1993(in Chinese). [81] 陈崇希, 陈爱光, 区永和. 中关铁矿矿井涌水量预测研究[R]. 北京: 北京地质学院水文地质教研室, 1974.Chen C X, Chen A G, O Y H. Prediction research on groundwater discharge in the iron mines of Zhong Guan[R]. Beijing: Teaching and Research Section of Hydrogeology, Beijing College of Geology, 1974(in Chinese). [82] 程旭学, 陈崇希, 闫成云, 等. 河西走廊疏勒河流域地下水资源合理开发利用调查评价[M]. 北京: 地质出版社, 2008.Cheng X X, Cheng C X, Yan C Y, et al. Ingestigation and assessment on rational groundwater resources utilizationin the Shule River basin, Hexi Corridor[M]. Beijing: Geological Publishing House, 2014(in Chinese). [83] 陈崇希. 地下水资源评价的原则和勘探思想的探讨[C]//地质矿产部水文地质工程地质研究所. 1978年全国第一届地下水资源评价学术研讨会论文集. 北京: 地质出版社, 1982: 22-33.Chen C X. On the principle of groundwater resource estimation and exploration ideas[C]//Institute of Hydrogeology and Engineering geology of Ministry of Geology and Mineral Resources. Proceedings of the first national seminar on groundwater resources assessment (1978). Beijing: Geological Publishing House, 1982: 22-33(in Chinese). [84] 陈崇希, 裴顺平, 王逊. 非完整河的数值模拟方法及建模中的若干问题[J]. 勘察科学技术, 1999(4): 3-6. https://www.cnki.com.cn/Article/CJFDTOTAL-KCKX199904000.htmChen C X, Pei S P, Wang X. The numerical simulated method of partial penetration river and problems in the establishment models[J]. Site Investigation Science and Technology, 1999(4): 3-6(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-KCKX199904000.htm [85] 薛禹群, 谢春红. 地下水数值模拟[M]. 北京: 科学出版社, 2007.Xue Y Q, Xie C H. Numerical modeling of groundwater[M]. Beijing: Science Press, 2007(in Chinese). [86] 陈崇希, 王旭升, 胡立堂. 地下水流数值模拟中抽水井水位的校正[J]. 水利学报, 2007, 38(4): 481-485. https://www.cnki.com.cn/Article/CJFDTOTAL-SLXB200704015.htmChen C X, Wang X S, Hu L T. Emendation of drawdown in pumping wells for numerical modeling of groundwater flow[J]. Journal of Hydraulic Engineering, 2007, 38(4): 481-485(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SLXB200704015.htm [87] 陈崇希, 彭再丰. 晋陕交界处天桥泉域地下水开采模拟研究[R]. 武汉: 中国地质大学环境地质研究所, 1995.Chen C X, Peng Z F. Modeling study on groundwater exploitation in the catchment of Tian Spring on the border of Shanxi Province and Shaanxi Province[R]. Wuhan: Institute of Environmental Geology, China University of Geosciences, 1995(in Chinese). [88] 陈崇希. 滞后补给权系数-降雨补给潜水滞后性处理方法[J]. 水文地质工程地质, 1998, 25(6): 22-24. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG806.006.htmChen C X. Hysteresis recharge weight function method: For solving the rainfall hysteretic recharge to the water table[J]. Hydrogeology & Engineering Geology, 1998, 25(6): 22-24(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG806.006.htm [89] 陈崇希, 黎明, 刘文波. 单斜含水层-泉流系统概念模型研究[J]. 地球科学, 2002, 27(2): 140, 198. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200202005.htmChen C X, Li M, Liu W B. The research for the concept model of the single declining aquifers-spring system[J]. Earth Science, 2002, 27(2): 140, 198(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200202005.htm [90] Tóth J. A theoretical analysis of groundwater flow in small drainage basins[J]. Journal of Geophysics Research, 1963, 68(16): 4795-4812. [91] Bredehoeft J D, Young R A. The temporal allocation of ground water: A simulation approach[J]. Water Resources Research, 1970, 6(1): 3-21. [92] Bredehoeft J D. The water budget myth revisited: Why hydrogeologists model[J]. Ground Water, 2002, 40(4): 340-345. [93] 黎明, 陈崇希, 张明江. 新疆渭干河流域地下水三维流数值模拟[J]. 地质科技情报, 2005, 24(1): 74-78. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200501015.htmLi Min, Chen C X, et al. Numerical simulation of three-dimensional groundwater flow of Weigan River basin, Xinjiang[J]. Geological Science and Technology Information, 2005, 24(1): 74-78(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200501015.htm [94] 韩巍, 胡立堂, 陈崇希, 等. 疏勒河流域玉门-踏实盆地地下水流模型设计中的几个问题的探讨[J]. 勘察科学技术, 2005(1): 15-18. https://www.cnki.com.cn/Article/CJFDTOTAL-KCKX200501004.htmHan W, Hu L T, Chen C X, et al. Problems about numerical simulation of groundwater flow in Yumen-Tashi Basin, Shulehe River, China[J]. Site Investigation Science and Technology, 2005(1): 15-18(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-KCKX200501004.htm [95] 胡立堂, 陈崇希, 钱云平. 黑河中游盆地地下水流建模的若干问题[J]. 人民黄河, 2005, 27(5): 11-13. https://www.cnki.com.cn/Article/CJFDTOTAL-RMHH200505003.htmHu L T, Chen C X, Qian Y P. On problems in modeling of groundwater flow in the middle basin of Heihe River [J]. Yellow River, 2005, 27(5): 11-13(in Chinese). https://www.cnki.com.cn/Article/CJFDTOTAL-RMHH200505003.htm
计量
- 文章访问数: 1150
- PDF下载量: 158
- 被引次数: 0