Progress in the Study on Conjunctive Regulation of Surface Water and Groundwater in Arid Inland River Basins
Received date: 2008-10-01
Revised date: 2008-12-01
Online published: 2009-03-25
Surface water and groundwater conjunctive regulation is an effective approach for solving shortage of water resource in arid inland river basins that is essential significance to the optimum allocation of water resources in arid region. Based on connotations of conjunctive regulation of surface water and groundwater, the present situation on conjunctive regulation of surface water and groundwater was summarized at home and abroad. Some relative study methods were evaluated and shortcomings were pointed out. The research trends of surface water and groundwater conjunctive regulation were prospected. It is proposed that cross discipline collaboration, such as meteorology, ecology, should be paid more attention in formation mechanism of surface water and groundwater conjunctive regulation in the future. The information systems and management model of surface water and groundwater conjunctive regulation were developed for inland rivers. The high-effective use model of water resources based on ecological health and development of environment demand water value method and threshold on environment were discussed in inland rivers. It is suggested that integrated model for synthetic component of water circle is becoming a trend in model development on surface water and groundwater conjunctive regulation.
SUN Dongyuan, Yilihamu, FENG Shengli, ZHAO Chengyi . Progress in the Study on Conjunctive Regulation of Surface Water and Groundwater in Arid Inland River Basins[J]. PROGRESS IN GEOGRAPHY, 2009 , 28(2) : 167 -173 . DOI: 10.11820/dlkxjz.2009.02.002
[1] Sharma P, Sharma R C. Groundwater markets across climatic zones: a comparative analysis of arid and semi-arid zones of Rajasthan. Indian J Agricult Econ., 2004,59(1):138~150.
[2] Tushaar Shah, Singh O P, Aditi Mukherji. Some aspects of South Asia's groundwater irrigation economy: Analyses from a survey in India, Pakistan, Nepal Terai and Bangladesh. Hydrogeology Journal, 2006,14:286~309
[3] 吴红燕,王云智,董新光等. 新疆平原区井渠结合地下水数值 模拟与分析. 地下水,2007,29(2):23~27.
[4] 齐学斌,樊向阳,王景雷等. 井渠结合灌区水资源高效利用调 控模式. 水利学报,2004,(10):119~124.
[5] 周维博, 曾发琛. 井渠结合灌区地下水动态预报及适宜渠井用 水比分析. 灌溉排水学报, 2006,25(1):6~9.
[6] 齐学斌,庞鸿宾,赵辉等. 地表水地下水联合调度研究现状及 其发展趋势. 水科学进展,1999,10(1):89~94.
[7] Matsukawa, Joy, Finney, et al. Conjunctive use planning in Mad River Basin, California. Journal of Water Resources Planning and Management,1992,118(2):115~132.
[8] Basagaoqlu, Hakan,Marino, et al. Joint management of surface and ground water supplies. Ground Water, 1999,37 (2):214~222.
[9] Basagaoqlu, Hakan, Marino, et al.δ-from approximating problem for a conjunctive water resource management model.Advance in Water Resources,1999,23(1):69~81.
[10] Azaiez, M N. A model for conjunctive use of ground and surface water with opportunity costs. European Journal of Operational Research, 2002,143(3):611~624.
[11] Cosgrove, Donna M, Johnson, et al. Transient response functions for conjunctive water management in the Snake River Plain, Idaho. Journal of American Water Resources Association, 2004,40(6): 1469~1482.
[12] Ranganathan C R. Palanisami K. Modeling economics of conjunctive surface and groundwater irrigation systems.Irrigation and Drainage Systems,2004,18:127~143.
[13] Wright A, Toit I. du. Artificial recharge of urban waste- water, the key component in the development of an industrial town on the arid west coast of South Africa.Hydrogeology Journal,1996,4 (1): 118~129.
[14] Lima, Roy F Spalding. Effects of artificial recharge on groundwater quality and aquifer storage recovery.Water Resources Bullet., 1997,33(3):561~572.
[15] Riasat Ali, Jeffrey Turner. A study of the suitability of saline surface water for recharging the hypersaline palaeochannel aquifers of the Eastern Goldfields of Western Australia.Mine Water and the Environment, 2004, 23: 110~118
[16] 徐征和,陈吉亭,刘健勇等. 地下水回灌补源生态修复技术研 究. 地下水,2006,28(3): 78~81.
[17] Silliman S E, Booth D F. Analysis of time series measurements of sediment temperature for identification of gaining vs. losing portions of Juday Creek. J. Hydrol., 1993, 146(4):131~148.
[18] Belanger T V, Walker R B. Groundwater seepage in the Indian River Lagoon. Tropical Hydrology and Caribbean Water Resource, 1990:367~375.
[19] Spalding C P, Khaleel R. An evaluation of analytical solutions to estimate draw downs and stream depletions by wells. Water Resources Research,1991,27(4) :597~609.
[20] 张思聪,吕贤弼,翁文斌等.青岛市水资源管理模型的初步研究. 清华大学学报(自然科学版),1995,38(1):67~70.
[21] Deepak Khare, Jat b M K, Deva Sunder J. Assessment of water resources allocation options: Conjunctive use planning in a link canal command.Resources, Conservation and Recycling,2007, 51: 487~506.
[22] Fleckmenstein J, Anderson M, Fogg G, et al. Managing surface water-groundwater to restore fall flows in the consumes river.Journal of Water Resources Planning and Management, 2004, 130(4): 301~310.
[23] Syaukat, Yuaman, Fox, et al. Conjunctive surface and ground water management in the Jakarta region, Indonesia.Journal of American Water Resources Association,2004,40(1):241~250.
[24] Asaf Sarwar,Helmut Eggers. Development of a conjunctive use model to evaluate alternative management options for surface and groundwater resources.Hydrogeology Journal,2006,14: 1676~1687.
[25] Jobson H E, Harbaugh AW. Modifications to the diffusion analogy surface-water flow model (DAFLOW) for coupling to the modular finite-difference ground-water flow model (MODFLOW). U.S. Geological Survey Open-File Report,1999.
[26] Swain E D. Implementation and use of direct-flow connections in a coupled ground-water and surface-water model.Ground Water, 1994, 32(1):139~144.
[27] Sophocleous M A, Koelliker J K, Govindaraju R S, et al. Integrated numerical modeling for basin -wide water management: The case of the Rattlesnake Creek basin in south -central Kansas. Journal of Hydrology, 1999,214(1-4):179~196.
[28] PandayS, Huyakorn P S. A fully coupled physically-based spatially- distributed model for evaluating surface/subsurface flow.Advances in Water Resources,2004,27(4): 361~382.
[29] 贾仰文,王浩,倪广恒等. 分布式流域水文模型原理与实践. 北京:中国水利水电出版社,2005.
[30] 张奇. 湖泊集水域地表一地下径流联合模拟. 地理科学进展, 2007,26(5):1~10.
[31] 张展羽,高玉芳,李龙昌等. 沿海缺水灌区水资源优化调配耦 合模型. 水利学报,2006,37(10):1246~1252.
[32] 胡立堂. 干旱内陆河地区地表水和地下水集成模型及应用. 水 利学报,2008,39(4):410~418.
[33] 胡立堂,王忠静,赵建世等. 地表水和地下水相互作用及集成 模型研究. 水利学报, 2007,38(1):54~59.
[34] 王蕊,王中根,夏军. 地表水和地下水耦合模型研究进展. 地理 科学进展,2008,27(4):37~41.
[35] Payne B R. The status of isotope hydrology today.Journal Hydrol., 1988,100(1~3):207~237.
[36] Mathieu R T, Bariac. An isotopic study (2H and 18O) on water movements in clayey soils under a semiarid climate. Water Resources Research, 1996,32:779~789.
[37] Yi Yi, Bronwyn E Brock, Matthew D Falcone,et al. A coupled isotope tracer method to characterize input water to lakes.Journal of Hydrology,2007, doi:10.1016/j.jhydrol, 2007.11.008
[38] Bouchaou L, Michelot J L, Vengosh A, et al. Application of multiple isotopic and geochemical tracers for investigation of recharge, salinization, and residence time of water in the Souss – Massa aquifer, southwest of Morocco. Journal of Hydrology, 2008, 352: 267~287.
[39] 聂振龙,陈宗宇,申建梅等. 应用环境同位素方法研究黑河源 区水文循环特征. 地理与地理信息科学,2005, 21(1):104~108.
[40] 张应华,仵彦卿,丁建强等. 运用氧稳定同位素研究黑河中游 盆地地下水与河水转化. 冰川冻土,2005, 27(1):106~110.
[41] 顾正华,唐洪武,李云等. 水流模拟智能化问题的探讨. 水科学 进展,2004,15(1):129~133.
[42] Ioannis N Daliakopoulos, Paulin Coulibaly, Ioannis K Tsanis. Groundwater level forecasting using artificial neural networks. Journal of Hydrology,2005,309:229~240.
[43] Emery A Coppola Jr, Anthony J Rana, Mary M Poulton, et al. A neural network model for predicting aquifer water level elevations. Ground Water,2005,43(2):231~241.
[44] Emery Coppola Jr, Mary Poulton, Emmanuel Charles, et al. Application of artificial neural networks to complex groundwater management problems.Natural Resources Research,2003, 12 (4):303~ 320.
[45] 唐洪武,雷燕,顾正华. 河网水流智能模拟技术及应用. 水科学 进展,2008,19(2):232~37.
[46] 冯绍元,霍再林,康绍忠等. 干旱内陆区自然———人工条件下 地下水位动态的ANN 模型. 水利学报,2007,38(7):873~879.
[47] 陈丁江,吕军,沈晔娜等. 非点源污染河流水质的人工神经网 络模拟. 水利学报,2007,38 (12): 1519~1525.
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