用户名: 密码: 验证码:
滇中红层地下水富集规律及开发利用研究
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
滇中红层区地处扬子板块西南缘,紧邻哀牢山造山带,地形切割普遍较深,构造发育,岩性组合复杂,冬春季节久旱少雨,农村干旱缺水严重。充分利用地下水的调节作用,开发利用红层地下水资源是抵御旱灾和缓解农村人畜饮水困难的有效手段之一。本文以云南红层地下水勘查示范项目为依托,结合区域水文地质条件,对滇中红层地下水赋存条件、富集规律及开发利用等问题进行了专题研究。
     1、在系统总结研究区域水文地质资料和勘查示范成果基础上,提出了滇中红层地下水分类方案,并按含、隔水层空间组合的差异及富水性的强弱,将层间裂隙含水层进一步划分为单层型、互层型、夹层型三种组合形式;以解决农村人畜饮水为主要目标,兼顾传统划分标准和深井、浅井的差异,建立了滇中红层含水层富水性等级划分标准,即浅井、中深井以40m3/d和15m3/d为界,深井以300m3/d和100m3/d,将滇中红层地下水富水性等级划分为水量丰富、水量中等和水量贫乏三级。
     2、围绕影响红层地下水富集、赋存的主控因素,结合实例,从含水层特征及赋水规律、储水构造型式及机理、汇水地貌特征等方面,系统论述了滇中红层地下水富集条件及规律,并归纳总结了滇中红层富水块段的综合特征。总体上,滇中红层具有地下水类型齐全,储水构造类型多样,风化裂隙水分布局限,层间裂隙含水层和可溶岩层分布广泛,地下水循环径流条件普遍较好,可开发利用的深度较大等特点。
     3、在分析研究滇中红层含盐层的岩性组合、岩石化学特征及赋水空隙发育特点的基础上,论述了滇中红层含盐层地下水水质复杂、富水性差异大的特征,并结合实例探讨了含盐层地下水富集规律及淡水分布特点。
     4、以腰站街盆地为例,对滇中红层典型盆地地下水资源进行了数值模拟分析评价。研究表明,以解决农村生活用水为目标,采用分散的小井小水量开发地下水,将浅井、中深井的抽水试验稳定涌水量作为允许开采量,既可满足缺水农村解决生活用水困难的需要,地下水开采也有资源保证。
     5、对滇中红层地下水开发利用技术进行了研究,归纳总结出“多种形式小口径管井取水,多种方式供水”的红层地下水有效开发及供水方案,提出了钻探、成井、取水的设备配置及工艺,并对劣质水处理进行了探索性研究。论文成果深化了对滇中红层地下水的认识,达到了预期目标,对滇中红层找水与开发利用具有一定的指导和借鉴作用。
Located in southwestern margin of Yangtze Plate and close to Ailaoshan Orogenic Belt, complex geo-environment as well as drought and rainless during winters and springs, the red beds of Central Yunnan groundwater’s exploration and utilization is one of the most efficient methods to resist drought and relieve the drinking water problem of man-livestock. Based on groundwater’s investigation and demonstration data in the red beds of Yunnan, in addition with regional hydrogeology, this paper discusses the condition of existence, groundwater enrichment regularitys and groundwater exploit techniques.
     1. By geological survey and study, in addition with regional hydrogeology, this paper put forward groundwater classification of the red beds of Central Yunnan. New ideas and foundations on classification of interlayered fracture aquifer were launched. According to the differences of space combination between aquifer and aquiclude, in addition with the strong and weak of the water abundance, interlayered fracture aquifer were divided into monolayer, interbeds and interlayer. This paper aim at resolving the drinking water problem of man-livestock, give consideration to the traditional standards and difference among deep well and shallow well. Standard for water abundance was established. This standard was divided into Water yield rich, medium and poor.
     2. Based on main factors controlling groundwater enrichment, combined with the example, This paper described the conditions and regularity of groundwater enrichment and summarized feature synthesis of water rich block from the character of the aquifer and storage regularity, the type of groundwater-bearing structure, characteristics of catchment geomorphy. On the whole, the red beds of Central Yunnan has the following features: The kinds of groundwater are complete; The kinds of groundwater-bearing structure are various; The distribution of groundwater are limited, Widely distributed interlayered fracture aquifer and dissoluble rock; Runoff conditions of groundwater circulation were good; Exploitation and utilization has a good prospect.
     3.Based on analysis of salt layer lithological association, petrochemical characteristics and water enrichment void’development characteristics. This paper described the characteristics of groundwater quality, water abundance’differences. Combined with the example, it discussed the enrichment regularity of saline groundwater, and freshwater’distribution characteristics.
     4. With YaoZhanjie Basin as an example, research indicates that dispersed minor -caliber well were used to exploit and utilize groundwater, at the same time, using pumping test’steady discharge as allowable withdrawal, which meets both the requirements of the drinking water problem of man-livestock as well as groundwater resources assured.
     5. Based on the research of groundwater exploration and utilization in the red beds of Central Yunnan, this paper summarized effective alternative,equipment disposition for groundwater exploration and utilization, and give a exploring study of poor quality water treatment.
     The achievement of this paper has gained a better understanding of the issue of the groundwater in the red beds of Central Yunnan, which can be used for groundwater detection and utilization in this area.
引文
[1]辞典编辑委员会.地球科学大辞典[M].北京:地质出版社, 2006.653.
    [2]程强,寇小兵,黄绍槟,等.中国红层的分布及地质环境特征[J].工程地质学报, 2004,12(01):34~40.
    [3]李廷勇,王建力.中国的红层及发育的地貌类型[J].四川师范大学学报(自然科学版), 2002,25(4):428~431.
    [4]成都地质学院地层古生物教研室.地层学[Z].成都:成都地质学院, 1974:168~200.
    [5]彭华,吴志才.关于红层特点及分布规律的初步探讨[J].中山大学学报(自然科学版), 2003,42(5):109~110.
    [6]徐瑞春.红层与大坝[M].武汉:中国地质大学出版社, 2003.3~10.
    [7]郭永春,谢强,文江泉.我国红层分布特征及主要工程地质问题[J].水文地质工程地质, 2007,(6): 67~71.
    [8]程裕淇主编.中国区域地质概论[M].北京:地质出版社, 1994.395.
    [9]武选民,文冬光,郭建强,等.西部严重缺水地区人畜饮用地下水勘查示范工程[M].北京:中国大地出版社, 2006.39~42.
    [10]袁开先主编.水文地质学[M].北京:水利电力出版社, 1987. 1~5.
    [11]王大纯,张人权,史毅虹,等.水文地质学基础[M].北京:地质出版社,1995.1~5.
    [12] Parker G G. Early stage of hydrogeology in the United States, 1776 to 1912. Water Resources Bulletin, 1986,Vol.22,No.5.
    [13] Theis C V. The relation between the lowering of the diezometric surface and the ratem and duration of discharge of a well using groundwater storage[J]. American Geophysica1 Tranactions, 1935,16(2).
    [14] Hantush M S. Hydraulics of wells, Advances in Hydroscience.American Water Resources Association, 1964,Vol.10.
    [15] Bredehoeft J D. Status of quantitative groundwater hydrology, Advances in Hydroscience. American Water Resources Association, 1976,Vol.10.
    [16] Walker W H,et a1. Preliminary Report on Ground Water Resources of the Havana Region in west-Central Illinois, 1965.
    [17]刘吉成编译.苏联水文地质学发展前景.地质科技动态,地矿部情报研究所,第17期, 1988.
    [18] Bredehoeft J D. Status of Quantitative Groundwater Hydrology.Advances in Groundwater Hydrology. American Water Resources Association, 1976.
    [19] Bredehoeft J D. ,et a1.Ground-water Models. The Vnesco Press, 1982.
    [20] Wang H F, Anderson M P. Introduction to Groundwater Modeling-Finite Difference and Finite Element Methods. W.H.Freeman and Company, 1982.
    [21] Engelen G B. Methodological aspects of regiona1 hydrological systems analysis. 27th International Geological Congress,Vol.Ⅶ, P385~416, 1984.
    [22] Mc Donald M G, Harbaugh A W. A Modular Three-dimensional Finite-difference Ground-water Flow Mode1. U.S. Geological Survey Open-File Report 83~87, 1988.
    [23] Leake S A, Prudic D E. Documentation of a computer program to simulate aquifer-system compaction using the modular finite-difference ground-water flow mode1. U.S.Geological Survey Open-File Report 88~482. 1988.
    [24] Hsieh P A,Freckleton J R. Documentation of a computer program to simulate horizontal-flow barriers using the U.S.Geological Survey modular three-dimensional finite-difference ground -water flow mode1.U.S.Geological Survey Open-File Report 92~477, 1993.
    [25] Joss C J, Baehr A L.An adaptation of the ground-water flowcode MODFLOW to simulate three-dimensional air flow in the unsaturated zone.U.S.Geological Survey Open-File Report. 1995.
    [26]孙纳正.地下水流的数学模型和数值方法[M].北京:地质出版社, 1981.
    [27]林学钰.美国地下水资源管理概况[J].水文地质工程地质, 1983, (2): 52~57.
    [28] Bachmat Y, et a1. Groundwater Management: the use of numerical models. American Geophysical Union, 1980.
    [29] Wi11is R, Yeh W W-G. Groundwater Systems Planning and Management. 1987.
    [30] U.S.Department of the interior water and power resources service. Ground Water Manual. A water resources technical publication. Government Printing Office, 1981.
    [31] Gorelick s M.A review of distributed parameter groundwater management modeling methods. Water Resources Research, Vol.19, No.2,April 1983.
    [32] Anderson M P, Woessner W W. Applied Groundwater Modeling Simulation of Flow and Advective Transport. California: Academic Press, 1992.
    [33]刘本培,蔡运龙,等.地球科学导论[M].北京:高等教育出版社, 2000.
    [34]孙枢,李晓波.我国资源与环境科学近期发展战略刍议.地球科学进展, 2001,16 (5): 726~733.
    [35] Doell P. Will groundwater ease freshwater stress under climate change [J]? Hydrological Sciences Journal, 2009, 54(4).
    [36] Ong, John B. An approach to assessment of flow regimes of groundwater-dominated lakes in arid environments[J]. Journal of Hydrology, 2009,371 (1/4).
    [37] Hess TM. comparison of stochastic and deterministic downscaling methods for modelling potential groundwater recharge under climate change in East Anglia, UK: implications for groundwater resource management[J]. Hydrogeology Journal, 2009,17 (7).
    [38]许广明.地下流体渗流理论与数值模拟[M].北京:地质出版社, 2008.
    [39] Anderman E R, Hill M C. MODFLOW-2000, The U.S.geological survey modular ground-water model-Documentation of the hydrogeologic-unit flow (HUF) package. U.S.Geological Survey Open-File Report 00~342, 2000.
    [40] Carle S F. T-PROGS: A transition probability-based approach to geostatistical characterization of hydrostratigraphic architecture: Ph.D.dissertation, University of California, Davis, 1996.
    [41] Zheng C, Wang P. MT3DMS: A Modular Three-Dimensional Multispecies Transport Model for Simulation of Advection, Dispersion and Chemical Reactions of Contaminants in Groundwater Systems; Documentation and User’s Guide. University of Alabama, 1999.
    [42] Clement T P, Jones N L. RT3D Tutorials for GMS Users, Pacific Northwest National Laboratory Report, PNNL-11805. 1998.
    [43] Jaworska-Szulc B. Groundwater flow modelling of multi-aquifer systems for regional resources evaluation: the Gdansk hydrogeological system, Poland[J]. Hydrogeology journal, 2009,17 (6).
    [44] Wendland F. Groundwater recharge rates for regional groundwater modelling: a case study using GROWA in the Lower Rhine lignite mining area, Germany[J]. Hydrogeology journal, 2009,17(8).
    [45]丁继红,周德亮,马生忠.国外地下水模拟软件的发展现状与趋势[J].勘察科学技术, 2002, (1):37~42.
    [46]贺国平,邵景力,崔亚莉,等. FEFLOW在地下水流模拟方面的应用[J].成都理工大学学报(自然科学版), 2003, 30 (4): 356~ 361.
    [47]贺国平,张彤,赵月芬,等. GMS数值建模方法研究综述[J].地下水, 2007, 29 (3): 32~35.
    [48]祝晓彬.地下水模拟系统(GMS)软件[J].水文地质工程地质, 2003, (5): 53~55.
    [49]石建省.全国地下水资源及其环境问题调查评价总体方案与科技支撑体[A].中国地质调查局编.严重缺水地区地下水勘查论文集(第二集)[C].北京:地质出版社, 2004.8~19.
    [50]仵彦卿.与地下水资源研究有关的UNESCO第6个国际水文计划简介[J].地球科学进展, 2003,18 (1): 21.
    [51] Dean Hayes J.Contractor Speak Out on the State of the Ground Water Industry[J].Water Well Journal, 1998, (4).
    [52] Nevill C J. Managing Cumulative Impacts: Groundwater Reform in the Murray-Darling Basin, Australia[J].Water resources management, 2009,23 (13).
    [53] Birkenholtz T. Groundwater governmentality: hegemony and technologies of resistance in Rajasthan's (India) groundwater governance[J]. Geographical Journal, 2009, 175 (3).
    [54] Moiler D. Groundwater Allocation Using a Groundwater Level Response Management Method -Gnangara Groundwater System, Western Australia[J]. Water resources management, 2009,23 (9).
    [55] Abdel Raouf A R. Groundwater Exploration And Assessment In Rural Communities Of Yobe State, Northern Nigeria[J]. Water Resources Management, 2009,23 (3).
    [56] Apostolaki M G.Estimating Groundwater Withdrawal in Poorly Gauged Agricultural Basins[J]. Water resources management, 2009,23 (6).
    [57]袁道先.以地球系统科学理论推动水文地质学发展[J].水文地质工程地质. 2003, (1): 1.
    [58]韩子夜.地下水勘查与监测技术展望[J].水文地质工程地质. 2007, (2): 81~86.
    [59]刘光亚.基岩地下水[M].北京:地质出版社, 1979.
    [60]卢金凯.基岩裂隙水的野外调查方法[M].北京:地质出版社, 1985.
    [61]成都地质学院红层地下水科研组.四川盆地中部地区侏罗系遂宁组红层地下水及其农灌意义[J].成都地质学院学报, 1974, (1): 2~7.
    [62]成都地质学院红层地下水科研组.某些红色泥岩含水层及其农灌意义[A].国际交流地质学术论文集(5)水文地质工程地质[C].北京:地质出版社, 1974. 76~81.
    [63]边兆祥,任天培.走综合治旱的道路(提纲)——关于如何战胜川中干旱问题的看法[A].我省地质工作建议汇编[C].四川省地质学会, 1980, 63~66.
    [64]任天培.积极开发川中红层地下水资源[J].四川水利, 1981年水利规划专刊, 59~61.
    [65]王告函,施仑山,冯南训.四川盆地红层地下水分布富集特征及开发利用问题[A].四川水文地质专集[C].成都:四川人民出版社, 1981: 47~83.
    [66]罗祥康.川东红层地下水水文地质类型划分[J].四川地质(水文地质工程专辑), 1984,(11): 189~194.
    [67]刘海冲,鲁士魁.四川盆地红层地下水的富集规律与资源评价[J].工程勘察, 1983,(1): 72~74.
    [68]肖玉律.四川盆地中部丘陵区浅层地下水资源评价及开发利用[J].资源科学,1989,(5): 25~32.
    [69]高佩义.川东红层地下水富集与岩层倾角的关系[J].工程勘察, 1983, (1): 75~77.
    [70]卢金凯.对红层地下水富集规律的认识[J].水文地质工程地质, 1981, (4): 26~28.
    [71]周洎馄.南方红层地区找水方向[J].地质论评,1983, (5): 459.
    [72]刘光尧.红层中常见的不良水质[J].水文地质工程地质, 1981, (4): 37~40.
    [73]朱远峰.浙江金华盆地红层地下水系的形成及其分布规律[J].水文地质工程地质, 1985,(2): 57~59.
    [74]王希魁.湖南红层地下水控制因素及赋存规律[J].中国煤田地质, 1990, 2 (2): 41~43.
    [75]苏兆琨.湖南红层地下水类型及其特征[J].湖南地质, 1993, 12 (4): 262~267.
    [76]刘振忠,徐定芳.长沙黄花国际机场水源地的水文地质条件[J].湖南地质,1996,15(4): 209~216.
    [77]陈伟海,黄敬熙,张之淦.小平阳红层区水文地质特征与水资源开发[J].中国岩溶, 1995, 14 (4): 336~341.
    [78]张超岳.红层地下水形成条件及找水方向[J].地下水, 1987, (1): 47~49.
    [79]曹学松.赣东北地区白垩系红层地下水的赋存规律[J].水文地质工程地质, 1994, (2): 34~40.
    [80]朱远峰.红色岩层微孔隙的研究方法及微孔隙发育规律——以浙江金衢盆地为例[J].勘察科学技术, 1986, (3): 1~5.
    [81]徐永新.衡阳红层溶孔水碳酸钙析出的反应机理分析[J].水文地质工程地质,1988, (1):32~34.
    [82]刘光尧编著.山区找水与遥感水文地质方法[M].北京:中国建筑工业出版社, 1986.
    [83]毛文清,温清茂.红层地下水形成环境分析与水文地质分类[J].成都理工学院学报, 1997, 24 (增刊): 142~147.
    [84]李廷强,葛文彬,刘俊贤,等.四川盆地红层地区人畜饮用地下水找水方法初步总结[A].严重缺水地区地下水勘查论文集(第一集)[C].北京:地质出版社, 2003. 48~56.
    [85]鄢毅,王全伟.四川红层区干旱缺水现状及对策[A].严重缺水地区地下水勘查论文集(第一集)[C].北京:地质出版社, 2003. 57~59.
    [86]安永会,张福存,吴登定.红层盆地缺水类型区人畜饮用地下水勘查[A].严重缺水地区地下水勘查论文集(第一集)[C].北京:地质出版社, 2003. 60~62.
    [87]郑荣.红层找水兴国安邦——四川、重庆红层找水示范工程纪实[A].严重缺水地区地下水勘查论文集(第一集)[C].北京:地质出版社, 2003. 197~199.
    [88]鄢毅.川、渝红层地区浅层地下水勘查与开采技术初步研究[A].严重缺水地区地下水勘查论文集(第二集)[C].北京:地质出版社, 2004. 261~268.
    [89]郑万模,魏伦武,赖绍民.西南红层严重缺水区表层地下水富水性等级划分及其意义[A].严重缺水地区地下水勘查论文集(第二集)[C].北京:地质出版社, 2004. 269~274.
    [90]旷正国,樊新庆.重庆西部红层浅层地下水的咸淡水问题[A].严重缺水地区地下水勘查论文集(第二集)[C].北京:地质出版社, 2004. 275~280.
    [91]郭建强,薛忠岐.地球物理技术在地下水资源勘查中的应用[A].严重缺水地区地下水勘查论文集(第二集)[C].北京:地质出版社, 2004. 26~29.
    [92]曹福祥,孙建平.西部地区地下水勘查综合物探技术方法展望[A].严重缺水地区地下水勘查论文集(第二集)[C].北京:地质出版社, 2004. 152~155.
    [93]郑万模,魏伦武,李明辉.西南红层严重缺水地区找水工作[J].沉积与特提斯地质, 2004, 24(4): 106~107.
    [94]许向宁,王兰生,袁永旭.四川盆地红层找水打井工程与防灾减灾[J].地球与环境, 2005, 33(增刊): 364~367.
    [95]张福存,武毅,杨进生.西南红层缺水地区地下水勘查示范[R].中国地质调查局,地质调查成果简本, 2006年第2号.
    [96]张福存,鄢毅,刘安云,等.西南红层浅层地下水特征及其开发利用模式[J].水文地质工程地质, 2008, (3): 53~56.
    [97]张廷山,陈晓慧,姜照勇,等.四川盆地红层区地下水主要赋存特征及影响因素——以南充市为例[J].四川地质学报, 2005,25 (2): 97~100.
    [98]张廷山,陈晓慧,姜照勇,等.川东北红层区地下水赋存特征及合理开发思考[J].水资源与水工程学报, 2006,17 (1): 15~19.
    [99]王学刚,肖华.湖南红层找水初探[J].湖南地质, 2002, 21 (3): 196~199.
    [100]段仲源,寇敏燕,熊智彪,等.红层裂隙水特征与找水方法[J].华东地质学院学报, 2002, 25(4): 283~287.
    [101]苏培东,文敏,袁勇.川中红层区地下水特征及勘探开发方法探讨[J].水文, 2007,27(4):38~40.
    [102]吴恩江,韩宝平,王桂梁.红层中水-岩作用微观信息特征及对孔隙演化的影响——以兖州矿区为例[J].中国矿业大学学报, 2005, 34 (1): 123~128.
    [103]骆银辉,张成亚,饶春富,等.云南红层地下水贮存特征与开发利用途径[J].勘查科学技术, 2006, (2): 46~49.
    [104]李俊东.云南红层分布区地下水赋存规律及农村饮用水供水模式研究[D].北京:中国地质大学, 2005.
    [105]朱春林,李智毅,饶春富,等.滇中红层浅层地下水特征和农村供水示范工程的建立[J].地质通报, 2010, 29 (4): 610~615.
    [106]朱春林,邢志会,饶春富,等.滇中红层含盐层水文地质特征[J].云南地理环境研究, 2009, 21(6): 1~7.
    [107]朱春林,饶春富,邢志会,等.红层地下水开发的经济技术条件[J].云南地理环境研究, 2010, 22 (1): 1~5.
    [108]王宇,朱春林,李燕,等.红层地下水勘查开发的理论及方法[M].北京:地质出版社, 2008.
    [109]沈照理,刘光亚,杨成田,等.水文地质学[M].北京:科学出版社, 1985. 7~14.
    [110]殷昌平,孙庭芳,金良玉,等.地下水源地勘查与评价[M].北京:地质出版社, 1993. 250~251.
    [111]刘忠义.中国古代地下水开发利用浅述[J].地下水. 1987, (3): 186~187.
    [112]田秋菊,牛波,王现国,等.我国基岩地下水开发利用和研究现状[J].地下水, 2004,26(2):88~90.
    [113]骆银辉,周道银,徐世光,等.弱含水层地下水开采技术[J].勘察科学技术, 2008, (3): 49~51.
    [114]张洪叶.水文、水井钻探技术发展方向的探讨[J].探矿工程, 1980, (3): 16~18.
    [115]卢予北.水井工程技术现状与展望[J].探矿工程, 1999, (2): 38~41.
    [116]西部严重缺水地区地下水勘查新技术应用项目组.国内外地下水勘查新技术专集[M].中国地质调查局,2004,71~103, 112~115.
    [117]王平.四川省红层丘陵地区找水打井工程新闻发布会[EB/OL]. http://www.sc.gov.cn/zwgk/ zwdt/xwfb/200706/ t20070629_189419.shtml.
    [118]云南省国土资源厅,云南省地质矿产勘查开发局.云南省红层缺水地区地下水资源勘查开发利用规划[R]. 2007.
    [119]朱春林,饶春富,杨广珠,等.云南红层严重缺水地区地下水勘查示范成果总结与规划建议报告[R].云南省地质调查院. 2006.
    [120]鲁永新.楚雄州干旱分布特征及成因分析[J].楚雄师范学院学报, 2007, 22 (9): 60~65.
    [121]云南省地矿局水文地质工程地质公司.云南省水文地质报告(1:75万)[R]. 1983.
    [122]方晓思,李佩贤等著.滇中侏罗纪红层[M].北京:地质出版社, 2008,Ⅲ-Ⅹ.
    [123]朱同兴,黄志英,尹福光.楚雄中生代前陆盆地的构造沉降史研究[J].沉积与特提斯地质, 2000, 20 (4): 20~30.
    [124]尹福光,万方,许效松,等.楚雄盆地晚三叠世古地理变迁[J].沉积与特提斯地质, 2004, 24(3): 52~57.
    [125]许效松,尹光福,万方,等.楚雄盆地性质与沉积层序演化[J].岩相古地理, 1999, 19 (5): 1~10.
    [126]刘贻军,孟祥化,葛铭.云南楚雄前陆盆地晚三叠世沉积建造及盆地演化[J].现代地质, 1998, 12 (4): 576~581.
    [127]云南省地质局第三地质大队.大姚县石羊盐矿勘探报告[R]. 1963.
    [128]云南省地质局第三地质大队.禄丰县黑井盐矿勘探报告[R]. 1965.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700