鲁中南泰安纸坊泉域岩溶水强径流带成因及特征
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摘要
近年来,鲁中南地区岩溶地下水泉水流量衰减、干涸,水源地超采,岩溶塌陷等环境地质问题日益凸显,迫切需要加强研究。以泰安纸坊泉域为例,探讨了泉域内岩溶水强径流带分布、成因类型及典型水文地质特征,以达到合理开发、保护岩溶地下水的可行性。结果表明,岩溶水强径流带是有巨大调蓄功能并发育于浅部地下水积极交替带的网络状强岩溶富水带,其地下水动态稳定,成井率高且识别特征明显,是本区岩溶水水源地开采的理想场所。研究强径流带系统的水文地质条件,掌握其规律,为进一步研究鲁中南地区岩溶地下水提供了一条有效途径。
In recent years,environmental geological problems,such as,karst groundwater spring water flow attenuation,dryness,water source over-exploitation and karst collapse,have become increasingly apparent in central and southern parts of Shandong Provinces.It is urgent to strengthen this research topic.The distribution,genetic types and typical hydrogeological characteristics of karst water strong run-off belts in the Tai'an Zhifang spring area were investigated in this study In order to achieve the feasibility of rational development and protection of karst groundwater.The results showed that the karst water strong run-off belts was a network-like strong karst water-rich zone with a large regulation function and developed in the active alternating zone of shallow groundwater.The groundwater regime was stable,with a high rate of bore formation and obvious identification characteristics.It is an ideal place for the exploitation of karst water sources in this area.Investigating the hydrogeological conditions of the strong run-off belts system and mastering its laws provided an effective way to further explore the karst groundwater in the central and southern portions of Shandong.
In recent years,environmental geological problems,such as,karst groundwater spring water flow attenuation,dryness,water source over-exploitation and karst collapse,have become increasingly apparent in central and southern parts of Shandong Provinces.It is urgent to strengthen this research topic.The distribution,genetic types and typical hydrogeological characteristics of karst water strong run-off belts in the Tai'an Zhifang spring area were investigated in this study In order to achieve the feasibility of rational development and protection of karst groundwater.The results showed that the karst water strong run-off belts was a network-like strong karst water-rich zone with a large regulation function and developed in the active alternating zone of shallow groundwater.The groundwater regime was stable,with a high rate of bore formation and obvious identification characteristics.It is an ideal place for the exploitation of karst water sources in this area.Investigating the hydrogeological conditions of the strong run-off belts system and mastering its laws provided an effective way to further explore the karst groundwater in the central and southern portions of Shandong.
引文
[1]廖资生.论北方岩溶水资源的开发与管理问题[J].中国岩溶,1985(Z1):107-114.(LIAO Z S.On the development and manage-ment of karst water resources in Northern China[J].Chinese Karst,1985(Z1):107-114.(in Chinese))
[2]梁永平,王维泰.中国北方岩溶水系统划分与系统特征[J].地球学报,2010,31(6):860-868.(LIANG Y P,WANG W T.Division and syst-em characteristics of karst water system in Northern China[J].Earth Journal,2010,31(6):860-868.(in Chinese))
[3]袁道先.中国岩溶学[M].北京:地质出版社,1986.(YUAN D X.Chinese karstology[M].Beijing:Geological Publishing House,1986.(in Chinese))
[4]张凤岐,李博涛.中国北方岩溶地下水系统和开发利用中的几个问题[J].中国岩溶,1990(1):9-16.(ZHANG F Q,LI B T.Several problemsin karst groundwater system and development and utilization in Northern China[J].Chinese Karst,1990(1):9-16.(in Chinese))
[5]王维泰,梁永平,王占辉,等.中国北方气候变化特征及其对岩溶水的影响[J].水文地质工程地质,2012,39(6):6-10,28.(WANG W T,LIANG Y P,WANG Z H,et al.Characteristics of cli-mate change in Northern China and its impact on karst water[J].Hydrogeology&Engineering Geology,2012,39(6):6-10,28.(in Chinese))
[6]刘光亚.岩溶地下水径流带系统[J].河北地质学院学报,1986(Z1):305-326.(LIU G Y.Karst groundwater run-off belts system[J].Journal of Hebei Institute of Geology,1986(Z1):305-326.(in Chinese))
[7]裴捍华,杨亲民,郭振中,等.山西岩溶水强径流带的成因类型及其水文地质特征[J].中国岩溶,2003(3):55-60.(PEI H H,YANG Q M,GUO Z Z,et al.Genetic types and hydrogeological characteristics of karst water and strong run-off belts in Shanxi[J].Chinese Karst,2003(3):55-60.(in Chinese))DOI:10.3969/j.issn.1001-4810.2003.03.008.
[8]方向清,傅耀军,华解明,等.北方岩溶地下水系统模式及特征[J].合肥工业大学学报(自然科学版),2011,34(2):286-291.(FANG X Q,FU Y J,HUA J M,et al.Model and characteristics of karst groundwater system in the Northern China[J].Journal of HeFei University of Technollo-gy(Natural Science),2011,34(2):286-291.(in Chinese))DOI:10.3969/j.issn.1003-5060.2011.02.030.
[9]高宝玉,梁永平,王维泰.柳林泉域岩溶水特点与地质背景条件分析[J].中国岩溶,2008(3):209-214.(GAO B Y,LIANG Y P,WANG W T.Analysis of karst water character ristics and geological background conditions in Liulin spring area[J].Chin-ese Karst,2008(3):209-214.(in Chinese))DOI:10.3969/j.issn.1001-4810.2008.03.003.
[10]梁永平,王维泰,赵春红,等.中国北方岩溶水变化特征及其环境问题[J].中国岩溶,2013,32(1):34-42.(LIANG Y P,WANG W T,ZHAO C H,et al.Variation characteristics of karst water in Northern China and its environmental problems[J].Chinese Karst,2013,32(1):34-42.(in Chinese))DOI:10.3969/j.issn.1001-4810.2013.01.006.
[11]郭高轩,刘文臣,辛宝东,等.北京岩溶水勘查开发的现状与思考[J].南水北调与水利科技,2011,9(2):33-36,45.(GUO G X,LIU W C,XIN B D,et al.The status quo and thinking of karst water exploration and development in Beijing[J].South to North Water Transfers and Water Science&Technology,2011,9(2):33-36,45.(in Chinese))DOI:10.3724/SP.J.1201.2011.02033.
[12]刘建立,朱学愚,钱孝星.中国北方裂隙岩溶水资源开发和保护中若干问题的研究[J].地质学报,2000(4):344-352.(LIU J L,ZHU X Y,QIAN X X.Studyon some problems in the developmentand protection of fractured karst water resources in Northern China[J].Acta Geologica Sinica,2000(4):344-352.(in Chinese))DOI:10.3321/j.issn:0001-5717.2000.04.007.
[13]陈梁,夏家璐.泰安幅1:20万区域水文地质调查报告[R].山东:山东省地质局,1979.(CHEN L,XIA J L.A regional hydrogeological sur-vey of the Tai′an area at 1:20 0000scale[R].Shandong:Geological Bureau.1979.(in Chinese))
[14]贺可强,刘炜金,邵长飞.鲁中南岩溶水资源综合类型及合理调蓄研究[J].地球学报,2002(4):369-374.(HE K Q,LIU W J,SHAO C F.Study on comprehensive types and rational storage of karst water resources in central and southern Shandong province[J].Acta Geoscie-ntica Sinica,2002(4):369-374.(in Chinese))DOI:10.3321/j.issn:1006-3021.2002.04.015.
[15]刘光亚.中国北方的岩溶水强径流带[J].河北地质大学学报,2017,40(2):15-19.(LIU G Y.Karst water strong run-off belts in Northern China[J].Journal of Hebei University of Geology.2017,40(2):15-19.(in Chinese))DOI:10.13937/j.cnki.hbdzdxxb.2017.02.003.
[16]吕朋菊,王念宝.不整合面上的滑脱构造[J].山东矿业学院学报,1985(2):81-83.(LYU P J.WANG N B.Slippage structure on unc-onformity surface[J].Journal of Shandong Mining Institute.1985(2):81-83.(in Chinese))
[17]李理,张进江,钟大赉,等.鲁西地区沿寒武系/太古宇不整合面滑脱构造的主要特征及形成机制[J].地质科学,2007(2):335-352.(LI L,ZHANG J J,ZHONG D L,et al.Main features andformation mechanism of detachment structures along the Cambrian/Archean unconfo-rmity in western Shandong province[J].Geological Science,2007(2):335-352.(in Chinese))DOI:10.3321/j.issn:0563-5020.2007.02.008.
[18]乔光建,梁韵,王斌.邢台百泉岩溶水库蓄水构造特征分析及功能评价[J].南水北调与水利科技,2010,8(1):139-143.(QIAO G J,LIANG Y,WANG B,Characteristics analysis and functional evaluation of water storage structure of Xingtai Baiquan karst reservoir[J].South to North Water Transfers and Water Science&Technology,2010,8(1):139-143.(in Chinese))DOI:10.3969/j.issn.1672-1683.2010.01.038.
[19]束龙仓,张颖,鲁程鹏.管道-裂隙岩溶含水介质非均质性的水文效应[J].南水北调与水利科技,2013,11(1):115-121.(SHU L C,ZHANG Y,LU C P,Hydrological effect of heterogeneity of pipeline-fractured karst aqueous media[J].South to North Water Transfers and Water Sci-ence&Technology,2013,11(1):115-121.(in Chinese))DOI:10.3724/SP.J.1201.2013.01115.
[20]王晓红,刘久荣,辛宝东,等.北京岩溶水系统划分及特征分析[J].城市地质,2016,11(3):8-15.(WANG X H,LIU J R,XIN B D,et al.Divisi-on and characteristics analysis of Beijing karst water system[J].Urban Geology 2016,11(3):8-15.(in Chinese))DOI:10.3969/j.issn.1007-1903.2016.03.002.
[21]胡海涛,许贵森.论构造体系与地下水网络[J].水文地质工程地质,1980(3):1-7.(HU H T,XU G S.Discussion of tectonic systems and groundwater networks[J].Hydrogeology&Engineering Geology,1980(3):1-7.(in Chinese))
[22]奚德荫.鲁中南地区岩溶水文地质条件及其特征[J].中国岩溶,1988(3):43-48.(XI D Y.Karst hydrogeological conditions and theircharacteristics in the central and southern Shandong[J].Chinese Karst,1988(3):43-48.(in Chinese))
[2]梁永平,王维泰.中国北方岩溶水系统划分与系统特征[J].地球学报,2010,31(6):860-868.(LIANG Y P,WANG W T.Division and syst-em characteristics of karst water system in Northern China[J].Earth Journal,2010,31(6):860-868.(in Chinese))
[3]袁道先.中国岩溶学[M].北京:地质出版社,1986.(YUAN D X.Chinese karstology[M].Beijing:Geological Publishing House,1986.(in Chinese))
[4]张凤岐,李博涛.中国北方岩溶地下水系统和开发利用中的几个问题[J].中国岩溶,1990(1):9-16.(ZHANG F Q,LI B T.Several problemsin karst groundwater system and development and utilization in Northern China[J].Chinese Karst,1990(1):9-16.(in Chinese))
[5]王维泰,梁永平,王占辉,等.中国北方气候变化特征及其对岩溶水的影响[J].水文地质工程地质,2012,39(6):6-10,28.(WANG W T,LIANG Y P,WANG Z H,et al.Characteristics of cli-mate change in Northern China and its impact on karst water[J].Hydrogeology&Engineering Geology,2012,39(6):6-10,28.(in Chinese))
[6]刘光亚.岩溶地下水径流带系统[J].河北地质学院学报,1986(Z1):305-326.(LIU G Y.Karst groundwater run-off belts system[J].Journal of Hebei Institute of Geology,1986(Z1):305-326.(in Chinese))
[7]裴捍华,杨亲民,郭振中,等.山西岩溶水强径流带的成因类型及其水文地质特征[J].中国岩溶,2003(3):55-60.(PEI H H,YANG Q M,GUO Z Z,et al.Genetic types and hydrogeological characteristics of karst water and strong run-off belts in Shanxi[J].Chinese Karst,2003(3):55-60.(in Chinese))DOI:10.3969/j.issn.1001-4810.2003.03.008.
[8]方向清,傅耀军,华解明,等.北方岩溶地下水系统模式及特征[J].合肥工业大学学报(自然科学版),2011,34(2):286-291.(FANG X Q,FU Y J,HUA J M,et al.Model and characteristics of karst groundwater system in the Northern China[J].Journal of HeFei University of Technollo-gy(Natural Science),2011,34(2):286-291.(in Chinese))DOI:10.3969/j.issn.1003-5060.2011.02.030.
[9]高宝玉,梁永平,王维泰.柳林泉域岩溶水特点与地质背景条件分析[J].中国岩溶,2008(3):209-214.(GAO B Y,LIANG Y P,WANG W T.Analysis of karst water character ristics and geological background conditions in Liulin spring area[J].Chin-ese Karst,2008(3):209-214.(in Chinese))DOI:10.3969/j.issn.1001-4810.2008.03.003.
[10]梁永平,王维泰,赵春红,等.中国北方岩溶水变化特征及其环境问题[J].中国岩溶,2013,32(1):34-42.(LIANG Y P,WANG W T,ZHAO C H,et al.Variation characteristics of karst water in Northern China and its environmental problems[J].Chinese Karst,2013,32(1):34-42.(in Chinese))DOI:10.3969/j.issn.1001-4810.2013.01.006.
[11]郭高轩,刘文臣,辛宝东,等.北京岩溶水勘查开发的现状与思考[J].南水北调与水利科技,2011,9(2):33-36,45.(GUO G X,LIU W C,XIN B D,et al.The status quo and thinking of karst water exploration and development in Beijing[J].South to North Water Transfers and Water Science&Technology,2011,9(2):33-36,45.(in Chinese))DOI:10.3724/SP.J.1201.2011.02033.
[12]刘建立,朱学愚,钱孝星.中国北方裂隙岩溶水资源开发和保护中若干问题的研究[J].地质学报,2000(4):344-352.(LIU J L,ZHU X Y,QIAN X X.Studyon some problems in the developmentand protection of fractured karst water resources in Northern China[J].Acta Geologica Sinica,2000(4):344-352.(in Chinese))DOI:10.3321/j.issn:0001-5717.2000.04.007.
[13]陈梁,夏家璐.泰安幅1:20万区域水文地质调查报告[R].山东:山东省地质局,1979.(CHEN L,XIA J L.A regional hydrogeological sur-vey of the Tai′an area at 1:20 0000scale[R].Shandong:Geological Bureau.1979.(in Chinese))
[14]贺可强,刘炜金,邵长飞.鲁中南岩溶水资源综合类型及合理调蓄研究[J].地球学报,2002(4):369-374.(HE K Q,LIU W J,SHAO C F.Study on comprehensive types and rational storage of karst water resources in central and southern Shandong province[J].Acta Geoscie-ntica Sinica,2002(4):369-374.(in Chinese))DOI:10.3321/j.issn:1006-3021.2002.04.015.
[15]刘光亚.中国北方的岩溶水强径流带[J].河北地质大学学报,2017,40(2):15-19.(LIU G Y.Karst water strong run-off belts in Northern China[J].Journal of Hebei University of Geology.2017,40(2):15-19.(in Chinese))DOI:10.13937/j.cnki.hbdzdxxb.2017.02.003.
[16]吕朋菊,王念宝.不整合面上的滑脱构造[J].山东矿业学院学报,1985(2):81-83.(LYU P J.WANG N B.Slippage structure on unc-onformity surface[J].Journal of Shandong Mining Institute.1985(2):81-83.(in Chinese))
[17]李理,张进江,钟大赉,等.鲁西地区沿寒武系/太古宇不整合面滑脱构造的主要特征及形成机制[J].地质科学,2007(2):335-352.(LI L,ZHANG J J,ZHONG D L,et al.Main features andformation mechanism of detachment structures along the Cambrian/Archean unconfo-rmity in western Shandong province[J].Geological Science,2007(2):335-352.(in Chinese))DOI:10.3321/j.issn:0563-5020.2007.02.008.
[18]乔光建,梁韵,王斌.邢台百泉岩溶水库蓄水构造特征分析及功能评价[J].南水北调与水利科技,2010,8(1):139-143.(QIAO G J,LIANG Y,WANG B,Characteristics analysis and functional evaluation of water storage structure of Xingtai Baiquan karst reservoir[J].South to North Water Transfers and Water Science&Technology,2010,8(1):139-143.(in Chinese))DOI:10.3969/j.issn.1672-1683.2010.01.038.
[19]束龙仓,张颖,鲁程鹏.管道-裂隙岩溶含水介质非均质性的水文效应[J].南水北调与水利科技,2013,11(1):115-121.(SHU L C,ZHANG Y,LU C P,Hydrological effect of heterogeneity of pipeline-fractured karst aqueous media[J].South to North Water Transfers and Water Sci-ence&Technology,2013,11(1):115-121.(in Chinese))DOI:10.3724/SP.J.1201.2013.01115.
[20]王晓红,刘久荣,辛宝东,等.北京岩溶水系统划分及特征分析[J].城市地质,2016,11(3):8-15.(WANG X H,LIU J R,XIN B D,et al.Divisi-on and characteristics analysis of Beijing karst water system[J].Urban Geology 2016,11(3):8-15.(in Chinese))DOI:10.3969/j.issn.1007-1903.2016.03.002.
[21]胡海涛,许贵森.论构造体系与地下水网络[J].水文地质工程地质,1980(3):1-7.(HU H T,XU G S.Discussion of tectonic systems and groundwater networks[J].Hydrogeology&Engineering Geology,1980(3):1-7.(in Chinese))
[22]奚德荫.鲁中南地区岩溶水文地质条件及其特征[J].中国岩溶,1988(3):43-48.(XI D Y.Karst hydrogeological conditions and theircharacteristics in the central and southern Shandong[J].Chinese Karst,1988(3):43-48.(in Chinese))