云南南洞地下河系统边界及性质研究
|
摘要
地下河系统具有固定补给范围和资源要素,是岩溶地下水进行独立循环的基本单元,控制了岩溶水的运移富集、水化学演化特征、资源构成以及环境地质问题。开展地下河系统研究首要任务是确定系统边界位置及其水文地质性质。以南洞地下河系统为研究对象,据野外调查、勘探、试验资料,以地球系统科学理论为指导,运用现代岩溶学、地质学及水文地质学的分析方法,确定南洞地下河系统是由1号暗河和2号暗河系统组成的,其中2号暗河还有叠置于其上的平石板和黑龙潭两个全排型暗河子系统;其含水岩层主要为三叠系个旧组(T_2g)灰岩、灰质白云岩、白云质灰岩;根据边界的水文地质性质可以划分为地表分水岭边界、地下分水岭边界、隔水边界、岩溶含水层深埋滞留型边界。
With a fixed source of recharge and resource elements, underground river system forms an independent unit in karst groundwater circulation, controlling karst water movement and enrichment, hydrochemical evolution, composition of water resources and environmental geological problems. In order to carry out karst groundwater system research, the primary task is to determine the location of the system boundaries and its hydrogeological properties. In this paper, taking Nandong underground river system as the research object, based on field investigation, exploration, test data, a multi-disciplinary method including modern karstology, geology and hydrogeology are applied. It is conclude that the Nandong underground river system is composed of two subsystems, namely No.1 and No.2 underground river subsystems, and the No.2 underground river system has two full-row type underground subsystems of Pingshiban and Heilongtan.The aquifer is mainly limestone, calcite dolomite and dolomitic limestone of Triassic system. According to the hydrogeological properties of the boundaries, it can be divided into surface watershed boundary, underground watershed boundary, confining boundaries, karst aquifers deep stagnant boundary and other types.
With a fixed source of recharge and resource elements, underground river system forms an independent unit in karst groundwater circulation, controlling karst water movement and enrichment, hydrochemical evolution, composition of water resources and environmental geological problems. In order to carry out karst groundwater system research, the primary task is to determine the location of the system boundaries and its hydrogeological properties. In this paper, taking Nandong underground river system as the research object, based on field investigation, exploration, test data, a multi-disciplinary method including modern karstology, geology and hydrogeology are applied. It is conclude that the Nandong underground river system is composed of two subsystems, namely No.1 and No.2 underground river subsystems, and the No.2 underground river system has two full-row type underground subsystems of Pingshiban and Heilongtan.The aquifer is mainly limestone, calcite dolomite and dolomitic limestone of Triassic system. According to the hydrogeological properties of the boundaries, it can be divided into surface watershed boundary, underground watershed boundary, confining boundaries, karst aquifers deep stagnant boundary and other types.
引文
[1] 王宇.西南岩溶地区岩溶水系统分类、特征及勘查评价要点[J].中国岩溶,2002,21(2):114-119.
[2] 谭继中,谭继泽.云南断陷盆地浅循环岩溶水赋存规律初步研究[J].地质与资源,2003,12(2):91-96.
[3] 王宇,袁道先,杨世瑜.云南省岩溶水系统特征及调查要点[J].云南地质,2007,26(2):131-142.
[4] 康晓波,王宇,张华,等.丽江黑龙潭泉群水文地质特征及断流的影响因素分析[J].中国岩溶,2013,32(4):398-403.
[5] 郭芳,姜光辉,蒋忠诚.中国南方岩溶石山地区不同岩溶类型的地下水与环境地质问题[J].地质科技情报,2006,25(1):83-87.
[6] 袁忠玉,彭淑惠.近年昆明市茨坝-岗头村富水块段地下水位持续下降原因分析[J].中国岩溶,2013,32(3):313-317.
[7] 王宇.裂隙含水层的储存调节功能评价[J].昆明理工大学学报(理工版),2010,35(1):29-32.
[8] 赵春红,李强,梁永平,等.北京西山黑龙关泉域岩溶水系统边界与水文地质性质[J].地球科学进展,2014,29(3):412-419.
[9] 韩冬梅,徐恒力,梁杏.北方岩溶大泉地下水系统的圈划:以太原盆地东西山地区为例[J].地球科学,2006,31(6):885-890.
[10] 裴建国,梁茂珍,陈阵.西南岩溶石山地区岩溶地下水系统划分及其主要特征值统计[J].中国岩溶,2008,27(1):6-10.
[11] 郭清海,王焰新.水文地球化学信息对岩溶地下水流动系统特征的指示意义:以山西神头泉域为例[J].地质科技情报,2006,25(3):85-88.
[12] Aiuppa A,Avino R,Brusca L,et al.Mineal Control of Arsenic Content in Thermal Waters from Volcano-Hosted Hydrothermal Systems:Insight from Island of Ischiaand Phlegrean Fields(Campanian Volcanic Province,Italy)[J].Chemical Geology,229(4):313-330.
[13] 许模,肖维,毛邦燕,等.圆梁山隧道毛坝向斜段岩溶作用强度模拟研究[J].湖南科技大学学报(自然科学版),2010,25(2):36-39.
[14] 武选民,史生胜,黎志恒,等.西北黑河下游额济纳盆地地下水系统研究(上)[J].水文地质工程地质,2002,29(1):16-20.
[15] 武选民,史生胜,黎志恒,等.西北黑河下游额济纳盆地地下水系统研究(下)[J].水文地质工程地质,2002,29(2):30-33.
[16] 王占和,谌天德,于德胜,等.塔里木盆地地下水系统划分[J].新疆地质,2004,22(3):262-264.
[17] 潘曙兰.稳定同位素在太原地区岩溶水资源研究中的应用[J].中国岩溶,1989,8(2):66-70.
[18] 马致远,牛光亮,党学亚,等.鄂尔多斯盆地渭北东部奥陶系岩溶地下水的补给环境[J].地球科学进展,2004(s1):161-165.
[19] 杨吉龙,韩冬梅,苏小四,等.环境同位素特征对滨海岩溶地区海水入侵过程的指示意义[J].地球科学进展,2012,27(12):1344-1352.
[20] 洪义国.硝酸盐氮氧稳定同位素分馏过程记录的海洋氮循环研究进展[J].地球科学进展,2013,28(7):751-764.
[21] 李向全,侯新伟,张宏达,等.太原盆地地下水系统水化学:同位素特征研究[J].干旱区资源与环境,2006,20(5):109-114.
[22] 邓英尔,贾疏源,黄润秋,等.岩溶缝洞系统地下水系研究[J].地球科学进展,2008,23(5):489-494.
[23] 云南省地质矿产局水文工程地质公司.云南省个旧市城市供水水文地质普查报告(1∶5万)[R].1984:14-15.
[24] 云南省地矿局滇南工程勘察公司.云南省南洞地下河系统磨石沟地段工程勘察报告(1∶10000)[R].1994:8-9.
[2] 谭继中,谭继泽.云南断陷盆地浅循环岩溶水赋存规律初步研究[J].地质与资源,2003,12(2):91-96.
[3] 王宇,袁道先,杨世瑜.云南省岩溶水系统特征及调查要点[J].云南地质,2007,26(2):131-142.
[4] 康晓波,王宇,张华,等.丽江黑龙潭泉群水文地质特征及断流的影响因素分析[J].中国岩溶,2013,32(4):398-403.
[5] 郭芳,姜光辉,蒋忠诚.中国南方岩溶石山地区不同岩溶类型的地下水与环境地质问题[J].地质科技情报,2006,25(1):83-87.
[6] 袁忠玉,彭淑惠.近年昆明市茨坝-岗头村富水块段地下水位持续下降原因分析[J].中国岩溶,2013,32(3):313-317.
[7] 王宇.裂隙含水层的储存调节功能评价[J].昆明理工大学学报(理工版),2010,35(1):29-32.
[8] 赵春红,李强,梁永平,等.北京西山黑龙关泉域岩溶水系统边界与水文地质性质[J].地球科学进展,2014,29(3):412-419.
[9] 韩冬梅,徐恒力,梁杏.北方岩溶大泉地下水系统的圈划:以太原盆地东西山地区为例[J].地球科学,2006,31(6):885-890.
[10] 裴建国,梁茂珍,陈阵.西南岩溶石山地区岩溶地下水系统划分及其主要特征值统计[J].中国岩溶,2008,27(1):6-10.
[11] 郭清海,王焰新.水文地球化学信息对岩溶地下水流动系统特征的指示意义:以山西神头泉域为例[J].地质科技情报,2006,25(3):85-88.
[12] Aiuppa A,Avino R,Brusca L,et al.Mineal Control of Arsenic Content in Thermal Waters from Volcano-Hosted Hydrothermal Systems:Insight from Island of Ischiaand Phlegrean Fields(Campanian Volcanic Province,Italy)[J].Chemical Geology,229(4):313-330.
[13] 许模,肖维,毛邦燕,等.圆梁山隧道毛坝向斜段岩溶作用强度模拟研究[J].湖南科技大学学报(自然科学版),2010,25(2):36-39.
[14] 武选民,史生胜,黎志恒,等.西北黑河下游额济纳盆地地下水系统研究(上)[J].水文地质工程地质,2002,29(1):16-20.
[15] 武选民,史生胜,黎志恒,等.西北黑河下游额济纳盆地地下水系统研究(下)[J].水文地质工程地质,2002,29(2):30-33.
[16] 王占和,谌天德,于德胜,等.塔里木盆地地下水系统划分[J].新疆地质,2004,22(3):262-264.
[17] 潘曙兰.稳定同位素在太原地区岩溶水资源研究中的应用[J].中国岩溶,1989,8(2):66-70.
[18] 马致远,牛光亮,党学亚,等.鄂尔多斯盆地渭北东部奥陶系岩溶地下水的补给环境[J].地球科学进展,2004(s1):161-165.
[19] 杨吉龙,韩冬梅,苏小四,等.环境同位素特征对滨海岩溶地区海水入侵过程的指示意义[J].地球科学进展,2012,27(12):1344-1352.
[20] 洪义国.硝酸盐氮氧稳定同位素分馏过程记录的海洋氮循环研究进展[J].地球科学进展,2013,28(7):751-764.
[21] 李向全,侯新伟,张宏达,等.太原盆地地下水系统水化学:同位素特征研究[J].干旱区资源与环境,2006,20(5):109-114.
[22] 邓英尔,贾疏源,黄润秋,等.岩溶缝洞系统地下水系研究[J].地球科学进展,2008,23(5):489-494.
[23] 云南省地质矿产局水文工程地质公司.云南省个旧市城市供水水文地质普查报告(1∶5万)[R].1984:14-15.
[24] 云南省地矿局滇南工程勘察公司.云南省南洞地下河系统磨石沟地段工程勘察报告(1∶10000)[R].1994:8-9.
© 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 |