羊庄岩溶水系统水化学成因及同位素特征
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摘要
以羊庄岩溶地下水系统为研究对象,通过水化学分析及同位素测试,旨在评价地下水资源,指导开发利用。结果显示:羊庄岩溶地下水系统以现代水为主,在径流过程中主要与灰岩发生水岩相互作用,人类活动对地下水水质的影响较大,岩溶地下水遭受一定程度污染,地下水化学场及水动力场发生不同程度改变。建议相关职能部门采取有效措施抑制地下水污染进一步发展。
Taking Yangzhuang karst groundwater system as the research object, this paper aims at evaluating groundwater resources and guiding the resource development and utilization through hydrochemical analysis and isotope test. The results show that the karst groundwater system in Yangzhuang is dominated by modern water,which mainly interacts with limestone in the course of runoff. Human activities have a great impact on groundwater quality. The karst groundwater is polluted to a certain extent,and groundwater chemical field and hydrodynamic field have changed to different degrees. It is suggested that the relevant functional departments take effective measures to restrain the further development of groundwater pollution.
Taking Yangzhuang karst groundwater system as the research object, this paper aims at evaluating groundwater resources and guiding the resource development and utilization through hydrochemical analysis and isotope test. The results show that the karst groundwater system in Yangzhuang is dominated by modern water,which mainly interacts with limestone in the course of runoff. Human activities have a great impact on groundwater quality. The karst groundwater is polluted to a certain extent,and groundwater chemical field and hydrodynamic field have changed to different degrees. It is suggested that the relevant functional departments take effective measures to restrain the further development of groundwater pollution.
引文
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[2] 袁建飞,邓国仕,徐芬,等.毕节市北部岩溶地下水水文地球化学特征[J].水文地质工程地质,2016,43(1):12-21.
[3] 邓启军,李方红,李伟,等.蒲阳河流域地下水水化学及同位素特征[J].水文地质工程地质,2017,44(2):8-14.
[4] 苗迎,孔祥胜,宋朝静,等.南宁市区地下水水化学特征及形成机制[J].中国岩溶,2015,34(3):228-233.
[5] 隋海波,康凤新,李常锁,等.水化学特征揭示的济北地热水与济南泉水关系[J].中国岩溶,2017,36(1):49-58.
[6] 贾新生,张东,赵志琦,等.南太行山山前平原地下水和地表水氢氧同位素组成及环境意义[J].地球与环境,2016,44(3):281-289.
[7] 王洁青,周训,李晓露,等.云南兰坪盆地羊吃蜜温泉水化学特征与成因分析[J].现代地质,2017,31(4):822-831.
[8] Kodjo Apelete Raoul Kpegli,Abdoukarim Alassane,Rim Trabelsi,et al.Geochemical processes in Kandi Basin,Benin,West Africa:A combined hydrochemistry and stable isotopes approach [J].Quaternary International,2015,369:99-109.
[9] SONG Chao,HAN Guilin,WANG Pan,et al .Hydrochemical and isotope characteristics of spring water discharging from Qiushe Loess Section in Lingtai ,northwestern China and their implication to groundwater recharge [ J ] .Journal of Groundwater Science and Engineering,2017,5(4):364-373.
[10] Carina Zang,Juliane Dame,Marcus Nisser .Hydrochemical and environmental isotope analysis of groundwater and surface water in a dry mountain region in Northern Chile [ J ] .Environ Monit Assess,2018,190:334 .
[11] 沂蒙山区羊庄盆地1∶5万水文地质调查(山亭幅、陶庄幅、枣庄市幅)综合评价报告[R].山东省鲁南地质工程勘察院,2016.
[12] 三上英敏.地下水硝酸汚染に係わる汚染源簡易判定について[EB/OL].http://www.hokkaido-ies.go.jp/new/2009/pdf/seika/hozen.pdf,2010-3-8.
[13] 沈照理,朱宛华,钟佐燊.水文地球化学基础[M].北京:地质出版社,1993.
[14] 张人权,梁杏,靳孟贵,等.水文地质学基础[M].北京:地质出版社,2011.
[15] 薛禹群,张幼宽.地下水污染防治在我国水体污染控制与治理中的双重意义[J].环境科学学报,2009,29(3):474-481 .
[16] 张秋霞,周建伟,康凤新,等.淄博矿区地下水污染水动力和同位素解析[J].环境科学与技术,2016,39(8):116-122 .
[17] 陈新明,甘义群,刘运德,等.长江干流水体氢氧同位素空间分布特征[J].地质科技情报,2011,30(5):110-114 .
[18] 郑淑慧,侯发高,倪葆龄.我国大气降水的氢氧稳定同位素研究[J].科学通报,1982,13:801-806.
[19] 李惠娣.测年方法在地下水中的应用[J].水资源与水工程学报,2008,19(1):1-6.
[20] 中国地质调查局.水文地质手册(第二版)[M].北京:地质出版社,2012.