[1]蔡磊,苏晶文,李状,等.新安江流域上游地区地下水化学特征及水文地球化学作用研究[J].华东地质,2023,44(03):262-272.[doi:10.16788/j.hddz.32-1865/P.2023.03.002]
　CAI Lei,SU Jingwen,LI Zhuang,et al.Study on the chemical characteristics and hydrogeochemistry process of groundwater in the upper reaches of Xin’an River Basin[J].East China Geology,2023,44(03):262-272.[doi:10.16788/j.hddz.32-1865/P.2023.03.002]
点击复制

新安江流域上游地区地下水化学特征及水文地球化学作用研究()
分享到：

《华东地质》[ISSN:2096-1871/CN:32-1865/P]

卷:
44
期数:
2023年03期
页码:
262-272
栏目:
长江经济带资源与环境专辑
出版日期:
2023-09-28

文章信息/Info

Title:
Study on the chemical characteristics and hydrogeochemistry process of groundwater in the upper reaches of Xin’an River Basin
作者:
蔡磊1;  苏晶文1;  李状2;  史洪峰1;  王睿1;  杨洋1;  丁勇3
1. 中国地质调查局南京地质调查中心, 江苏 南京 210016;
2. 中国地质调查局天津地质调查中心, 天津 300170;
3. 安徽省地质矿产勘查局332地质队, 安徽 黄山 245000
Author(s):
CAI Lei1;  SU Jingwen1;  LI Zhuang2;  SHI Hongfeng1;  WANG Rui1;  YANG Yang1;  DING Yong3
1. Nanjing Center, China Geological Survey, Nanjing 210016, Jiangsu, China;
2. Tianjin Center, China Geological Survey, Tianjin 300170, China;
3. No. 332 Geological Party, Bureau of Geology and Mineral Resources Exploration of Anhui Province, Huangshan 245000, Anhui, China
关键词:
地下水; 水岩作用; 岩石风化作用; 阳离子交替吸附作用; 新安江流域
Keywords:
groundwater; water-rock interaction; rock weathering; cation alternating adsorption; Xin’an River Basin
分类号:
P641.3
DOI:
10.16788/j.hddz.32-1865/P.2023.03.002
摘要:
新安江流域上游地区地下水水化学成分复杂,水与含水介质间发生的各种溶解、沉淀、吸附等水-岩相互作用在地下水复杂成分形成和演化过程中发挥重要功能。文章采用数理统计、主成分分析和聚类分析、Gibbs模型、硅酸平衡、主要离子比例系数等方法,研究了新安江流域上游地区地下水水化学特征和水文地球化学作用,分析了水化学组分来源。结果表明:研究区地下水阳离子以Ca2+、Na+为主,阴离子以HCO-3为主,还存在少量Cl-、SO2-4,地下水主要水化学类型为HCO3-Ca型、HCO3-Na·Ca型、HCO3-Ca·Mg型;地下水水化学组分主要来自碳酸盐矿物和硅酸盐矿物的风化溶解,其次来源于蒸发岩的风化溶解。地下水的溶滤作用、阳离子交替吸附作用以及人类生产生活等活动共同影响地下水水化学特征。
Abstract:
The chemical composition of groundwater in the upper reaches of Xin’an River Basin is complex. Water-rock interactions such as dissolution, precipitation and adsorption between water and water-bearing medium play an important role in controlling the formation and evolution of complex groundwater components. In this paper, mathematical statistics, principal component and cluster analysis, Gibbs model, silicic acid balance, proportion coefficient of major ions and other methods are used to study the hydrochemistry characteristics and hydrogeochemical process of the groundwater in the upper reaches of Xin’an River Basin, also analyzed the sources of hydrochemical components. The results show that the cations in groundwater in the study area are mainly Ca2+and Na+, the anions are mainly HCO-3, with a small amount of Cl-and SO2-4. The main hydrochemical types of groundwater are HCO3-Ca, HCO3-Na·Ca and HCO3-Ca·Mg. The hydrochemical components of groundwater are mainly derived from the weathering and dissolution of carbonate and silicate minerals, followed by the weathering dissolution of evaporite. The water chemical characteristics of groundwater are affected by the leaching of groundwater, the cation alternating adsorption and human activities.

参考文献/References:

[1] 魏善明,丁冠涛,袁国霞,等.山东省东汶河沂南地区地下水水化学特征及形成机理[J].地质学报, 2021,95(6):1973-1983. WEI S M,DING G T,YUAN G X,et al.Hydrochemical characteristics and formation mechanism of groundwater in Yi’nan, East Wenhe River basin in Shandong Province[J].Acta Geologica Sinica,2021,95(6):1973-1983.
[2] 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,1995:55. WANG D C,ZHANG R Q,SHI Y H,et al.General Hydrogeology[M].Beijing:Geology Press.1995:55.
[3] 栾风娇,周金龙,贾瑞亮,等.新疆巴里坤-伊吾盆地地下水水化学特征及成因[J].环境化学,2017,36(2):380-389. LUAN F J,ZHOU J L,JIA R L,et al.Hydrochemical characteristics and formation mechanism of groundwater in plain areas of Barkol-Yiwu Basin, Xinjiang[J].Environmental Chemistry,2017,36(2):380-389.
[4] GASTMANS D,HUTCHEON I,MENEGáRIO A A,et al.Geochemical evolution of groundwater in a basaltic aquifer based on chemical and stable isotopic data:Case study from the Northeastern portion of Serra Geral Aquifer,S? Paulo state (Brazil)[J].Journal of Hydrology,2016,535:598-611.
[5] CAROL E,KRUSE E,MASPLA J,et al. Hydrochemical and isotopical evidence of groundwater salinization processes on the coastal plain of Samborombón Bay,Argentina[J].Journal of Hydrology,2009,365(3/4):335-345.
[6] 王晓曦,王文科,王周锋,等.滦河下游河水及沿岸地下水水化学特征及其形成作用[J].水文地质工程地质,2014,41(1):25-33. WANG X X,WANG W K,WANG Z F,et al.Hydrochemical characteristics and formation mechanism of river water and groundwater along the downstream Luanhe River,northeastern China[J].Hydrogeology and Engineering Geology,2014,41(1):25-33.
[7] 文冬光,沈照理,钟佐燊.地球化学模拟及其在水文地质中的应用[J].地质科技情报,1995,14(1):99-104. WEN D G,SHEN Z L,ZHONG Z S.Geochemical modeling and its applications in hydrogeology[J].Geological Science and Technology Information,1995,14(1):99-104.
[8] 李义连,王焰新,周来茹,等.地下水矿物饱和度的水文地球化学模拟分析--以娘子关泉域岩溶水为例[J].地质科技情报,2002,21(3):32-36. LI Y L,WANG Y X,ZHOU L R,et al.Hydrogeochemical modeling on saturation of minerals in groundwater:A case study at Niangziguan,Northern China[J].Geological Science and Techology Information,2002,21(3):32-36.
[9] 刘海,康博,沈军辉.基于反向地球化学模拟的地下水形成作用:以安徽省泗县为例[J].现代地质,2019,33(2):440-450. LIU H,KANG B,SHEN J H.Formation of groundwater based on inverse geochemical modeling:A case study from the Sixian County,Anhui Province[J].Geoscience,2019,33(2):440-450.
[10] 刘林,周迅,叶永红.基于多元统计分析的浅层地下水受人为活动影响表征性指标筛选[J].资源调查与环境,2014,35(4):305-310. LIU L,ZHOU X,YE Y H.Screening of characteristic indexes for shallow groundwater influenced by human activities using multivariate statistics[J].Resources Survey and Environment,2014,35(4):305-310.
[11] 金阳,姜月华,周权平,等.丹阳市吕城地区浅层地下水演化特征及成因[J].华东地质,2021,42(4):475-482. JIN Y,JIANG Y H,ZHOU Q P,et al.Evolution characteristics and genesis of shallow groundwater in Lücheng area of Danyang City[J].East China Geology,2021,42(4):475-482.
[12] 中国地质调查局南京地质调查中心.皖江城市群综合地质调查成果报告[R].南京:中国地质调查局南京地质调查中心,2021. Nanjing Center,China Geological Survey.Report on comprehensive geological survey results of Wanjiang Urban Agglomeration[R].Nanjing:Nanjing Center, China Geological Survey,2021.
[13] 李状,苏晶文,董长春,等.安徽马鞍山市当涂地区地下水水化学特征及演化机制[J].中国地质,2022,49(5):1509-1526. LI Z,SU J W,DONG C C,et al. Hydrochemistry characteristics and evolution mechanisms of the groundwater in Dangtu area, Ma’anshan City,Anhui Province[J].Geology in China,2022,49(5):1509-1526.
[14] 刘富环,张起理,祝良祯,等.祁门幅、屯溪幅1:20万区域水文地质普查报告[R].芜湖:安徽省地质矿产局第二水文地质工程地质队,1985. LIU F H,ZHANG Q L,ZHU L Z,et al.1:200000 regional hydrogeological survey report of Qimen Sheet and Tunxi Sheet[R].Wuhu:No.2 Hydrology Engineering Geology Team,Bureau of Geology and Mineral Exploration of Anhui Province,1985.
[15] 张振国,何江涛,王磊,等.衡水地区深层地下水水化学特征及其演化过程[J].现代地质,2018,32(3):565-573. ZHANG Z G,HE J T,WANG L,et al.Hydrochemical characteristics and evolution processes of deep groundwater in Hengshui Area[J].Geoscience,2018,32(3):565-573.
[16] 张景涛,史浙明,王广才,等.柴达木盆地大柴旦地区地下水水化学特征及演化规律[J].地学前缘,2021,28(4):194-205. ZHANG J T,SHI Z M,WANG G C,et al. Hydrochemical characteristics and evolution of groundwater in the Dachaidan area, Qaidam Basin[J].Earth Science Frontiers, 2021,28(4):194-205.
[17] 侯国华,高茂生,党显璋.唐山曹妃甸浅层地下水水化学特征及咸化成因[J].地学前缘,2019,26(6):49-57. HOU G H,GAO M S,DANG X Z.Hydrochemical characteristics and salinization causes of shallow groundwater in Caofeidian,Tangshan City[J].Earth Science Frontiers,2019,26(6):49-57.
[18] 方展,卞建民,孙晓庆,等.吉林省抚松县矿泉水形成机理及过程模拟[J].科学技术与工程,2017,17(14):39-44. FANG Z,BIAN J M,SUN X Q,et al.Mineral water formation mechanism and process modeling in Fusong County[J].Science Technology and Engineering,2017,17(14):39-44.
[19] 董维红,孟莹,王雨山,等.三江平原富锦地区浅层地下水水化学特征及其形成作用[J].吉林大学学报(地球科学版),2017,47(2):542-553. DONG W H,MENG Y,WANG Y S,et al.Hydrochemical characteristics and formation of the shallow groundwater in Fujin,Sanjiang Plain[J].Journal of Jilin University (Earth Science Edition),2017,47(2):542-553.
[20] 安乐生,赵全升,叶思源,等.黄河三角洲浅层地下水化学特征及形成作用[J].环境科学,2012,33(2):370-378. AN L S,ZHAO Q S,YE S Y,et al.Hydrochemical characteristics and formation mechanism of shallow groundwater in the Yellow River Delta[J].Environmental Science,2012,33(2):370-378.

相似文献/References:

[1]李亮,邢怀学,龚建师,等.太湖流域北部地下水化学特征及成因分析[J].华东地质,2022,43(02):217.[doi:10.16788/j.hddz.32-1865/P.2022.02.009]
　LI Liang,XING Huaixue,GONG Jianshi,et al.Hydrochemical characteristics and formation mechanism of groundwater in northern Taihu Lake Basin[J].East China Geology,2022,43(03):217.[doi:10.16788/j.hddz.32-1865/P.2022.02.009]
[2]赵毅斌,刘前进,黄旭娟.瑞金市沙洲坝地区岩溶发育特征与地下水富集规律[J].华东地质,2022,43(02):227.[doi:10.16788/j.hddz.32-1865/P.2022.02.010]
　ZHAO Yibin,LIU Qianjin,HUANG Xujuan.Characteristics of karst development and the law of groundwater enrichment in Shazhouba area of Ruijin City[J].East China Geology,2022,43(03):227.[doi:10.16788/j.hddz.32-1865/P.2022.02.010]
[3]刘前进,黄旭娟,何文城.赣南青塘盆地岩溶水特征及开发利用区划[J].华东地质,2022,43(03):364.[doi:10.16788/j.hddz.32-1865/P.2022.03.012]
　LIU Qianjin,HUANG Xujuan,HE Wencheng.Characteristics and exploitation divisions of karst water in Qingtang Basin, Southern Jiangxi[J].East China Geology,2022,43(03):364.[doi:10.16788/j.hddz.32-1865/P.2022.03.012]
[4]陶小虎,王赫生,龚建师,等.苏北阜宁县地下水水化学特征及成因分析[J].华东地质,2023,44(03):357.[doi:10.16788/j.hddz.32-1865/P.2023.03.011]
　TAO Xiaohu,WANG Hesheng,GONG Jianshi,et al.Hydrochemical characteristics and genesis of the groundwater in Funing County, Northern Jiangsu[J].East China Geology,2023,44(03):357.[doi:10.16788/j.hddz.32-1865/P.2023.03.011]
[5]裴江涛,杨璐,骆祖江.江苏海门地区地面沉降成因分析[J].华东地质,2023,44(04):467.[doi:10.16788/j.hddz.32-1865/P.2023.04.010]
　PEI Jiangtao,YANG Lu,LUO Zujiang.Cause analysis of land subsidence in Haimen area of Jiangsu Province[J].East China Geology,2023,44(03):467.[doi:10.16788/j.hddz.32-1865/P.2023.04.010]

备注/Memo

备注/Memo:
收稿日期:2022-8-23;改回日期:2022-11-14。
基金项目:中国地质调查局"皖江城市群综合地质调查(编号:DD20190261)"和国家重点研发计划课题"城市地下全要素信息集成与智能建模技术(编号:2019YFC0605102)"项目联合资助。
作者简介:蔡磊,1985年生,男,高级工程师,硕士,主要从事水文和环境地质研究工作。Email:cailei329@163.com。
通讯作者:苏晶文,1979年生,女,教授级高级工程师,硕士,主要从事水工环地质调查研究。Email:sjingwen@cgs.cn。
更新日期/Last Update: 1900-01-01