2021 Vol. 37, No. 9
Article Contents

WANG Milei, DOU Yanguang, ZOU Liang, XUE Biying, HU Rui, YUE Baojing, XU Gang, LIN Xi, LI Linsen. HYDROCHEMICAL CHARACTERISTICS OF GROUNDWATER AND GENESIS OF MINERAL WATER AT LAOSHAN MOUNTAIN AND SURROUNDING AREAS, QINGDAO[J]. Marine Geology Frontiers, 2021, 37(9): 17-24. doi: 10.16028/j.1009-2722.2021.126
Citation: WANG Milei, DOU Yanguang, ZOU Liang, XUE Biying, HU Rui, YUE Baojing, XU Gang, LIN Xi, LI Linsen. HYDROCHEMICAL CHARACTERISTICS OF GROUNDWATER AND GENESIS OF MINERAL WATER AT LAOSHAN MOUNTAIN AND SURROUNDING AREAS, QINGDAO[J]. Marine Geology Frontiers, 2021, 37(9): 17-24. doi: 10.16028/j.1009-2722.2021.126

HYDROCHEMICAL CHARACTERISTICS OF GROUNDWATER AND GENESIS OF MINERAL WATER AT LAOSHAN MOUNTAIN AND SURROUNDING AREAS, QINGDAO

More Information
  • The Laoshan Mountain and its surrounding areas are rich in mineral water under the joint control of structural faults and weathering granite crust. In this paper, 14 hydrogeological wells are selected from the area surrounding the Laoshan Mountain for revealing the hydrogeological characteristics and concerned problems. The main hydrogeological problems are concentrated in the middle and lower reaches of rivers where human activities are frequent and active. Both industrial and agricultural pollution leads to the excess of nitrate in groundwater, in addition to saltwater intrusion occurred in the nearshore areas. A mineral water well located in the weathered crust of granite was discovered this time in the Lanseguigu District. The groundwater in the well belongs to the type of HCO3·SO4-Ca·Na. The contents of strontium (Sr) and metasilicic acid (H2SiO3) of the groundwater are 0.66 and 25.49 mg/L respectively, which are both higher than the standard content for drinking natural mineral water. The formation of the mineral water is closely related to the geological environment of the Laoshan area and mineral compositions of surrounding rocks. The strontium-metasilicic acid mineral water is formed by the dissolution of strontium and silica from granite into water by a long term water-rock interaction. This discovery is significant and may provide a new mineral water producing area in the Laoshan region of Qingdao.

  • 加载中
  • [1] 范典高,段本春. 青岛即墨东北部地区基岩富水区新探[J]. 青岛海洋大学学报,1999,29(2):296-300.

    Google Scholar

    [2] 中华人民共和国国家卫生健康委员会, 国家市场监督管理总局. GB 8537—2018食品安全国家标准 饮用天然矿泉水[S]. 北京: 中国标准出版社, 2018.

    Google Scholar

    [3] 胡琴耀. 曲水矿泉水文地球化学特征与水资源评价[D]. 南昌: 东华理工大学, 2016.

    Google Scholar

    [4] 安可士. 我国饮用天然矿泉水开发现状及主要问题[J]. 华北地质矿场杂志,1999(4):341-346.

    Google Scholar

    [5] 危润初. 靖宇国家级自然保护区天然矿泉水形成机理研究[D]. 长春: 吉林大学, 2014.

    Google Scholar

    [6] 赵广涛,李玉瑛,曹钦臣,等. 青岛西北地区矿泉水的水化学特征与形成机理[J]. 青岛海洋大学学报,1998,28(1):135-141.

    Google Scholar

    [7] 孙岩. 青岛地区矿泉水的分类及分布规律[J]. 海洋地质与第四纪地质,1997,17(1):95-100.

    Google Scholar

    [8] 孙嘉诗. 崂山饮用天然矿泉水[J]. 海洋地质与第四纪地质. 1996, 16(增刊.): 85-87.

    Google Scholar

    [9] 赵永军,孙春燕,于典军. 崂山区饮用水生产行业现状及发展对策[J]. 山东水利,2004,7:22-23. doi: 10.3969/j.issn.1009-6159.2004.01.015

    CrossRef Google Scholar

    [10] 谭长伟. 变质岩区地下水富集规律的探讨[J]. 地下水, 1992, 14(2): 115-118.

    Google Scholar

    [11] 宋健,唐方头,邓志辉,等. 沧口断裂黄岛断裂几何结构和活动特征[J]. 北京大学学报(自然科学版),2017,53:1020.

    Google Scholar

    [12] 郭玉贵,金秉福,秦小光,等. 青岛沧口断裂的地质构造特征与第四纪活动性研究[J]. 震灾防御技术,2007,2(2):101-115. doi: 10.3969/j.issn.1673-5722.2007.02.001

    CrossRef Google Scholar

    [13] 栾光忠,任鲁川,段本春. 青岛及其邻区NE、NW向断裂的活动性研究[J]. 青岛海洋大学学报,1999,29(4):727-732.

    Google Scholar

    [14] 高雅洁. 中国东部中生代板内花岗岩成因及构造意义——以崂山花岗岩为例[D]. 青岛: 中国科学院海洋研究所.

    Google Scholar

    [15] 赵广涛,王德滋,曹钦臣,等. I-A型复合花岗岩体的热演化及其意义:以崂山花岗岩体为例[J]. 中国科学(D辑):地球科学,1998,28(4):296-302.

    Google Scholar

    [16] 郭良, 相石宝, 徐兴永. 山东崂山花岗岩地质地貌特征[J]. 地质评论. 2007, 53(增刊): 138-143.

    Google Scholar

    [17] 张保民. 青岛崂山花岗岩构造断裂系的含水性[J]. 山东地质. 1990, 6(1): 26-33.

    Google Scholar

    [18] 赵广涛, 曹钦臣, 孙跃鹏. 崂山花岗岩地区含锶、偏硅酸矿泉水的形成机理[J] 青岛海洋大学学报, 1996, 26(2): 239-246.

    Google Scholar

    [19] 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.

    Google Scholar

    [20] 沈照理, 朱宛华, 钟左燊. 水文地球化学基础[M]. 北京: 地质出版社, 1993.

    Google Scholar

    [21] 敬海霞,黄江华,葛旭,等. 安徽省舒城县柳抱泉天然饮用矿泉水水质特征及成因分析[J]. 地下水,2018,40(4):43-44,85. doi: 10.3969/j.issn.1004-1184.2018.04.012

    CrossRef Google Scholar

    [22] 谢厥琼. 广东省偏硅酸型饮用天然矿泉水水质特征、形成条件及水源地类型[J]. 广东地质,1998,13(3):39-43.

    Google Scholar

  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(5)

Tables(2)

Article Metrics

Article views(2243) PDF downloads(115) Cited by(0)

Access History

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint