Primary Discussion of Deochemistry Characteristic and Formation of the Mineral Water in the Shuangcheng Basin

张玉敏; 赵焱; 杨诘诺; 安鹏飞

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Primary Discussion of Deochemistry Characteristic and Formation of the Mineral Water in the Shuangcheng Basin

更新时间：2026-01-19

- Primary Discussion of Deochemistry Characteristic and Formation of the Mineral Water in the Shuangcheng Basin
- Issue 2, Pages: 44-46(2011)
- 作者机构：
  
  1. 黑龙江省地质调查研究总院
  2. 黑龙江地质科学研究所
  3. 黑龙江省904水文地质工程地质勘察院
- 作者简介：
- 基金信息：
- DOI：
  CLC： P641.3
- Published：2011
- 稿件说明：
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[1]张玉敏,赵焱,杨诘诺,安鹏飞.双城盆地矿泉水地球化学特征与成因探讨[J].能源研究与管理,2011(02):44-46.

张玉敏, 赵焱, 杨诘诺, et al. Primary Discussion of Deochemistry Characteristic and Formation of the Mineral Water in the Shuangcheng Basin[J]. 2011, (2): 44-46.
[1]张玉敏,赵焱,杨诘诺,安鹏飞.双城盆地矿泉水地球化学特征与成因探讨[J].能源研究与管理,2011(02):44-46. DOI：

张玉敏, 赵焱, 杨诘诺, et al. Primary Discussion of Deochemistry Characteristic and Formation of the Mineral Water in the Shuangcheng Basin[J]. 2011, (2): 44-46. DOI：

摘要

总结了双城盆地地下水化学特征

得出本区地下水为锶质偏硅酸矿泉水

并从水岩作用角度对矿泉水的形成机制进行了分析

结果表明:本区矿泉水主要的成因为含水层上部及含水层岩层经过长期降水渗入、溶滤作用形成可溶解性的锶岩和偏硅酸岩。

Abstract

The chemical characteristics of groundwater in the Shuangcheng Basin were summarized in this paper

which was found to be drink mineral water;And the sources and formation mechanism of Sr and metasilicate in mineral water from the angle of water-rock role were analyzed

to obtain the causes of mineral water are that strontium rocks and metasilicate rock above and in aquifer become soluble in long-term rainfall infiltration and dissolve permeability effect.

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