临朐山旺泉天然苏打水形成机理简析
DOI:
作者:
作者单位:

作者简介:

通讯作者:

基金项目:


Primary Analysis on Forming Mechanism of Natural Soda Water in Shanwang Spring in Linqu County
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
    摘要:

    临朐山旺泉苏打水赋存于临朐群牛山组蜂窝状玄武岩中,水质优良,开发前景广阔,该文利用高压反应釜模拟实际地层条件下水岩平衡反应,同时辅以同位素分析,矿物X-射线衍射分析等手段,结合当地特殊的水文地质背景,系统性地阐明了苏打水形成机理。

    Abstract:

    Shanwang spring natural soda water occurred in vesicular basalt rocks in Niushan formation of Linqu group. Its water quanlity is good and has vast exploitable prospect. In this paper, by using high pressure reaction kettle, actual forming conditions of water and rock reaction balance has been simulated. At the same time, with the Isotopic analysis, X-ray diffraction analysis and other means, combining with local special hydrological and geological background, the formation mechanism of soda water has been introduced systematically.

    参考文献
    相似文献
    引证文献
引用本文

杨培杰,赵菲,王元波,白兴港.临朐山旺泉天然苏打水形成机理简析[J].山东国土资源,2016,32(5):

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
历史
  • 收稿日期:
  • 最后修改日期:
  • 录用日期:
  • 在线发布日期: 2016-05-28