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海底金矿矿坑涌水水源判识及演化研究

李克蓬 马凤山 张洪训 李威 吕英磊

工程地质学报2017,Vol.25Issue(1):180-189,10.
工程地质学报2017,Vol.25Issue(1):180-189,10.DOI:10.13544/j.cnki.jeg.2017.01.024

海底金矿矿坑涌水水源判识及演化研究

RECHARGE SOURCE IDENTIFICATION AND EVOLUTION OF INFLOWING WATER IN A SEABED GOLD MINE

李克蓬 1马凤山 1张洪训 2李威 2吕英磊2

作者信息

  • 1. 中国科学院地质与地球物理研究所,页岩气与地质工程重点实验室 北京 100029
  • 2. 山东黄金矿业(莱州)有限公司三山岛金矿 莱州 261442
  • 折叠

摘要

Abstract

This paper aims to capture the evolution rules of fracture-inflowing water at the shallow depth of Xinli gold deposit exploited undcr seawater.From a hydrogeochemical point of view,it uses the principal component analysis and maximum likelihood method to identify the water-recharging sources of the inflowing water and estimate their mixing ratios.Using numerical modeling,the paper verifies indirectly the inflowing water evolutionary character and calculates it with the proposed method.The research shows that the method can effectively identify the combined patterns and variations of end-members of mine inflowing water,and calculate the most possible mixing ratios.The end-member model of the fracture-inflowing water of the Xinli gold mine has been changed from the type Ⅰ bedrock saline water+seabottom groundwater to the type Ⅰ bedrock saline water+seabottom groundwater+seawater.The sea bottom groundwater and seawater are prone to percolating into the mine pit from the shoulders of its both sides.The seawater percentage of the mine inflowing water goes through an increasing first and decreasing history.

关键词

海底金矿/裂隙涌水/水源判识/混合比/演化

Key words

Seabed gold mine/Fracture-inflowing water/Water-recharging source identification/Mixing ratio/Evolution

分类

矿业与冶金

引用本文复制引用

李克蓬,马凤山,张洪训,李威,吕英磊..海底金矿矿坑涌水水源判识及演化研究[J].工程地质学报,2017,25(1):180-189,10.

基金项目

国家重点研发计划课题(2016YFC0402802),国家自然科学基金项目(41172271,41372323)资助. (2016YFC0402802)

工程地质学报

OA北大核心CSCDCSTPCD

1004-9665

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