Identification of Mine Water Sources Based on the Spatial and Chemical Characteristics of Bedrock Brines: A Case Study of the Xinli Gold Mine
文献类型：期刊论文
| 作者 | Duan, Xueliang2,3,4; Ma, Fengshan2,3; Gu, Hongyu1; Guo, Jie2,3; Zhao, Haijun2,3; Liu, Guowei2,3,4; Liu, Shuaiqi2,3,4 |
| 刊名 | MINE WATER AND THE ENVIRONMENT
 |
| 出版日期 | 2021-08-10 |
| 页码 | 17 |
| 关键词 | Water inrush Subsea mining Water source identification |
| ISSN号 | 1025-9112 |
| DOI | 10.1007/s10230-021-00810-1 |
| 英文摘要 | Water inrush caused by mining below the seafloor is extremely harmful to mine production. Identifying the sources of mine water can help guide mine water management and sustainable mine development. Saline brines were known to be entering the Xinli Mine, a portion of which lies beneath Laizhou Bay, Shandong Province, China. Preliminary classification of the bedrock brines was determined using hydrochemical analysis and the spatial position of the brines. Four bedrock brine types were identified: shallow, middle, middle high-salinity, and deep. The study area was divided into three levels (shallow, middle, and deep) according to the spatial distribution of the brines. Hierarchical-multi-index analysis (HMIA) was used, along with five pairs of chemical indicators (Cl, delta O-18, Mg, Ca, SO4, Na), to identify the mixing lines for each level. A ternary hybrid model was used to calculate the mixing ratio of mine water from different sources in the shallow sublevels. The bedrock brine classification and water source identification were evaluated by analysis of brine genesis and mixing ratio deviation, respectively. The mixed modes of mine water in the shallow and middle sublevels were seawater-saline water-shallow brine and seawater-saline water-middle brine, respectively. The mixed modes in the deep sublevels were seawater-saline water-deep brine and seawater-saline water-middle brine with a transition between these two modes. Previous studies classified bedrock brine as only one category, and using the mixing ratio greatly improved accuracy. The average proportion of seawater in the mine water has increased over time, but the rate of increased has slowed. In the shallow sublevels, the proportion of seawater in the - 105 m sublevel was higher than that in the - 135 m sublevel, but the difference has decreased every year, indicating that the seawater mainly infiltrates by vertical recharge. The mine water samples from the footwall and in the middle of the - 105 m sublevel were nearly 50% seawater, while the mine water sites on the hanging wall had a relatively low seawater proportion, indicating that the water-conducting fractures were mainly in the footwall. |
| WOS关键词 | INRUSH ; INTRUSION ; ISOTOPES ; AQUIFERS ; DISTRICT ; DEPOSIT ; PILLAR |
| 资助项目 | National Natural Science Foundation of China[41831293] ; National Natural Science Foundation of China[41907174] |
| WOS研究方向 | Water Resources |
| 语种 | 英语 |
| WOS记录号 | WOS:000683628900002 |
| 出版者 | SPRINGER HEIDELBERG |
| 资助机构 | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/101905]  |
| 专题 | 地质与地球物理研究所_中国科学院页岩气与地质工程重点实验室 |
| 通讯作者 | Ma, Fengshan |
| 作者单位 | 1.China Geol Survey, Chengdu Ctr, Chengdu 610081, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Shale Gas & Geoengn, Beijing 100029, Peoples R China 3.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China 4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China |
| 推荐引用方式 GB/T 7714 | Duan, Xueliang,Ma, Fengshan,Gu, Hongyu,et al. Identification of Mine Water Sources Based on the Spatial and Chemical Characteristics of Bedrock Brines: A Case Study of the Xinli Gold Mine[J]. MINE WATER AND THE ENVIRONMENT,2021:17. |
| APA | Duan, Xueliang.,Ma, Fengshan.,Gu, Hongyu.,Guo, Jie.,Zhao, Haijun.,...&Liu, Shuaiqi.(2021).Identification of Mine Water Sources Based on the Spatial and Chemical Characteristics of Bedrock Brines: A Case Study of the Xinli Gold Mine.MINE WATER AND THE ENVIRONMENT,17. |
| MLA | Duan, Xueliang,et al."Identification of Mine Water Sources Based on the Spatial and Chemical Characteristics of Bedrock Brines: A Case Study of the Xinli Gold Mine".MINE WATER AND THE ENVIRONMENT (2021):17. |
入库方式： OAI收割
来源：地质与地球物理研究所
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