Groundwater Source Discrimination and Proportion Determination of Mine Inflow Using Ion Analyses: A Case Study from the Longmen Coal Mine, Henan Province, China; [Differenzierung der Grundwasserherkunft und Bestimmung des Anteils der Bergwässer mittels Ionenanalyse. Eine Fallstudie von der Longmen Kohlengrube in der Provinz Henan in China]; [Discriminación de la fuente de agua subterránea y determianción de la proporción de influjo de agua utilizando análisis de iones — Un caso de estudio en la mina de carbón Longmen, provincia de Henan, China]

被引：0

作者：

Xu Z. ^{[1
,2
]}

Sun Y. ^{[1
,2
]}

Gao S. ^{[1
,2
]}

Zhao X. ^{[1
,2
]}

Duan R. ^{[3
,4
]}

Yao M. ^{[1
,2
]}

Liu Q. ^{[1
,2
]}

机构：

[1] School of Resources and Geosciences, China University of Mining and Technology, Xuzhou

[2] National Engineering Research Center of Coal Mine Water Hazard Controlling, Suzhou

[3] Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing

[4] University of Chinese Academy of Sciences, Beijing

来源：

Mine Water and the Environment | 2018年 / 37卷 / 2期

基金：

中国国家自然科学基金;

关键词：

Mine water disaster prevention; Mine water source identification; Quantitative analysis; Water characteristic ion; Water quality characteristics;

D O I：

10.1007/s10230-018-0512-6

中图分类号：

学科分类号：

摘要：

Complex hydrogeological conditions in China’s coal mines have contributed to frequent mine water disasters. A simple and effective method to determine water inflow sources and paths is therefore essential. The Longmen Mine, located in Henan Province, in central China was used as a case study. A Piper diagram and cluster analysis were used to screen the characteristic values of 18 water samples from potential aquifers. A comprehensive fuzzy evaluation of the groundwater ions was carried out to determine the main source of the total mine inflow. Then, based on conservation of ionic masses, a matrix function was established to calculate the groundwater recharge composition. Finally, using measured water inflows for the Cambrian limestone aquifer, the calculated and observed results were compared. The results showed that the Carboniferous Taiyuan Formation limestone aquifer (the L7 limestone aquifer) accounts for 60.8% of the total mine inflow, while the Cambrian limestone and roof sandstone aquifers account for 34.8 and 4.4% of the inflow, respectively. The normal mine inflow totals about 19,200 m3/day, of which 6,840 m3/day is from the Cambrian limestone aquifer. This agrees well with the calculated value of 6,720 m3/day. Thus, the method is feasible and reliable. © 2018, The Author(s).

引用

页码：385 / 392

页数：7

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