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2025, 10, v.44 133-137
陕北张家峁煤矿火烧区含水层水化学特征研究
基金项目(Foundation): 中煤科工西安研究院(集团)有限公司科技创新基金项目(2022-XAYJS06); 陕西省自然科学基金重点研发计划项目(2022SF-046)
邮箱(Email): wanghai3777@163.com.;
DOI: 10.13301/j.cnki.ct.2025.10.026
投稿时间: 2024-05-12
投稿日期(年): 2024
修回时间: 2024-05-16
终审时间: 2024-07-08
终审日期(年): 2024
审稿周期(年): 1
发布时间: 2025-09-25
出版时间: 2025-09-25
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摘要:

陕北张家峁煤矿火烧区含水层为强富水含水层,是矿井开采充水的主要水源,存在采掘活动诱发突涌水灾害的风险。以陕北张家峁煤矿火烧区含水层为研究对象,通过对2-2、3-1煤层烧变区含水层水样的采集和分析,研究了火烧区含水层的水化学特征,以及对矿井水的充水模式。研究结果表明,矿区内的风化基岩水、2-2煤层烧变岩水、煤系基岩裂隙水及各地表水的水样以Ca2+离子和HCO3~-离子为主,水质类型为HCO3-Ca型,矿化度多小于0.5 g/L,表明地下水处于氧化环境,其来源主要为地表水或大气降水,循环径流条件较好。3-1煤层烧变岩水矿化度较高(多大于1.0 g/L),阳离子中Na+、Mg2+离子为主,说明地下水循环径流条件较差。后期,将进一步深入研究火烧区含水层水化学特征,随开掘活动的长期演化规律。研究结果对于深入认识矿区的水文地质条件,以及指导烧变岩水害的防治具有一定的参考价值。

Abstract:

The aquifer in the burned area of Zhangjiamao coal mine in northern Shaanxi province is a strong water-rich aquifer, which is the main source of mine water during mining and there is a risk of water inrush disaster induced by mining activities. Takes the aquifer in the burned area of Zhangjiamao coal mine as the research object. By collecting and analyzing water samples from the aquifer in the 2-2 and 3-1 coal seam burning zones, the hydrochemical characteristics of the aquifer in the burned zone and the water filling mode of the mine water are studied. The research results indicate that the weathered bedrock water, 2-2 coal seam burnt rock water, coal bearing bedrock fissure water. The water samples of coal measure bedrock fracture water and surface water are mainly Ca2+ ions and HCO3~- ions,the water quality type is HCO3-Ca type, and the salinity is mostly less than 0.5 g/L, indicating that the groundwater is in an oxidizing environment, its source is mainly surface water or atmospheric precipitation, and the circulating runoff conditions are good. The mineralization degree of the rock water during coal combustion is relatively high(mostly greater than 1.0 g/L), and Na+ and Mg2 + ions are mainly present in the cations, indicating poor conditions for groundwater circulation and runoff. In the later stage, further in-depth research will be conducted on the long-term evolution of the hydrochemical characteristics of the aquifer in the burned area with excavation activities. The research results have certain reference value for a deeper understanding of the hydrogeological conditions in mining areas and for guiding the prevention and control of water damage caused by burnt rocks.

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基本信息:

DOI:10.13301/j.cnki.ct.2025.10.026

中图分类号:TD745

引用信息:

[1]胡俭,呼少平,王海.陕北张家峁煤矿火烧区含水层水化学特征研究[J].煤炭技术,2025,44(10):133-137.DOI:10.13301/j.cnki.ct.2025.10.026.

基金信息:

中煤科工西安研究院(集团)有限公司科技创新基金项目(2022-XAYJS06); 陕西省自然科学基金重点研发计划项目(2022SF-046)

投稿时间:

2024-05-12

投稿日期(年):

2024

修回时间:

2024-05-16

终审时间:

2024-07-08

终审日期(年):

2024

审稿周期(年):

1

发布时间:

2025-09-25

出版时间:

2025-09-25

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