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神东矿区地下水变化观测与分析研究

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针对西部大规模高强度煤炭开采对地下水的影响,利用神东矿区约1500 km2区域的200余个钻孔的长期观测结果,研究了超大综采工作面开采工艺对地下水系统的影响规律,地下水流场变化与基岩和含水层空间分布的关系。研究表明,超大综采工作面开采形成了地下水“汇聚带”,开采对基岩和含水层厚度较薄区的地下水系统影响较大,研究区采后含水介质厚度稳定且较厚区域含水层含水厚度损失大部分在30%左右,且逐步趋于稳定。
Observations and analysis of groundwater change in Shendong mining area
The long-term observation data, from over 200 boreholes in Shendong mining area about 1500 km2, have been used for understanding the mining influence on groundwater system by the super-large mechanized face, characteristics with intensive coal mining in west China. It focuses on the relationship between the groundwater flow field and the spatial distribution of bed rock and aquifers. Results show that the super-large face has induced groundwater "convergence zone" and indicate the significant influence on the groundwater system in the area of thin bed rock and thin aquifer. Statistics reveals about 30%of water loss occurred in area with stable and thick aq-uifer after mining in the study area, after then the groundwater system has been gradually stabilized. The research is helpful to the scientific prediction of underground water supply and stored volume, for underground reservoir en-gineering and management.

super-large faceunderground aquifergroundwater flow fieldaquifer loss

顾大钊、张建民、王振荣、曹志国、张凯

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神华集团有限责任公司,北京 100011

神华神东煤炭集团公司,陕西 神木719315

超大工作面 地下含水层 地下水流场 含水层损失

2012BAC10B03

2013

煤田地质与勘探
中煤科工集团西安研究院

煤田地质与勘探

CSTPCDCSCD北大核心
影响因子:1.079
ISSN:1001-1986
年,卷(期):2013.(4)
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