干旱区生态环境知识资源中心(Arid): 隔水层再造-西北保水采煤关键隔水层N

Arid

	隔水层再造-西北保水采煤关键隔水层N_2红土工程地质研究
其他题名	Reconstruction of aquifuge:The engineering geological study of N_2 laterite located in key aquifuge concerning coal mining with water protection in northwest China
	李文平; 王启庆; 李小琴
来源期刊	煤炭学报
ISSN	0253-9993
出版年	2017
卷号	42 期号:1 页码:88-97
中文摘要	西北干旱-半干旱区浅表层水(河流湖泊水、沟谷径流水、第四系砂层潜水等),是维系区域生态地质环境(生态层)的珍贵水源,是煤层开采水资源保护的主体。根据区域浅表层水含隔水层地质结构,西北煤田煤层覆岩之上广泛分布新近系N_2红土,为浅表层水底部的直接隔水层或沟谷径流的下垫层,对区域保水采煤、生态环境保护,起到至关重要的作用,是关键隔水层。在分析N_2红土区域分布特征、基本物理-水理-力学性基础上,采用N_2红土采动破裂钻孔原位压水试验、蠕变渗透性测试、水-土相互作用试验等,对N_2红土不同程度采动破裂前后及其采后应力恢复蠕变的隔水性能变化特征进行了深入研究分析,发现N_2红土隔水性能受采动破坏后,具有很好的自我恢复功能,并从其地质结构组成、水-土相互作用及其流变特性方面,解释了隔水性自然恢复机理;由此提出隔水层再造及其应具备的主要工程地质属性。
英文摘要	In the arid-semiarid area of northwest China, the shallow water such as the water of rivers and lakes,valley runoff water, the phreatic water of Quaternary in sand-layer and so on are precious water resources which maintain regional ecological geological environment and the body of water resource protection in coal mining.According to the regional geological structure of the shallow water aquifer-aquifuge, the N_2 laterite,distributed widely above coal seam in northwest coal field of China,as the direct aquifuge bottom of regional shallow water or valleys runoff cushion,playing a crucial role to the coal mining with water protection and ecological environment protection, is the key aquifuge soil.In this paper,based on the analysis of regional distribution features, the basic physical,hydro-physical and the mechanical properties of N_2 laterite, the impermeability of post-mining stress recovery creep,before mining crack and post mining was deeply studied and analyzed by the water pressure test before and after mining, the test of creep permeability and the experiment of soil-water interaction and so on.The results show that the N_2 laterite has a good capacity of self-re covery after the impermeability was broken by mining crack.The mechanism of impermeability self-recovery was explained from the perspective of geological structure, soil-water interaction and rheological properties; and according to this finding, the reconstruction of aquifuge and major engineering geological properties included was proposed.
中文关键词	浅表层水 ; N_2红土 ; 采动破裂 ; 水-土相互作用 ; 蠕变 ; 隔水性 ; 隔水层再造
英文关键词	shallow water N_2 laterite mining crack soil-water interactions creep impermeability reconstruction of aquifuge
语种	中文
国家	中国
收录类别	CSCD
WOS类目	MINING MINERAL PROCESSING
WOS研究方向	Mining & Mineral Processing
CSCD记录号	CSCD:5918728
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/236277
作者单位	(徐州)中国矿业大学资源与地球科学学院, 徐州, 江苏 221116, 中国
推荐引用方式 GB/T 7714	李文平,王启庆,李小琴. 隔水层再造-西北保水采煤关键隔水层N_2红土工程地质研究[J],2017,42(1):88-97.
APA	李文平,王启庆,&李小琴.(2017).隔水层再造-西北保水采煤关键隔水层N_2红土工程地质研究.煤炭学报,42(1),88-97.
MLA	李文平,et al."隔水层再造-西北保水采煤关键隔水层N_2红土工程地质研究".煤炭学报 42.1(2017):88-97.