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高潜水位采煤沉陷区积水范围动态演化规律
引用本文:陈晓谢,张文涛,朱晓峻,刘辉,张敏,孙爱国,杨晓玉.高潜水位采煤沉陷区积水范围动态演化规律[J].煤田地质与勘探,2020,48(2):126-133.
作者姓名:陈晓谢  张文涛  朱晓峻  刘辉  张敏  孙爱国  杨晓玉
作者单位:安徽大学资源与环境工程学院,安徽合肥 230601;安徽省矿山生态修复工程实验室,安徽合肥 230601;安徽理工大学地球与环境学院,安徽淮南 232001;安徽大学资源与环境工程学院,安徽合肥 230601;安徽省矿山生态修复工程实验室,安徽合肥 230601;河北工程大学矿业与测绘学院,河北邯郸 056038;安徽恒源煤电股份有限公司五沟煤矿,安徽淮北 235131;合肥财经职业学院,安徽合肥 230601
基金项目:国家自然科学基金;安徽省自然科学基金;安徽省高等学校自然科学研究重点项目
摘    要:为了研究高潜水位采煤沉陷区积水范围动态演化规律,以安徽淮北五沟煤矿1031工作面为研究区域,基于Landsat-8遥感数据解译结果,总结了2013-2017年1031工作面上方地表积水范围演化规律,分析净降水量、地下水埋深、工作面推进距离等因素对积水范围演化的影响,并提出积水边界角的概念,建立了积水边界角随采动时间变化的函数关系式。研究发现:高潜水位采煤沉陷区地表积水演化分为4个阶段:未形成期、同步增长期、残余增长期、相对稳定期;在同步增长期和残余增长期,工作面推进距离、净降水量与积水面积日增长量呈正相关,地下水埋深与积水面积日增长量呈负相关;工作面推进距离是积水范围演化的关键影响因素,在工作面推进距离为476 m左右时,地表产生积水,工作面停采后5个月左右,积水面积趋于稳定;积水边界角先呈减小趋势,再趋于稳定,在同步增长期和残余增长期,积水边界角总体呈减小趋势,但受气象、地下水埋深等因素影响而波动;相对稳定期,积水边界角整体趋于90°。本研究为高潜水位采煤沉陷积水区土地利用规划、土地复垦、水陆复合生态系统建立等提供理论依据。

关 键 词:高潜水位  采煤沉陷区  遥感监测  积水演化阶段  积水边界角  五沟煤矿
收稿时间:2019-10-18

Dynamic evolution law of water accumulation range in coal mining subsidence area with high-level groundwater
CHEN Xiaoxie,ZHANG Wentao,ZHU Xiaojun,LIU Hui,ZHANG Min,SUN Aiguo,YANG Xiaoyu.Dynamic evolution law of water accumulation range in coal mining subsidence area with high-level groundwater[J].Coal Geology & Exploration,2020,48(2):126-133.
Authors:CHEN Xiaoxie  ZHANG Wentao  ZHU Xiaojun  LIU Hui  ZHANG Min  SUN Aiguo  YANG Xiaoyu
Institution:(College of Resources and Environmental Engineering,Anhui University,Hefei 230601,China;Anhui Province Engineering Laboratory for Mine Ecological Remediation,Hefei 230601,China;School of Earth and Environment,Anhui University of Science&Technology,Huainan 232001,China;School of Mining and Geomatics,Hebei University of Engineering,Handan 056038,China;Wugou Coal Mine of Anhui Hengyuan Coal Power Co.Ltd.,Huaibei 235131,China;Hefei College of Finance&Economics,Hefei 230601,China)
Abstract:In order to study the dynamic evolution law of the water accumulation range with high-level groundwater, the working face 1031 of Wugou coal mine was taken as the research area. Based on Landsat-8 remote sensing data, the evolution law of water accumulation range above working face 1031 during 2013-2017 was summarized and the influence of factors such as net rainfall, groundwater depth and working surface propulsion distance on the evolution of water accumulation range was analyzed. The concept of the boundary angle of the water accumulation range was proposed, and the functional relationship between the angle and the mining time was established. The study found that the evolution of surface water in the coal mining subsidence area was divided into four periods:unformed, synchronous growth, residual growth, stable. The groundwater depth is negatively correlated with the daily growth of the water accumulation range. The working face advancement distance is the driving factor for the change of the water accumulation range. When the working distance is about 476 m, water is accumulated on the surface, about 5 months after stopping mining, the area of water accumulation range tends to be stable, in the synchronous growth and residual growth period, the angle generally decreases, in the stable period the angle tends to be 90ås a whole, but it fluctuates due to other factors. This study provides a theoretical basis for land use planning, land reclamation, and establishment of a land-water complex ecosystem in the coal mining subsidence area with high-level groundwater. 
Keywords:high-level groundwater  coal mining subsidence area  remote sensing monitoring  evolution of subsidence water accumulation range  the boundary angle of water accumulation range  Wugou coal mine
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