采煤驱动下高潜水位矿区地表水时空特征变化研究:以大屯矿区为例

    Study on spatial-temporal characteristics of surface water change in high underground water mining area that driven by coal mining:a case study of Datun mine area

    • 摘要: 选用1984~2014年六期大屯矿区时间序列的TM/ETM+影像,基于遥感和地理信息系统技术,运用模型(TM3-TM5)/(TM3+TM5)对大屯矿区地表水信息提取,从面积变化进行了宏观分析。并在Fragstats4.0软件平台支持下,借助景观生态学的理论和方法,选取斑块类型面积(CA)、斑块个数(NP)、斑块平均面积(MPS)、景观形状指数(LSI)、面积加权的平均斑块分维数(AWMPFD)、斑块凝聚度(COHESION)、景观破碎度(CI)等指标详细地刻画了地表水资源时空变化特征。研究结果表明,采矿活动将导致地表水面积增长,但增长的表现形式不一。采矿前期主要是表现为面积较小的水域斑块数量的快速增加;采矿中后期则同时表现为水域斑块的融合与单个斑块面积的扩大。此外近年来矿区地表水域破碎化程度在降低,同时其斑块边界愈加复杂、不规则。

       

      Abstract: using Datun mine area’s the sixth phase time-sequenced TM/ETM+ image that the time is 1984~2014,and based on remote sensing(RS) and geographical information system (GIS).To apply model (TM3-TM5)/(TM3+TM5) to extract information of Datun mine area’s surface water.And analyses area change from macroscopic.With the support of software platform Fragstats4.0,also with the help of the methods from landscape ecology,choosing Class Area(CA),Patch Number(NP),Mean Patch Size(MPS),Land Shape Index (LSI),Area Weighted Mean Patch Fractal Dimension (AWMPFD),COHESION,Landscape Fragmentation Index(CI) those indexes and it have detailed carvings of surface water resources spatial-temporal characteristics.The results prove that mining activity will enlarge surface water’s area.But the form of expression is quite different.At the early stage for mining,it shows the quantity of the small patches rise rapidly.At the middle-late stage for mining,it shows the fusion of the patch and single patch’s expansion.Furthermore,recently,the surface water in mining area and it has a lower degree of landscape fragmentation,meanwhile,the border are increasingly complex and irregular.

       

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