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Land subsidence characteristics of Ordos using differential interferometry and persistent scatterer interferometry

机译:差分干涉法和持续散射法测量鄂尔多斯市地面沉降特征

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Land displacement in Ordos, China, between 8 January 2007 and 19 January 2011 was mapped using L-band ALOS PALSAR data. Twenty ALOS PALSAR scenes acquired were utilised to generate both PSI and DInSAR results. Several locations in the eastern Ordos experiencing rapid land subsidence were identified including Huo Luo Wan coalmine and Qu Jia Liang coalmine. The subsidence rates ranging from -35mm/year to 35 mm/year were detected. The comparison between PSI and DInSAR outcomes, although showing good agreement in general, reveals some gaps in PSI map near Qu Jia Liang coalmine mainly due to rapid changes within the four-year period. Six successive DInSAR results were exploited to generate time series deformation map, with selected points being analysed and the reason being given for the formation of gaps as well. The DInSAR deformation measurements were then converted into time series velocity maps and integrated with PSI outcome to generate a final product.
机译:使用L波段ALOS PALSAR数据绘制了2007年1月8日至2011年1月19日期间中国鄂尔多斯的土地流失情况。所获取的20个ALOS PALSAR场景用于生成PSI和DInSAR结果。确定了鄂尔多斯东部东部地面沉降迅速的几个地区,包括霍罗湾煤矿和曲家梁煤矿。检测到的沉降速率范围为-35mm /年至35mm /年。 PSI和DInSAR结果之间的比较虽然总体上显示出良好的一致性,但揭示了屈家良煤矿附近PSI地图中的一些差距,这主要是由于四年内的快速变化所致。利用六个连续的DInSAR结果生成时间序列变形图,分析了选定的点,并给出了形成间隙的原因。然后将DInSAR变形测量结果转换为时间序列速度图,并与PSI结果积分以生成最终产品。

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