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>Recent ground deformation of Taiyuan basin (China) investigated with C-, L-, and X-bands SAR images
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Recent ground deformation of Taiyuan basin (China) investigated with C-, L-, and X-bands SAR images
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机译:利用C,L和X波段SAR图像研究了太原盆地(中国)最近的地面变形
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摘要
C-, L- and X-bands Synthetic Aperture Radar (SAR) images acquired from November 2006 to June 2011 were processed with Small BAseline Subset DInSAR (SBAS-DInSAR) technique to investigate spatial and temporal variations in deformation over Taiyuan basin, China. The annual deformation rate, created by integrating C-, L- and X-bands interferograms, revealed severe subsidence regions in the basin, where the average subsidence exceeded 10. cm/y and the maximum subsidence reached to 24. cm/y. Meanwhile, it was found that shapes of these subsidence areas were characterized as either subsiding bowls or elongated subsiding belts, implying an intimate connection among groundwater exploration, ground subsidence and faults. Additionally, significant differences in displacement were identified near the faults. This phenomenon could be explained that faults acted as barriers to groundwater flow, impeding the horizontal propagation of fluid-pressure changes and therefore creating groundwater level difference across them. Furthermore, the time series of deformation maps presented inconspicuous nonlinear periodic variations, which might be caused by the seasonal groundwater level fluctuations. In view of the poor water resource and presented features of subsidence over the study area, we deduced that excessive pumping of groundwater was the dominant process driving land subsidence. Our results could provide scientific evidence on a sound management of ground water pumping to mitigate potential damages on infrastructures and environments.
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机译:利用小型BAseline子集DInSAR(SBAS-DInSAR)技术处理了2006年11月至2011年6月采集的C,L和X波段合成孔径雷达(SAR)图像,以研究中国太原盆地变形的时空变化。通过对C,L和X波段干涉图进行积分得出的年变形率显示出盆地中的严重沉降区域,该区域的平均沉降超过10 cm / y,最大沉降达到24. cm / y。同时,发现这些沉降区域的形状以沉降碗或细长沉降带为特征,这暗示着地下水勘探,地面沉降和断层之间的紧密联系。此外,在断层附近发现了位移的显着差异。可以解释这种现象,即断层是阻碍地下水流动的障碍,阻碍了流体压力变化的水平传播,并因此在它们之间产生了地下水位差。此外,形变图的时间序列呈现出不明显的非线性周期性变化,这可能是由地下水位的季节性波动引起的。考虑到水资源匮乏以及研究区域沉降的特点,我们推论出过量抽水是驱动土地沉降的主要过程。我们的结果可以为合理管理地下水泵以减轻对基础设施和环境的潜在损害提供科学依据。
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