首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Subsidence of Kolkata (Calcutta) City, India during the 1990s as observed from space by differential synthetic aperture radar interferometry (D-InSAR) technique
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Subsidence of Kolkata (Calcutta) City, India during the 1990s as observed from space by differential synthetic aperture radar interferometry (D-InSAR) technique

机译:使用差分合成孔径雷达干涉法(D-InSAR)技术从太空观测的1990年代印度加尔各答(Calcutta)市的沉降

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In Kolkata City, India potential land subsidence, due to over-drafting of groundwater under confined condition, has been reported by a number of previous workers and by the local media. The presence of a thick surface clay layer with an average thickness of more than 40 in over the aquifer sand layer raises questions on the possibility and doubtfulness of land subsidence in Kolkata City. In this work, D-InSAR based study has been undertaken to detect and measure land subsidence phenomenon in Kolkata City. For detecting slow land subsidence phenomenon in Kolkata City occurring primarily due to piezometric fall consequent to groundwater overdrafting, we have chosen the InSAR data pairs acquired during post-monsoon (t(1))-pre-monsoon (t(2)) periods when the lowering of piezometric head was the maximum and therefore land subsidence would be more prominent than that of pre-monsoon (t(1))-pre-monsoon (t(2)) and postmonsoon (t(1))-post-monsoon (t(2)) periods of similar time intervals. For detecting slow land subsidence phenomenon essentially from long temporal baseline data pairs (usually in years), temporal clecorrelation and atmospheric artefacts have been found to pose serious difficulties. Adaptive filtering of the noisy interferograms followed by summing of the independent interferograms was performed in complex domain in order to suppress noise from the fringes and highlight the deformation fringes over atmospheric artefacts respectively. Results indicate that an area in Kolkata City surrounded by Machhua Bazar, Calcutta University and Raja Bazar Science College had been undergoing subsidence during the observation period, i.e., 1992-1998 with an estimated rate of 5 to 6.5 imn/year. (c) 2006 Elsevier Inc. All rights reserved.
机译:在印度加尔各答市,先前的许多工人和当地媒体都报道了由于密闭条件下过度透水导致的潜在地面沉降。在加尔各答市,含水层沙层上平均厚度超过40英寸的厚表土层的存在引起了人们对地面沉降的可能性和怀疑的质疑。在这项工作中,已经进行了基于D-InSAR的研究,以检测和测量加尔各答市的地面沉降现象。为了检测加尔各答市的缓慢地面沉降现象,其主要是由于地下水超渗而导致的测压下降而引起的,我们选择了在季风后(t(1))-季风前(t(2))期间采集的InSAR数据对。测压头的下降最大,因此,地面沉降比季风前(t(1))-季风前(t(2))和季风后(t(1))-季风后的沉降更突出(t(2))个时间间隔相似的时间段。为了从基本较长的时间基线数据对(通常以年为单位)检测慢速地面沉降现象,发现时间互相关和大气伪影构成了严重困难。在复杂域中对噪声干涉图进行自适应滤波,然后对独立干涉图求和,以抑制来自条纹的噪声并突出显示大气伪影上的变形条纹。结果表明,加尔各答市内一个被马赫华巴扎尔(Machhua Bazar),加尔各答大学(Calcutta University)和拉贾巴扎尔科学学院(Raja Bazar Science College)包围的地区在观测期内即1992-1998年处于沉降状态,估计速率为5至6.5 imn /年。 (c)2006 Elsevier Inc.保留所有权利。

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