利用DinSAR方法估算印尼西苏门答腊岛巴东市ALOS PALSAR图像的地面沉降

Rahmi Sukmawati, M. Waqar, -. Syafriani, -. Yohandri, J. T. S. Sumantyo
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引用次数: 1

摘要

地面沉降在世界各地的大城市和印度尼西亚都有发生。巴东作为西苏门答腊最大的城市之一,也面临着由于自然现象和人为诱发的地面沉降问题。巴东市位于苏门答腊岛西海岸,是导致频繁地震的三个活动板块的交汇点。本研究的主要目的是利用DInSAR方法了解巴东地区受地表沉降影响面积的分布、地表沉降的估计数值以及地表沉降速度的数值。本研究使用的数据是巴东市2007 - 2010年ALOS PALSAR 1.1级图像,由日本千叶大学JMRSL CERES获得,并通过阿拉斯加卫星设施网站收集。差分干涉合成孔径雷达(DInSAR)被认为是探测地面沉降最有效的技术之一。DInSAR方法用于绘制海拔变化,每年绘制地面沉降图。填图结果显示,西苏门答腊巴东地区地表沉降最大的区域分布为巴东乌塔拉、南加洛和巴东巴拉街道。巴东西拉丹和鹿buk Begalung街道地面沉降不明显。2009年9月30日巴东乌加拉、南加洛和西巴东街道地震后,利用DInSAR方法估算的巴东地区地面沉降分布在0 ~ 32.70 cm左右,地面沉降速度在0.13 ~ 12 cm/年左右。在巴东市易受洪水影响的地区,地面沉降的预期影响之一可能会增加。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Land subsidence estimation using DinSAR method ALOS PALSAR image in Padang City West Sumatra, Indonesia
Land subsidence is a phenomenon that occurs in big cities around the world and in Indonesia. Padang as one of the largest cities in West Sumatera also facing land subsidence due to natural phenomena and human induced. Padang City is located at the west coast of Sumatera Island which is the junction point of three active plates that cause frequent earthquakes. Main goals of this research are to know the distribution of area affected by land subsidence, to know the estimated value of land subsidence and to know the value of the velocity of land subsidence in Padang area using DInSAR method. The data used in this study is ALOS PALSAR Image Level 1.1 of Padang city during 2007 to 2010 was obtained through JMRSL CERES Chiba University, Japan and collected through Alaska Satellite Facility website. Differential Interferometric Synthetic Aperture Radar (DInSAR) is a technique considered to be one of the most efficient technique for detecting land subsidence. The DInSAR method is used in mapping altitude changes developed into a land-subsidence map each year. The mapping results show the distribution of the areas affected by the maximum land subsidence in Padang area of West Sumatera are Padang Utara, Nanggalo, and Padang Barat Subdistricts. The land subsidence insignificant occurred is Padang Selatan and Lubuk Begalung Subdistricts. The estimated value of the land subsidence distribution in Padang area using DInSAR method has decreased significantly after the earthquake of September 30, 2009 in Padang Utara, Nanggalo and West Padang Subdistricts is around 0 - 32.70 cm, and the value of land subsidence velocity is around 0.13 - 12 cm/year. One of the expected effects of land subsidence can be increased in the area susceptible for flooding in Padang city.
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