差分干涉法合成孔径雷达(DInSAR)在雅加达DKI地区的沉降分析

Cyntia Cyntia, I. Pudja
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引用次数: 5

摘要

雅加达DKI的地面沉降受到几个关键因素的影响,包括增加地表以上荷载的建筑物数量。仍然有许多人探索地下水资源作为清洁水的主要来源。此外,土壤类型以冲积土为主。该冲积层可能是地表地面沉降和隆起形式的土壤变形的参数之一,因为基本上,冲积土类型对上述荷载支撑力具有敏感性。因此,DKI雅加达的地面沉降是相对连续的。为了查明地面沉降情况,采用了一种高科技方法,2017年差分干涉合成孔径雷达(DInSAR)卫星图像雷达数据(SAR Sentinel-1A)。结果表明,DKI雅加达地区的地面沉降平均值约为-3.685厘米/年,最高沉降发生在雅加达西区,平均约为-5.850厘米/年。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Subsidence analysis in DKI Jakarta using Differential Interferometry Synthetic Aperture Radar (DInSAR) Method
Land subsidence in DKI Jakarta influenced by several key factors, including the number of buildings that increase the load above the surface. There are still many people who explore groundwater sources as the principal source of clean water. Also,  the soil type is dominated by alluvial. This alluvial deposit can be one of the parameters for soil deformation in the form of land subsidence and uplift in land surface because basically, alluvial soil types have a susceptibility to the load support power above. So that the land subsidence in DKI Jakarta is relatively continuous. To find out the land subsidence is used a high-tech method,  Differential Interferometry Synthetic Aperture Radar (DInSAR) satellite image of radar data (SAR Sentinel-1A) in 2017. The result shows the land subsidence in the average value of DKI Jakarta which is about -3.685 cm/year and the highest subsidence happened in the West Jakarta district about -5.850 cm/year in average.
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