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利用干涉合成孔径雷达和带通滤波检测快速沉降大都市中民用建筑的地面差异位移。

Detecting differential ground displacements of civil structures in fast-subsiding metropolises with interferometric SAR and band-pass filtering.

作者信息

Solano-Rojas Darío, Wdowinski Shimon, Cabral-Cano Enrique, Osmanoğlu Batuhan

机构信息

Marine Geology and Geophysics, School of Marine and Atmospheric Science, University of Miami, 4600 Rickenbacker Causeway, Miami, FL, 33149-1098, USA.

Department of Earth and Environment, Institute of Environment, Florida International University, Miami, FL, 33199, USA.

出版信息

Sci Rep. 2020 Sep 22;10(1):15460. doi: 10.1038/s41598-020-72293-z.

DOI:10.1038/s41598-020-72293-z
PMID:32963307
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7508836/
Abstract

Ground displacements due to changes in soil conditions represent a threat to the stability of civil structures in many urban areas, worldwide. In fast-subsiding areas, regional subsidence (wavelength ~ 1,000's m) can be dominantly high and, consequently, mask other signals at local scales (wavelength ~ 10-100's m). Still, engineering and construction applications require a comprehensive knowledge of local-scale signals, which can threaten the stability of buildings and infrastructure. Here we present a new technique based on band-pass filters for uncovering local-scale signals hidden by regional subsidence as detected by interferometric SAR measurements. We apply our technique to a velocity field calculated from 21 high-resolution COSMO-SkyMed scenes acquired over Mexico City and obtain components of long (> 478 m), intermediate (42-478 m) and short (< 42 m) spatial wavelengths. Our results reveal that long-wavelength velocities exceed - 400 mm/year, whereas intermediate- and short-wavelength velocities are in the order of ± 15 mm/year. We show that intermediate-wavelength velocities are useful for retrieving signals such as uplift along elevated viaducts of Metro lines 4 and B, as well as differential displacements in Pantitlán station's pedestrian overpass system and across sharp geotechnical boundaries in the piedmont of Sierra de Santa Catarina-where surface faulting occurs.

摘要

在全球许多城市地区,土壤条件变化引起的地面位移对土木结构的稳定性构成威胁。在快速沉降地区,区域沉降(波长约为1000米)可能占主导地位,从而掩盖了局部尺度(波长约为10 - 100米)的其他信号。尽管如此,工程和建筑应用仍需要全面了解局部尺度信号,这些信号可能威胁建筑物和基础设施的稳定性。在此,我们提出一种基于带通滤波器的新技术,用于揭示干涉合成孔径雷达(InSAR)测量所检测到的被区域沉降掩盖的局部尺度信号。我们将该技术应用于根据在墨西哥城获取的21个高分辨率COSMO - SkyMed场景计算出的速度场,得到了长(> 478米)、中(42 - 478米)和短(< 42米)空间波长的分量。我们的结果表明,长波长速度超过 - 400毫米/年,而中波长和短波长速度约为±15毫米/年。我们表明,中波长速度有助于检索诸如沿着地铁4号线和B号线高架桥的隆起信号,以及潘蒂特兰车站人行天桥系统中的差异位移信号,还有圣卡塔琳娜山脉山麓发生地表断层处跨越尖锐岩土边界的信号。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/fef8defcdb92/41598_2020_72293_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/a1d82ad49402/41598_2020_72293_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/da7f42f17c65/41598_2020_72293_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/3c38f4628e8f/41598_2020_72293_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/5aba2df6e394/41598_2020_72293_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/d42d6cb001b2/41598_2020_72293_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/46cce4b47c31/41598_2020_72293_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/fef8defcdb92/41598_2020_72293_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/a1d82ad49402/41598_2020_72293_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/da7f42f17c65/41598_2020_72293_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/3c38f4628e8f/41598_2020_72293_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/5aba2df6e394/41598_2020_72293_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/d42d6cb001b2/41598_2020_72293_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/46cce4b47c31/41598_2020_72293_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7078/7508836/fef8defcdb92/41598_2020_72293_Fig7_HTML.jpg

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