Detection of Liquefaction Phenomena from the 2017 Pohang (Korea) Earthquake Using Remote Sensing Data

On 15 November 2017, liquefaction phenomena were observed around the epicenter after a 5.4 magnitude earthquake occurred in Pohang in southeast Korea. In this study, we attempted to detect areas of sudden water content increase by using SAR (synthetic aperture radar) and optical satellite images. We...

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Main Authors: Hyunseob Baik, Young-Sun Son, Kwang-Eun Kim
Format: Article
Language:English
Published: MDPI AG 2019-09-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/11/18/2184
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spelling doaj-424352de5f8e4791a557bd7931c6d5bc2020-11-24T20:53:44ZengMDPI AGRemote Sensing2072-42922019-09-011118218410.3390/rs11182184rs11182184Detection of Liquefaction Phenomena from the 2017 Pohang (Korea) Earthquake Using Remote Sensing DataHyunseob Baik0Young-Sun Son1Kwang-Eun Kim2Department of Geophysical Exploration, KIGAM campus, Korea University of Science and Technology (UST), Daejeon 34114, KoreaKorea Institute of Geoscience and Mineral Resources (KIGAM), Daejeon 34132, KoreaKorea Institute of Geoscience and Mineral Resources (KIGAM), Daejeon 34132, KoreaOn 15 November 2017, liquefaction phenomena were observed around the epicenter after a 5.4 magnitude earthquake occurred in Pohang in southeast Korea. In this study, we attempted to detect areas of sudden water content increase by using SAR (synthetic aperture radar) and optical satellite images. We analyzed coherence changes using Sentinel-1 SAR coseismic image pairs and analyzed NDWI (normalized difference water index) changes using Landsat 8 and Sentinel-2 optical satellite images from before and after the earthquake. Coherence analysis showed no liquefaction-induced surface changes. The NDWI time series analysis models using Landsat 8 and Sentinel-2 optical images confirmed liquefaction phenomena close to the epicenter but could not detect liquefaction phenomena far from the epicenter. We proposed and evaluated the TDLI (temporal difference liquefaction index), which uses only one SWIR (short-wave infrared) band at 2200 nm, which is sensitive to soil moisture content. The Sentinel-2 TDLI was most consistent with field observations where sand blow from liquefaction was confirmed. We found that Sentinel-2, with its relatively shorter revisit period compared to that of Landsat 8 (5 days vs. 16 days), was more effective for detecting traces of short-lived liquefaction phenomena on the surface. The Sentinel-2 TDLI could help facilitate rapid investigations and responses to liquefaction damage.https://www.mdpi.com/2072-4292/11/18/2184earthquakeliquefactiontime series analysissatellite imageoptical and SAR data
collection DOAJ
language English
format Article
sources DOAJ
author Hyunseob Baik
Young-Sun Son
Kwang-Eun Kim
spellingShingle Hyunseob Baik
Young-Sun Son
Kwang-Eun Kim
Detection of Liquefaction Phenomena from the 2017 Pohang (Korea) Earthquake Using Remote Sensing Data
Remote Sensing
earthquake
liquefaction
time series analysis
satellite image
optical and SAR data
author_facet Hyunseob Baik
Young-Sun Son
Kwang-Eun Kim
author_sort Hyunseob Baik
title Detection of Liquefaction Phenomena from the 2017 Pohang (Korea) Earthquake Using Remote Sensing Data
title_short Detection of Liquefaction Phenomena from the 2017 Pohang (Korea) Earthquake Using Remote Sensing Data
title_full Detection of Liquefaction Phenomena from the 2017 Pohang (Korea) Earthquake Using Remote Sensing Data
title_fullStr Detection of Liquefaction Phenomena from the 2017 Pohang (Korea) Earthquake Using Remote Sensing Data
title_full_unstemmed Detection of Liquefaction Phenomena from the 2017 Pohang (Korea) Earthquake Using Remote Sensing Data
title_sort detection of liquefaction phenomena from the 2017 pohang (korea) earthquake using remote sensing data
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2019-09-01
description On 15 November 2017, liquefaction phenomena were observed around the epicenter after a 5.4 magnitude earthquake occurred in Pohang in southeast Korea. In this study, we attempted to detect areas of sudden water content increase by using SAR (synthetic aperture radar) and optical satellite images. We analyzed coherence changes using Sentinel-1 SAR coseismic image pairs and analyzed NDWI (normalized difference water index) changes using Landsat 8 and Sentinel-2 optical satellite images from before and after the earthquake. Coherence analysis showed no liquefaction-induced surface changes. The NDWI time series analysis models using Landsat 8 and Sentinel-2 optical images confirmed liquefaction phenomena close to the epicenter but could not detect liquefaction phenomena far from the epicenter. We proposed and evaluated the TDLI (temporal difference liquefaction index), which uses only one SWIR (short-wave infrared) band at 2200 nm, which is sensitive to soil moisture content. The Sentinel-2 TDLI was most consistent with field observations where sand blow from liquefaction was confirmed. We found that Sentinel-2, with its relatively shorter revisit period compared to that of Landsat 8 (5 days vs. 16 days), was more effective for detecting traces of short-lived liquefaction phenomena on the surface. The Sentinel-2 TDLI could help facilitate rapid investigations and responses to liquefaction damage.
topic earthquake
liquefaction
time series analysis
satellite image
optical and SAR data
url https://www.mdpi.com/2072-4292/11/18/2184
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AT youngsunson detectionofliquefactionphenomenafromthe2017pohangkoreaearthquakeusingremotesensingdata
AT kwangeunkim detectionofliquefactionphenomenafromthe2017pohangkoreaearthquakeusingremotesensingdata
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