Korean Journal of Remote Sensing (대한원격탐사학회지)

Korean Society of Remote Sensing (대한원격탐사학회)
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Ground Subsidence Measurements of Noksan National Industrial Complex using C-band Multi-temporal SAR images

C-밴드 다중시기 SAR 위성 영상을 이용한 녹산국가산업단지 일대의 지반침하 관측

  • Cho, Minji (National Institute of Meteorological Research, Korea Meteorological Administration) ;
  • Lee, Chang-Wook (National Institute of Meteorological Research, Korea Meteorological Administration)
  • 조민지 (기상청 국립기상연구소) ;
  • 이창욱 (기상청 국립기상연구소)
  • Received : 2014.04.03
  • Accepted : 2014.04.17
  • Published : 2014.04.30
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Abstract

Established in the lower reaches of the Nakdong river in Busan, the Noksan national industrial complex is one of the deepest soft ground areas in Korea. In case of the costal landfill having deep soft ground, there is a significant residual settlement over a long period of time. In this study, there was observed ground subsidence occurred in the Noksan national industrial complex from September 2002 to April 2007 by applying DInSAR and SBAS time series method using RADARSAT-1 and Envisat SAR datasets. As a result, it was calculated that ground subsidence developed at the velocity of about maximum 10 cm/yr and mean 6 cm/yr at the eastern center, west, western center and southern area contiguous on the coastline of the study area during the period from September 2002 to April 2007. In addition, the RADARSAT-1 average displacement map has been compared with the total displacement map observed by accurate magnetic probe extensometer during the period from 2001 to 2002. Since the time series displacement has shown a linear trend mostly, we consider that continuous monitoring should be needed until the ground subsidence of the study area has been stabilized.

녹산국가산업단지가 설립된 부산 낙동강 하류는 국내에서 연약지반이 가장 깊이 분포하고 있는 지역 중에 하나이다. 연약지반의 깊이가 깊은 해안 매립지의 경우, 장기간에 걸쳐 상당히 큰 잔류침하가 발생하게 된다. 본 연구는 RADARSAT-1과 Envisat의 다중시기 SAR 영상을 이용한 차분간섭기법과 SBAS 시계열 기법을 통해, 녹산산업국가단지에서 2002년 9월부터 2007년 4월 동안에 발생된 지반침하를 관측하였다. 그 결과 연구지역의 동쪽 중앙, 서쪽 중앙, 서쪽, 해안가와 닿아있는 남단에서 최대 10 cm/yr, 평균 6 cm/yr의 속도로 지반침하가 발생되고 있음을 확인하였다. 또한 RADARSAT-1 SAR 영상을 이용한 평균지표변위도는 2001년부터 2002년까지 침하계로 관측된 현장관측자료와 비교 분석되었다. 시간에 따른 지표변위 양상이 거의 선형에 가깝게 나타나므로, 연구지역의 지반침하가 안정권에 접어들 때까지 지속적인 모니터링이 필요할 것으로 사료된다.

Keywords

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