Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (3): 836-845.doi: 10.13278/j.cnki.jjuese.20160364

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Periodical Analysis of Land Subsidence in Beijing Plain Based on Morlet Wavelet Technology

Wang Jie1,2,3, Gong Huili1,2,3, Chen Beibei1,2,3, Gao Mingliang1,2,3, Zhou Chaofan1,2,3, Liang Yue1,2,3, Chen Wenfeng1,2,3   

  1. 1. Key Lab of 3D Information Acquisition and Application, Ministry of Education, Beijing 100048, China;
    2. State Key Laboratory Breeding Base of Process of Urban Environment and Digital Simulation, Beijing 100048, China;
    3. School of Resources Environment and Tourism, Capital Normal University, Beijing 100048, China
  • Received:2017-12-29 Online:2018-05-26 Published:2018-05-26
  • Supported by:
    Supported by National Natural Science Foundation of China (41130744, 41171335, 41401492), National Key Basic Research Program ("973" Program) of China (2012CB723403) and General Program of Science and Technology Development Project of Beijing Municipal Education Commission of China (KM201510028012)

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Abstract: Land subsidence in Beijing has been developing rapidly since it was discoverd in the 1960s. Uneven ground deformation can destory buildings, and urban infrastructures such as underground pipelines,threatening urban security. In order to analyze the characteristics and the evolution trend of land subsidence in Beijing plain, 27 scenes of Radarsat-2 data from 2011 to 2014 were collected, and the interference point target analysis (IPTA) technology was performed, to obtain the time series land subsidence information. On this basis, four land subsidence areas were selected representatively, and multi-scale evolution characteristics of land subsidence were analyzed through Morlet wavelet tranform respectively. The results show that the maximum subsidence rate is 162.70 mm/a while the average rate is 50.08 mm/a, and subsidence rates are quite different among these areas in spatial distribution. Moreover, the wavelet transforms analysis indicates that the land subsidence present obvious local periodic variation characteristics in the time domain. In particular, at the time scale of 28 T(1 T represents a perod of 24 d), there is a time period of about 13.3 months, with different unstable oscillation periods in different positions.

Key words: land subsidence, interference point target analysis (IPTA), Morlet wavelet, periodicity

CLC Number: 

  • P642.26
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