Abstract

The long-term spatial-temporal deformation monitoring of densely distributed infrastructures near the lake area is of great significance to understand the urban health status and prevent the potential traffic safety problems. In this paper, the permanent scatterer interferometry (PSI) technology with TerraSAR-X imagery over the area around Dongting Lake was utilized to generate the long-term spatial-temporal deformation. Since the X-band SAR interferometric phases are highly influenced by the thermal dilation of the observed objects, and the deformation of large infrastructures are highly related to external temperature, a combined deformation model considering the thermal expansion and the seasonal environmental factors was proposed to model the temporal variations of the deformation. The time series deformation and the thermal dilation parameter over the area were obtained, and a comparative study with the traditional linear model was conducted. The Dongting Lake Bridge and the typical feature points distributed around the lake were analyzed in details. In order to compensate for the unavailability of external in situ measurements over the area, phase residuals and the subsidence generated through Differential Interferometric Synthetic Aperture Radar (D-InSAR) were utilized to verify the accuracy of the obtained deformation time series. Experiment results suggested that the proposed model is suitable and suggested for the selected study site. The root mean square error (RMSE) of the residual phase was estimated as 0.32 rad, and the RMSE compared with D-InSAR derived deformation was ±1.1 mm.

Highlights

  • Dongting Lake is located at the South Bank of Yangtze River in the north of Hunan Province, China, which is a tectonic lake with the characteristics of barrier lake

  • From the temporal evolution shown by the time series deformation maps generated by the seasonal model (TESM), it can be seen that the results show a periodic temporal evolution

  • Along-term deformation investigation over the area with densely distributed infrastructures around Dongting Lake was presented based on permanent scatterer interferometry (PSI) technology using 24 TerraSARX images from December 2011 to April 2013

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Summary

Introduction

Dongting Lake is located at the South Bank of Yangtze River in the north of Hunan Province, China, which is a tectonic lake with the characteristics of barrier lake. Yueyang is a lakeside city of Hunan Province next to Dongting Lake, which is under the combined geological structure characteristics of intermittent uplift denudation and intermittent stable uplift deposition (i.e., uplift and stable alternating) [1]. As a city with a population of 5.8 million, plenty of residential areas and developed transportation network are distributed in Yueyang. The residential areas around Dongting Lake are under high potential danger of accumulated deformation, collapse of ground surface, or even landslides of the slope, which greatly endangers the safety of the area. The longterm spatial-temporal deformation monitoring over this area is of great significance to understand its health status and prevent the potential traffic safety problems

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