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Monitoring the Subsidence Induced by Salt Mining in Tuzla, Bosnia and Herzegovina by SBAS-DInSAR Method

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Abstract

The ground subsidence induced by salt mining has been causing significant damage in Tuzla, Bosnia and Herzegovina since the 1950s. Several investigations and geodetic surveys have been conducted, i.e., traditional topographic surveys (1950–2003) and static GPS surveys (2004–2007). The last GPS survey (2006–2007) revealed that the subsidence in Tuzla was still occurring at a rate of about − 10 cm/year in some areas. Although monitoring of the subsidence has been on-going at a few points since 2010, by means of the real-time kinematic GNSS method, it lacks spatial coverage. Therefore, an appropriate method is required to monitor the subsidence over an extensive area at a low cost and with less labor time. Differential Interferometry Synthetic Aperture Radar (DInSAR), together with the Small Baseline Subset (SBAS) time-series algorithm, is one of the solutions for use as an effective monitoring tool. The spatial distribution of the subsidence obtained by SBAS-DInSAR shows a good agreement with the subsidence obtained from the former monitoring results. The temporal transition of the subsidence obtained by SBAS-DInSAR is evaluated using the results by the real-time kinematic GNSS monitoring system. It was shown that the DInSAR results coincide with the GNSS results with a discrepancy of less than 10 mm. SBAS-DInSAR detected that the subsidence had almost vanished everywhere, except the north and northeast portions of Pannonica Lake where the rate of subsidence was − 1 to − 4 cm/year during the period of October 2014–May 2019. This study demonstrates that SBAS-DInSAR can be employed as a useful and effective subsidence monitoring tool without the need to install any devices in the monitoring area.

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Fig. 1

modified from Mancini et al. 2009a), and c vertical X–X’ cross section (Ferhatbegović 2004)

Fig. 2

(modified from Mancini et al. 2009a)

Fig. 3

modified from Stecchi (2008) (salt deposit border, safety pillar, and mining region were added by the authors), and d map of GPS densification and reference points (re-drawn from Stecchi (2008) and Mancini et al. (2009a)

Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9

modified from Stecchi 2008), and c subsidence distribution obtained by traditional topographical surveys from 1956 to 2003 (re-drawn from Mancini et al. 2009b)

Fig. 10
Fig. 11
Fig. 12
Fig. 13

modified from Mancini et al. 2009b), b subsidence obtained by SBAS-DInSAR October 9, 2014 to May 28, 2019, c section A–A’, d section B–B’, e section C–C’, and f section D–D’

Fig. 14
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Abbreviations

AW3D30:

ALOS World 3D—30-m resolution digital elevation model

DEM:

Digital Elevation Model

DInSAR:

Differential Interferometry Synthetic Aperture Radar

GIS:

Geographic Information System

GNSS:

Global Navigation Satellite System

GPS:

Global Positioning System

InSAR:

Interferometry Synthetic Aperture Radar

JAXA:

Japan Aerospace Exploration Agency

LOS:

Line of Sight

SAR:

Synthetic Aperture Radar

SBAS:

Small Baseline Subset

\(\lambda\) :

Wavelength

\(\theta_{0}\) :

Off-nadir angle

\(\theta_{i}\) :

Incidence angle

\(\beta\) :

Angle of the satellite flight (orbit) direction

\(D_{{{\text{sub}}}}\) :

Subsidence

\(D_{{{\text{LOS}}}}\) :

Displacement along satellite’s line of sight (LOS)

\(D_{{{\text{N}} - {\text{S}}}}\) :

Displacement in North–South direction

\(D_{{{\text{E}} - {\text{W}}}}\) :

Displacement in East–West direction

\(D_{{{\text{U}} - {\text{P}}}}\) :

Displacement in Up–Down (vertical) direction

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Acknowledgements

This research was partially supported by JSPS KAKENHI (Grant-in-Aid for Scientific Research, Japan Society for the Promotion of Science) Grant no. 16H03153 and the International Collaborative Research Fund of Yamaguchi University. The SAR data were provided by the European Space Agency (ESA) and are distributed for free through the Copernicus program. The digital elevation model (DEM) and ALOS Global Digital Surface Model "ALOS World 3D-30m (AW3D30)” were provided by the Japan Aerospace Exploration Agency (JAXA). The authors wish to express their appreciation to those agencies. They also extend their appreciation to Tuzla City Municipality for their encouragement, Professor Z. Ferhatbegović for his suggestions regarding the description of geological features in Tuzla, and H. Griswold for proofreading the manuscript.

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Parwata, I.N.S., Shimizu, N., Grujić, B. et al. Monitoring the Subsidence Induced by Salt Mining in Tuzla, Bosnia and Herzegovina by SBAS-DInSAR Method. Rock Mech Rock Eng 53, 5155–5175 (2020). https://doi.org/10.1007/s00603-020-02212-1

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