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Matteo Albano1, Marco Polcari1, Christian Bignami1, Marco Moro1, Michele Saroli2,1, Salvatore Stramondo1 1 - Istituto Nazionale di Geofisica a Vulcanologia,

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Presentation on theme: "Matteo Albano1, Marco Polcari1, Christian Bignami1, Marco Moro1, Michele Saroli2,1, Salvatore Stramondo1 1 - Istituto Nazionale di Geofisica a Vulcanologia,"β€” Presentation transcript:

1 Matteo Albano1, Marco Polcari1, Christian Bignami1, Marco Moro1, Michele Saroli2,1, Salvatore Stramondo1 1 - Istituto Nazionale di Geofisica a Vulcanologia, Via di Vigna Murata 605, Roma (Italy) 2 - UniversitΓ  degli Studi di Cassino e del Lazio meridionale, Via G. di Biasio 43, Cassino (Italy) Monitoring the change of soil seismic response through the InSAR-derived ground subsidence: application to the Mexico City subsidence

2 Outline Introduction Method The case study Results and validation
Conclusions

3 Central Italy 2016 earthquakes
Introduction SAR as a ground displacement measurement technique EARTHQUAKES Central Italy 2016 earthquakes (INGV, 2016) Campi Flegrei (Trasatti et al., 2015) VOLCANOS Subsidence of Bologna (Stramondo et al., 2007) ANTHROPOGENIC PHENOMENA

4 Introduction Urban subsidence caused by groundwater withdrawal
Bologna (Stramondo et al., 2007) Morelia (Cigna et al., 2012) Guzman (Brunori et al., 2012) Thessaloniki (Svigkas et al., 2016) Effect on the dynamic behavior of soils

5 Introduction Effect on the dynamic behavior of soils: theory Soil Rock
Hs vs a t a t vs DHs Rock Soil Uniform, damped soil on a rigid rock Hs = soil thickness Vs = shear wave velocity a t Amplification factor Frequency (w) (Kramer, 1996) 2 4 6 8 10 12 5 15 20 𝐴= 1 π‘π‘œπ‘  2 πœ”π» 𝑣 𝑠 + [πœ‰ πœ”π» 𝑣 𝑠 ] 2 πœ” 𝑛 = 𝑣 𝑠 𝐻 𝑠 πœ‹ 2 +π‘›πœ‹ ; 𝑛=0, 1,…,∞ πœ” 0 = πœ‹ 𝑣 𝑠 2𝐻 𝑠 n = 0 𝑇 𝑠 = 2πœ‹ πœ” 0 = 4 𝐻 𝑠 𝑣 𝑠 Hs Ts

6 Introduction Effect on the dynamic behavior of soils: experimental evidence Mexico city (AvilΓ©s and PΓ©rez-Rocha, 2010; Arroyo et al., 2013) ALAMEDA PARK – CITY CENTER Fourier amplitude (m/s) Ts(s) Ts(s)

7 InSAR ground subsidence as a tool for local seismic hazard monitoring
Objective Urban subsidence from InSAR Ts(s) Change of the soil resonant period InSAR ground subsidence as a tool for local seismic hazard monitoring

8 InSAR displacements t0 οƒž tn
Method InSAR displacements t0 οƒž tn Soil resonant period Ts (tn) Soil thickness Hs (tn) (Gosar and Lenart, 2010) 𝐻 𝑠 =π‘Žβˆ™ 𝑇 𝑠 𝑏 𝐻 𝑠 =π‘Žβˆ™ 𝑇 𝑠 𝑏 Ts ??? Soil thickness (t0) 𝐻 𝑠 =π‘Žβˆ™ 𝑇 𝑠 𝑏

9 The case study MEXICO CITY Land area:1485 km2 8.84 million people
Density: 6000 people/km2

10 The case study Seismic hazard http://gmo.gfz-potsdam.de/ Urban area
Hard volcanic deposits Alluvial fans Clays and clayey silts Urban area The Global Seismic Hazard Map 2280 2260 2240 2220 2200 2180 2160 2140 Height a.s.l. (m) Hs  60m Santoyo et al., 2005

11 The case study Ground subsidence SAR data Leveling GPS data
Cabral-Cano et al., 2008 Leveling GPS data Cabral-Cano et al., 2008 Sowter et al., 2016 LΓ³pez-Quiroz et al., 2009 (Osmanoglu et al., 2011) Chaussard et al., 2014

12 The case study A-priori data Soil thickness (Hs)
NORMAS TECNICAS COMPLEMENTARIAS DEL REGLAMENTO DE CONSTRUCCIONES DEL DISTRITO FEDERAL (November 2004) Soil thickness (Hs) Soil resonant period (Ts) Design response spectrum (AvilΓ©s & PΓ©rez-Rocha, 2010)

13 Results and validation
SAR data and results ENVISAT RADARSAT-2 Constellation ENVISAT RADARSAT-2 Time interval November,2004 February,2006 April,2013 September,2013 Image nΒ° 13 10 Sensor C-band Mode Stripmap tilde IW-mode Resolution 100 m Orbit Descending Incidence angle 23Β° 35Β° SBAS (Berardino et al., 2002) IPTA (Werner et al., 2003)

14 Results and validation
Soil thickness (Hs) 2004 2013 Variation between

15 Results and validation
Soil resonant period (Ts) 2004 2013 Variation between

16 Design response spectrum
Results and validation Soil resonant period (Ts) Variation between Design response spectrum

17 Results and validation
27 accelerometric stations (Arroyo et al., 2013) RMSE = 0.2s AE02 BO39 PE10 CJ03

18 Conclusions We developed a procedure to evaluate the effect of ground subsidence on the spatial and temporal seismic response of soils by exploiting InSAR-derived ground displacements. The proposed procedure has been applied to estimate the resonant period change of the subsoil of Mexico City caused by the very fast subsidence which affects the city. The resonant period estimates have been validated with field measurements. The results can be improved by processing a complete SAR dataset from 2005 to 2017 The proposed procedure is suitable for the on-line implementation.


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