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Ground Motion in Mexico City During M 7.1 Earthquake of September 19, 2017 Praveen K. Malhotra September 24, 2017

Praveen K. Malhotra - peer.berkeley.edu · Praveen K. Malhotra September 24, 2017. 2of 14 Ground Accelerations at UNAM Stationin Mexico City (116 km from Epicenter) 3of 14 Resultant

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Ground Motion in Mexico City DuringM 7.1 Earthquake of September 19, 2017

Praveen K. MalhotraSeptember 24, 2017

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Ground Accelerations at UNAM Station in Mexico City (116 km from Epicenter)

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Resultant Horizontal Ground Accelerations at UNAM Station in Mexico City

PGA = 0.0553 g

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Ground Velocities at UNAM Station in Mexico City (116 km from Epicenter)

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Resultant Horizontal Ground Velocities at UNAM Station in Mexico City

PGV = 4.17 in/s

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Ground Displacements at UNAM Station in Mexico City (116 km from Epicenter)

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Resultant Horizontal Ground Displacements at UNAM Station in Mexico City

PGD = 2.17 in

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Central-Period & Normalized-Velocity

• Central-period,

Tc = 2π (PGD/PGA)0.5 = 2 s

Hence, low-frequency ground motion

• Normalized-velocity,

PGVn = PGV/(PGD·PGA)0.5 = 0.61

Hence, medium-band ground motion

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Tripartite Plot of 5% Damping Response Spectrum at UNAM Station in Mexico City

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Acceleration-Deformation Plot of 5% Damping Response Spectrum

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Envelope Response Spectra for Various Values of Damping

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Deformation Demands on Structures of Various Lateral Strength and Damping

Lateral Strength

(% of Weight)

Deformation Demand (in)

5% 10% 20% 30%

18% 0.5

15% 3.6

10% 4 2.4

8% 4 2.7 0.2

6% 4 2.7 1.7 0.1

4% 4 2.7 1.7 1.2

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Observations and Comments

• Ground motion at UNAM station in Mexico City was low-frequency and medium-band

• Deformation demands were low on even weak structures

• Cyclic-demands were modest

• Such ground motions are not expected to collapse ‘engineered’ structures in seismically active regions

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Acknowledgments

• Data may be downloaded from the Center for Engineering Strong Motion Data: http://www.strongmotioncenter.org/

• Data processing, observations and comments are preliminary

• No warranty of any kind is assumed