Abstract

The production of fragility functions describing the probable behaviour and damage on historical buildings is a key step in a method for the estimation of the magnitude of historical seismic events that uses a Bayes'. The fragilities are estimated by integrating the structural capacity with the seismic demand using either static methods, as the Capacity Spectrum Method (CSM), or dynamic methods, as Incremental Dynamic (IDA) and Multiple Stripes Analysis (MSA). Uncertainties in both resistance, demand, and distance and magnitude models propagate to the posterior magnitude distribution. The present paper studies the effect of uncertainties related both to the production of fragility functions and prior distributions, in the estimation of the magnitude of the 1763 Komárom earthquake (in historical Hungary). In the XVIII century most of the structures in the region were built of earth, adobe, clay or stone masonry, which is complex to model. While micro or detailed macro-modelling strategies are computationally costly, simplified macro-approaches are often more efficient, but require a pre-identification of the failure mode(s) and the determination of the backbone curve. For this study, a simplified macro-model of a Hungarian peasant house archetype is calibrated for CSM and IDA. The physical and geometrical uncertainties are incorporated in the fragilities using Monte-Carlo simulation. Prior magnitude and distance distributions are studied. The final magnitude estimates are presented and discussed.

Highlights

  • The most common methods for the estimation of the magnitude of historical seismic events [1, 2] belong to the domain of seismology, using interdisciplinary knowledge of both geophysicists and historians [3]

  • The present paper focusses on how fragility and ground motion prediction equation (GMPE) related uncertainties, and assumptions based on prior information, impact the final magnitude estimates, extending earlier works on the simplified assessment of the behaviour of historical unreinforced masonry walls and magnitudes for the 1763 Komárom earthquake

  • Despite the poor description of the im with Capacity Spectrum Method (CSM), the experimental capacity curves and the FEMA HAZUS manual led to similar fragility moments, the fragility medians rather than their standard deviations are relevant for the final magnitude estimates

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Summary

Introduction

The most common methods for the estimation of the magnitude of historical seismic events [1, 2] belong to the domain of seismology, using interdisciplinary knowledge of both geophysicists and historians [3] Another method applies the background of Probabilistic Seismic Hazard Analysis (PSHA) and uses historical seismic records of damage to translate the nonlinear structural damage into fragility curves [4], obtained either by dynamic methods as Incremental Dynamic and Multiples Stripes Analysis (IDA & MSA) [5] or by static methods as the Capacity Spectrum Method (CSM) [6].

Methodologies
The Magnitude estimation method
Static and dynamic based analysis and fragilities
Complex vs simplified modelling
IDA based fragilities
CSM based fragilities
FEMA HAZUS based fragilities
Magnitude estimates
Sensitivity study
Prior magnitude and distance distributions
Comparison of magnitude estimates
Findings
Discussion of the results
Conclusions
Full Text
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