Numerical analysis of seismic wave amplification in Nice (France) and comparisons with experiments

TL;DR

This paper uses numerical Boundary Element Method analysis to study seismic wave amplification in Nice, France, comparing results with experiments, and highlights the influence of geological parameters and wave types on amplification levels.

Contribution

It introduces a boundary element model considering various wave types and soil properties, improving estimation of seismic amplification over traditional 1D analysis.

Findings

Numerical results closely match experimental data for real earthquakes.

2D basin effects significantly influence seismic amplification.

Soil properties and wave types critically affect amplification levels.

Abstract

The analysis of site effects is very important since the amplification of seismic motion in some specific areas can be very strong. In this paper, the site considered is located in the centre of Nice on the French Riviera. Site effects are investigated considering a numerical approach (Boundary Element Method) and are compared to experimental results (weak motion and microtremors). The investigation of seismic site effects through numerical approaches is interesting because it shows the dependency of the amplification level on such parameters as wave velocity in surface soil layers, velocity contrast with deep layers, seismic wave type, incidence and damping. In this specific area of Nice, a one-dimensional (1D) analytical analysis of amplification does not give a satisfactory estimation of the maximum reached levels. A boundary element model is then proposed considering different wave types (SH, P, SV) as the seismic loading. The alluvial basin is successively assumed as an isotropic linear elastic medium and an isotropic linear viscoelastic solid (standard solid). The thickness of the surface layer, its mechanical properties, its general shape as well as the seismic wave type involved have a great influence on the maximum amplification and the frequency for which it occurs. For real earthquakes, the numerical results are in very good agreement with experimental measurements for each motion component. Two-dimensional basin effects are found to be very strong and are well reproduced numerically.