A Preliminary Model of Site Amplification for use in Ground-Motion Modeling in Southern Ontario
Abstract ID#: 33247
The key to the site characterization is the relationship between fpeak and drift thickness (depth to bedrock), which we derive using H/V data from earthquakes in the region, combined with a detailed digital drift thickness map available online from the Ontario Geological Survey (OGS). The OGS map also provides information on soil type, which is correlated with peak amplitudes (Apeak) of response. H/V spectral shapes may be associated with four main soil categories, which in decreasing order of stiffness are: bedrock, till, sand/clay, and organic soil/fill. The value of Apeak increases as stiffness decreases. We model site response by defining a generic site amplification curve, which is dependent only on fpeak and soil category. The generic curve enables an estimate of site amplification to be made over the entire frequency band from 0.1 to 20 Hz, knowing just the site depth and type. These site amplification curves can be applied in the development of regional GMPEs, and in the construction of robust near-real-time IGMs.
