Application of 3D Ambient Noise Tomography for Void Detection
Geotechnical Special Publication, ISSN: 0895-0563, Vol: 2024-February, Issue: GSP 348, Page: 603-613
2024
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Example: if you select the 1-year option for an article published in 2019 and a metric category shows 90%, that means that the article or review is performing better than 90% of the other articles/reviews published in that journal in 2019. If you select the 3-year option for the same article published in 2019 and the metric category shows 90%, that means that the article or review is performing better than 90% of the other articles/reviews published in that journal in 2019, 2018 and 2017.
Citation Benchmarking is provided by Scopus and SciVal and is different from the metrics context provided by PlumX Metrics.
Conference Paper Description
A first-time application of 3D ambient noise tomography (3D ANT) method is presented for detection of deep voids. The method is based on the solution of 3D P-SV elastic wave equations and adjoint-state optimization to directly invert experimental cross-correlation functions (CCF) for extraction of S-wave velocity (Vs) structure. The main advantage of this approach is that it does not rely on assumptions of energy balance and far-field waves as required by methods using characteristics of Green’s function (GF). Instead, the source power-spectrum density is inverted to account for source distribution (location and energy), which allows to exploit full information content of all available CCFs from ambient noise recordings. The 3D ANT capability in detecting deep voids is investigated at a test site in southern Florida. For the field experiment, 72 vertical geophones of 4.5-Hz resonance were deployed in a 4 × 18 grid over 9.0 × 76.5 m area on the ground surface to record noise data for 34 min. The CCFs extracted from the noise recordings have good energy at 5–20 Hz and a consistent wave propagation pattern for the entire test area. The inverted result reveals that the 3D ANT was able to image a large deep void at 28-to 44-m depth, which is generally consistent with results from invasive SPTs.
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