Example of the complete workflow Sample Clauses

Example of the complete workflow. The seismic array was composed by 17 stations (Figure 34). However, due to malfunctioning, only the data of 14 stations (grey circles in the Figure 34) could be used for the processing. The intra-station distances in the array ranged between 5.4 m to 115 meters. The first step of the analysis consists in a visual inspection of the recordings at all stations. In particular, in order to identify malfunctioning of one station or channel and to select signal windows suitable for the H/V analysis, the quality of the recording was evaluated (1) analysing the signal stationarity in the time domain (Figure 35a), (2) the relevant unfiltered Xxxxxxx spectra (Figure 35b), and (3) the H/V variation over time (Figure 35a). b) Figure 35 – a) H/V spectral ratio versus time and corresponding time histories for station 3032. b) Xxxxxxx spectra for each of selected window. at station 3032. Left) Vertical component spectra, centre) E-W component spectra, right) N-S component spectra. Figure 36 - Experimental space-correlation function values (circles) for different frequencies. The red circles indicate values discarded. The black lines depict the estimated space-correlation function values for the phase velocity showing the best fit to the data. The bottom panels show the relevant root-mean square errors (RMS) versus phase velocity tested. Figure 38 - Comparison of experimental phase velocity estimated by the ESAC method and by the f-k method (both for Beam Forming and Maximum Likelihood Method). The red circles represent the values used for the joint inversion. The intervals (Black lines) around the observed ESAC phase velocities are obtained by calculating the square root of the covariance of the error function. a) b) Figure 39 - a) average H/V for each station of the array (e.g. 06 stands for station 3006, 32 stands for station 3032, etc.) and b) the average H/V of the array. The red circles represent the values used in the inversion procedure. The inversion of dispersion and H/V curves to estimate the S-wave velocity profile was carried out fixing to 7 the number of layers overlying the half-space in the model (Table 5). Through a genetic algorithm a search over 80000 models was carried out and the agreement between the theoretical H/V and Rayleigh-wave dispersion curves with the observed ones was evaluated by means of a cost function (see above). The inversion was repeated several times starting from different seed numbers, i.e. from a different population of initial mo...
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Related to Example of the complete workflow

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