The signals simulated for the three arrays A, B and C are analysed using the spatial auto-correlation method described in section 5.2. The azimuths and the distances between all couples of stations are shown in figure 6.15. The pairs of grey circles are the selected rings for the spatial auto-correlation computation. Distances are summarized in table 6.4.
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As in the f-k method (section 6.1.3), the choice of the window length for calculating the auto-correlations is crucial. An example of its influence is presented hereafter. The average auto-correlation ratios are calculated with equation 1.11 for pairs of stations separated by distances between 30 and 40 m. In figure 6.14, the auto-correlation curves are plotted for various window lengths, counted in number of cycles of the central considered frequency (
): 10, 25 and 50 (from light to dark grey, respectively). For the three curves, the average values are close to the true auto-correlation curve (black thick line) in the range 3.5 to 5.5 Hz. Below 3.5 Hz, the 10 cycle auto-correlation curve deviates from the correct function, while the two other curves (25 and 50 cycles) are close to it for frequency as low as 2.5 Hz. This discrepancy for short windows is probably due to a lack of source azimuth coverage (Asten et al. (2004)), as the number of acting random sources is inversely proportional to the considered duration. Another explanation might be that the spectral estimates are more influenced by unavoidable side effects generated by cutting signals into time windows. Also, long time window curves are smoother than short ones and exhibit smaller standard deviations (figure 6.14). During this thesis, the 25 cycle time windows are kept for the computation of auto-correlation curves.
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A total of 15 auto-correlation ratio curves (five by array) are calculated for time windows of 25 cycles. Only one curve per array is shown in figure 6.16 with grey dots and grey errors bars. The consistency of all 15 auto-correlation curves is checked on dispersion curves in figure 6.17(a) to 6.17(c), for arrays A to C, respectively.
The fifteen auto-correlation curves with the selected samples are inverted with five independent runs keeping the same parameterization as for the two preceding methods. The results are shown in figure 6.18. Only three auto-correlation curves among the fifteen are shown in figure 6.18(d) to 6.18(f). A good agreement is found between the calculated curves and the observed auto-correlations (black dots and their error bars) even below 2 Hz. The theoretical dispersion curve is drawn for comparison in figure 6.18(c). The auto-correlation method correctly retrieves the dispersion curve for all frequencies above 2.5 Hz. For lower frequency, a systematic bias is observed in figure 6.18(c). Comparing figures 6.11(b) and 6.13(b), the inversion of auto-correlation offers a little more constraint on Vs at the base of the sediment layer.
over the whole column and
below the major impedance contrast is not resolved as for the other methods.
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