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Results suggest that the short-time Fourier transform is in general more reliable than the wavelet transform for the present purpose.
The advantage and priority of this method over numerical or exact analytical solution (i.e., Laplace transform) is in the cases which the heterogeneity and variation of reservoir properties such as porosity and permeability with position or pressure could not be neglected, in these situations, the numerical or exact analytical solution is very tedious and may be impossible.
The advantage and priority of the OC method over exact analytical solution (i.e., Laplace transform) is in the cases that the heterogeneity and variation of reservoir properties such as porosity and permeability with position or pressure could not be neglected; in these cases, the exact analytical solution is very tedious and may be impossible.
The only difference between the Morlet wavelet and Gabor transform is in the exponent term, which helps determine the shape of the wavelet.
The delay time τ for a structure obtained from solving the time-dependent Schrodinger equation using Laplace transform is in fact close to the approximate values in Equation 9.
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The general processes involved in calculating the watershed transform is shown in Figure 1.
The inverse RCM transform is defined as in(48) (48).
A novel threshold-based piecewise companding transform is proposed in this paper.
This transform is shown in Fig. 7.
Discrete Wavelet Transform [23]: Daubechies family of wavelet transform is used in this technique.
An averaged Morlet Wavelet transform is shown in Fig. 2B after dexmedetomidine administration.
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