WO2010075412A2 - Automatic dispersion extraction of multiple time overlapped acoustic signals - Google Patents
Automatic dispersion extraction of multiple time overlapped acoustic signals Download PDFInfo
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- WO2010075412A2 WO2010075412A2 PCT/US2009/069242 US2009069242W WO2010075412A2 WO 2010075412 A2 WO2010075412 A2 WO 2010075412A2 US 2009069242 W US2009069242 W US 2009069242W WO 2010075412 A2 WO2010075412 A2 WO 2010075412A2
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- slowness
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- dispersion
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- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/40—Seismology; Seismic or acoustic prospecting or detecting specially adapted for well-logging
- G01V1/44—Seismology; Seismic or acoustic prospecting or detecting specially adapted for well-logging using generators and receivers in the same well
- G01V1/48—Processing data
- G01V1/50—Analysing data
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- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/28—Processing seismic data, e.g. for interpretation or for event detection
- G01V1/30—Analysis
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/28—Processing seismic data, e.g. for interpretation or for event detection
- G01V1/30—Analysis
- G01V1/307—Analysis for determining seismic attributes, e.g. amplitude, instantaneous phase or frequency, reflection strength or polarity
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V2210/00—Details of seismic processing or analysis
Definitions
- This invention relates broadly to the extraction of the slowness dispersion characteristics of multiple possibly interfering signals in broadband acoustic waves, and more particularly to the processing of acoustic waveforms where there is dispersion, i.e. a dependence of wave speed and attenuation with frequency.
- Dispersive processing of borehole acoustic data has been a key ingredient for the characterization and estimation of rock properties using borehole acoustic modes.
- the most common parameters describing the dispersion characteristics are the wavenumber, k(f), and the attenuation, A(f), both functions of the frequency/ and are of great interest in characterization of rock and fluid properties around the borehole.
- they are of interest in a variety of other applications such as non-destructive evaluation of materials using ultrasonic waves or for handling ground roll in surface seismic applications, where the received data exhibits dispersion that needs to be estimated.
- the dispersion characteristic consisting of the phase and group slowness (reciprocal of velocity) are linked to the wavenumber k as follows:
- One class of extraction methods uses physical models relating the rock properties around the borehole to the predicted dispersion curves. Waveform data collected by an array of sensors is back propagated according to each of these modeled dispersion curves and the model is adjusted until there is good semblance (defined below) among these back propagated waveforms indicating a good fit of the model to the data.
- An example is the commercial DSTC algorithm used for extracting rock shear velocity from the dipole flexural mode (see C. Kimball, "Shear slowness measurement by dispersive processing of borehole flexural mode," Geophysics, vol. 63, no. 2, pp. 337-344, March 1998) (in this case we directly invert for the rock property of interest).
- the algorithm advantageously involves the solution of a convex optimization problem that is computationally efficient to implement.
- Another advantage of this approach is that the model order selection is automatically taken care of as the sparsity conditions ensure that only the candidate modes are extracted as long as the regularization parameter for the penalty is chosen in an appropriate range.
- Figure 1 is a schematic representation of a physical set-up for acquisition of waves in a borehole.
- Figure 2 illustrates the array waveforms and modal dispersion curves governing the propagation of the acoustic energy.
- Figure 3 is a schematic representation of the piecewise linear approximation to the dispersion curve. Also shown are the dispersion parameters corresponding to a first order Taylor series approximation in a band around /D.
- Figure 4 illustrates the efficacy of local Taylor expansions of orders one and two in capturing the behavior of a typical quadrupole dispersion curve.
- Figure 5 illustrates a collection of broadband basis in a given band around the center frequency /0.
- Figure 6 is a schematic representation of the column sparsity of the signal support in ⁇ . Sparsity of the number of modes in the band (a) implies a column sparsity in mode representation in the broadband basis in the band (b).
- Figure 7 illustrates noisy data in a band containing two time overlapping modes.
- Figure 8 illustrates an example of the behavior of the residual as a function of ⁇ . Note how the mode leakage occurs into the residual as we increase ⁇ .
- the KS test is used to detect changes in the distribution of the residuals as a function of ⁇ .
- Figure 9 illustrates an example of the KS test statistic sequence and the p-value sequence for determining the operating ⁇ .
- Figure 10 is a schematic representation of the discretization of the parameter space of phase and group slowness in a band and the mismatch of the dictionary with respect to the true modes in the data.
- Figure 11 illustrates an example of the mode clusters in the phase and group slowness domain due to dictionary mismatch corresponding to the 6 largest peaks in the modulus image.
- Figure 12 illustrates the flow of processing in a band for dispersion extraction in the f-k domain.
- Figure 13 is a schematic representation of the first order Taylor series approximation to the dispersion curve in a band around the center frequency fa of the mother wavelet at scale a.
- Figure 14 illustrates a combination of the space-time and frequency- wavenumber processing for dispersion extraction using CWT (depicting the (a) f-k domain and (b) time domain characteristics of the CWT coefficients in terms of the propagation parameters at a given scale).
- Figure 15 illustrates an example of implication of time compactness of the CWT coefficients at a given scale at one sensor on the phase of the FFT coefficients in the band.
- Figure 16 illustrates an example of mode consolidation and model order selection using the phase slowness and time location estimates.
- Figure 17 illustrates the broadband space time propagators in the CWT domain.
- Figure 18 illustrates the reconstructed CWT coefficients at a given scale for two mode dispersion extraction problem with significant time overlap.
- Figure 19 illustrates the flow of the processing in the space time domain processing the output of the broadband processing in the f-k domain as applied to the CWT coefficients at a given scale.
- Figure 20 illustrates an array waveform data with two time overlapping modes.
- Figure 21 illustrates extracted dispersion curves in frequency bands. The solid lines denote the true underlying dispersion curves for the two modes. The extracted curves are shown by solid lines marked with circles.
- Embodiments of the invention may be implemented, at least in part, either manually or automatically. Manual or automatic implementations may be executed, or at least assisted, through the use of machines, hardware, software, firmware, middleware, microcode, hardware description languages, or any combination thereof. When implemented in software, firmware, middleware or microcode, the program code or code segments to perform the necessary tasks may be stored in a machine readable medium. A processor(s) may perform the necessary tasks.
- an acoustic source (100) which may be in communication with surface equipment is fired in a fluid filled borehole and the resulting waves that are generated in the borehole are recorded at a linear array of sonic sensors (hydrophones) (102) located on the acoustic tool.
- the data is acquired in the presence of noise (environmental noise and sensor noise) and interference (unmodelled energy), collectively denoted by w ⁇ l,t).
- the noisy observations at the set of sensors can be expressed as,
- the data at each frequency is a superposition of M exponentials sampled with respect to the sensor locations z b ..,z L .
- the above system of equations corresponds to a sum of exponential model at each frequency.
- M(J) is the effective number of exponentials at frequency/.
- a corresponding method step (1200) is shown in figure 12.
- Figure 4 illustrates the results of approximating a typical dispersion curve (quadrupole) with first and second order Taylor expansions (shown by the green (400) and red (402) curves, respectively). The local fit obtained thereby is quite adequate for capturing the local behavior of the dispersion curve.
- Those skilled in the art will note the efficacy of local Taylor expansions of orders one and two in capturing the behavior of a typical quadrupole dispersion curve.
- the local linear and quadratic approximations shown in red and blue respectively overlay and match the true dispersion curve well in a local interval.
- the dispersion curve is parameterized by the phase and the group slowness.
- a corresponding step (1202) is shown in figure 12. For attenuation it is assumed that it is constant over the frequency band of interest, i.e.,
- Figure 3 is a schematic depiction of the local linear approximation to a dispersion curve over adjacent frequency bands.
- M(J) M for all frequencies in the band of interest
- the sampled exponential at a frequency /corresponding to a mode can be expressed in a parametric form as
- the discrete set of frequencies in F correspond to the discrete set of frequencies in the DFT of the data y(l,t) of equation 3.
- a broadband system of equations in the band can be expressed as,
- the matrix P F (m) corresponds to the matrix of exponentials for the wavenumber response for mode m in the band F
- the vector S F (m) is the vector of the mode spectrum for mode m in the band F.
- the signal (without noise) in band F is a superposition of M modes and can be written as,
- a framework for dispersion extraction in f-k domain in a band can be understood by first considering a broadband basis element (also called a broadband propagator) in a band F corresponding to a given phase slowness and group slowness
- the broadband signal is in the span of the broadband basis elements from the over-complete dictionary
- the presence of a few significant modes in the band implies that the signal representation in the over-complete dictionary is sparse.
- the signal is composed of a superposition of few broadband propagators in the over-complete dictionary.
- the problem of dispersion estimation is mapped to that of finding the sparsest signal representation in an over-complete dictionary of broadband propagators spanning a range of group and phase slowness.
- the true propagators might not lie in the chosen over complete basis, this approach will still work so long as there are dictionary elements close to the true ones.
- the nearest basis elements are chosen in the sparse representation, possibly more than one for each mode, and the mismatch is subsumed in the noise.
- Figure 5 illustrates an over-complete basis of broadband propagators in the given band in the f-k domain. Considering now the signal of equation 12 and assuming that the M broadband propagators are contained in the over complete dictionary ⁇ , the problem set-up in the over-complete basis can be represented in terms of the latter
- M « N XM exhibits column sparsity as shown in figure 6.
- the column support of X is represented by 1/, the column indicator function of X, consisting of l's at the locations of the columns containing non-zero entries and O's elsewhere.
- X M has the smallest column support which corresponds to that of the true modes, i.e., the signal support.
- the signal support corresponds to the slowness dispersion parameters of the modes present in the data and its cardinality is the model order in the band.
- the sparsity structure of the signal support in the broadband basis described above is also known as a simultaneous sparse structure in the literature e.g., see J. A. Tropp, A. C. Gilbert, and M. J. Strauss (J. A.
- tests are used between the distribution of residuals to select the regularization parameter ⁇ in the optimization problem O.P TTh 1 ere are essentially two roles played by the x l 2 penalty in this context.
- the first role is that of general regularization of the solution where due to ill- conditioning of the matrix ⁇ the noise can get amplified.
- the second role is that of model order selection, which is essentially related to selection of the sparsest (and correct) basis for signal representation. In the context of finding sparse solutions these two aspects go hand in hand. Note, for example, that at a very low value of ⁇ , the solution to OP ⁇ i comes close to the Least Squares (LS) solution.
- LS Least Squares
- KS test statistic D The properties of the KS test statistic D, its limiting distribution and the asymptotic properties can be found in (W. Feller, "On the Kolmogorov-Smirnov limit theorems for empirical distributions," Annals of Mathematical Statistics, vol. 19, p. 177, 1948.). Essentially the KS statistic is a measure of similarity between two distributions. In order to apply the KS-test the steps shown in TABLE A are performed.
- X l> starts hitting the right signal subspace in the over-determined basis the rate of change of distribution of the residual as implied by the change in the test statistic, is more rapid due to mode leakage into the residual.
- the solutions for this range of ⁇ exhibit stability in terms of getting to the right signal support.
- the KS tests can be performed between residuals either in the frequency domain or in the time domain. If the modes are time compact, as is often the case, it is useful to compare the distributions of the residuals in the space-time domain.
- An example of the KS test-curves for distribution of residuals in time domain and the corresponding operating range of ⁇ is shown in figure 9.
- Equation 12 and let be the best and unique I 2 approximation to S F in the constructed over-complete dictionary ⁇ . Then let denote the coefficient vector that synthesizes the signal: Consequently, given ⁇ > 0, there exists an N e and a quantization of the slowness parameter domain (phase and group slowness) such that
- the signal can be well represented in the over- complete basis. This mismatch can then be modeled as an additive error,
- the mode clusters can also be formed if there is a high level of coherence between the broadband basis elements.
- An example of such clustering around the true values of phase and group slowness is shown in figure 11.
- the broadband dispersion extraction method in the f-k domain is combined with the EPRT type broadband dispersion extraction in the space-time domain.
- the CWT of the array data is used in order to retain the time information in this context. Initially, the dispersion parameters in the CWT domain are identified.
- G(J) is the Fourier transform of the analyzing (mother) wavelet g(t) and S(J) is the Fourier transform of the signal being analyzed.
- the analyzing mother wavelet g(t) is chosen to satisfy some admissibility condition. For the sake of exposition first consider a single mode. Then under the complex exponential model of equation 5 (and ignoring attenuation), the CWT coefficients at scale a and time shift b of the received waveform at sensor / is given by,
- Time compactness of mode m implies time compactness of the CWT coefficients Cr ⁇ a,b) at each scale.
- the time-frequency support of the modes in the CWT domain obeys the time-frequency uncertainty relation corresponding to the mother wavelet used - at higher frequencies (smaller scales) the time resolution is sharp but the frequency resolution is poor and vice-versa.
- Time compactness in turn implies a linear phase relationship across frequencies in the coefficients of the mode spectrum of the CWT data at any sensor / and where CJ is the effective bandwidth of the analyzing wavelet at scale a.
- Equations 30 and 31 indicate that the same exponential relationship holds for the CWT coefficients at each scale a in the frequency domain as for the original signal with the frequency band now given by the support at that scale of the analyzing wavelet.
- Y ,(a,f) denotes the Fourier transform at frequency /of the CWT coeffients at scale a of the waveform received at sensor /
- Y a (f) is the corresponding vector consisting of Y ,(a,f) for all sensors, then we see that Y a (f) can be represented in terms of a sum of exponential broadband propagators model very similar to equations 10 and 12.
- a joint method for dispersion extraction in the CWT domain that utilizes the broadband multiple mode extraction methodology in the f-k domain and the time compactness of modes in the space-time domain in a manner similar to the EPRT algorithm is used.
- the difference is that while constructing the broadband propagators as in equation 13, a reference location z 0 at the centroid of the sensor array is chosen, i.e., replace the z, by z, - Zo in equation 13.
- FIG. 19 A corresponding step (1900) is shown in figure 19.
- This f-k domain processing is followed by a model order selection and a mode consolidation step (1902, figure 19) which is modified to include estimates of time location.
- the model order selection is now done based on clustering in the phase slowness and time location domain. The reason for this is that time location estimates obtained from the broadband processing in f-k domain are more robust than the group slowness estimates. The fact that time compactness of the modes implies a linear phase relationship across frequency in the mode spectrum is exploited to obtain the time location estimates.
- broadband propagators in the space-time domain each of which is defined as a time compact window propagating at the group slowness with a complex phase change across sensors in proportion to the difference of the phase and group slowness can be considered.
- u ⁇ (t) denote a rectangular window function of width T centered at zero.
- the broadband space time propagator at a scale a can be written as -
- C a [C 1 (a,b ⁇ ...,C M (a,b)] is the collection of CWT coefficients for M modes to be estimated at the reference sensor location z 0 in the respective time window of width T around time locations t o ⁇ ...,U M . Note that this is an over-determined system of equations and in order to estimate the CWT coefficients at the test moveout, the minimum mean square error (MMSE) estimate under the observation model is formed.
- MMSE minimum mean square error
- e is the residual error for the M-tuple test moveouts and (.)* denotes the pseudo- inverse operation.
- a combinatorial search is performed over all possible M tuples of test moveouts and the combination that minimizes the residual error is selected, i.e.,
- Step 1 Execute a broadband processing in band F - o Ia. Construct an over-complete dictionary of space time propagators ⁇ in band F for a given range of phase and group slowness (see step 1204, figure 12) and pose the problem as the problem of finding sparse signal representation in an over-complete basis. In particular solve the optimization problem OPT. 1 o Ib. Pick the regularization parameter ⁇ " in OPT 1 using KS-test between residuals, i.e. by executing steps in Table A.
- Step 2 Model order selection and mode consolidation (1904, figure 19) - Depending on whether one utilizes time information or not this step can be done in two ways o Model order selection (A) - No use of time localization of modes. Execute steps in Table B. Stop and go to next band. o Model order selection (B) - Use time localization of modes. Execute steps in Table C. Go to Step 5.
- A Model order selection
- B Use time localization of modes.
- Execute steps in Table C Go to Step 5.
- Step 3 For each mode choose a range of move-outs around the group slowness estimates and build space-time propagators using the phase slowness estimates and time location estimates of the modes.
- Step 5 (shown as 1910, figure 19): Update group slowness estimates -
- FIG. 20 shows the array of received waveforms comprising two time overlapping modes and added noise.
- the SNR is set to be 0 dB in the sense of total signal to total noise energy.
- the exponential model is given a perturbation by incorporating sensor gain and phase errors to make the simulation more realistic.
- Figure 21 shows the result of applying the described approach in both the f-k and space-time domains in four frequency bands.
- the solid lines represent the true dispersion curves and the curves marked by circles are the dispersion curves extracted by estimating the phase and group slownesses in these bands. The match of the estimate to the true curves validates the described approach.
- features of the invention may be implemented in computer programs stored on a computer readable medium and run by processors, application specific integrated circuits and other hardware. Moreover, the computer programs and hardware may be distributed across devices including but not limited to tooling which is inserted into the borehole and equipment which is located at the surface, whether onsite or elsewhere.
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| Application Number | Priority Date | Filing Date | Title |
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| GB1108626.1A GB2477470B (en) | 2008-12-22 | 2009-12-22 | Automatic dispersion extraction of multiple time overlapped acoustic signals |
| CA2751717A CA2751717C (en) | 2008-12-22 | 2009-12-22 | Automatic dispersion extraction of multiple time overlapped acoustic signals |
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| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| US10317545B2 (en) | 2012-03-12 | 2019-06-11 | Schlumberger Technology Corporation | Methods and apparatus for waveform processing |
| US20140169130A1 (en) * | 2012-12-13 | 2014-06-19 | Schlumberger Technology Corporation | Methods and Apparatus for Waveform Processing |
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| CA2751717C (en) | 2015-10-06 |
| US20130114376A1 (en) | 2013-05-09 |
| GB201108626D0 (en) | 2011-07-06 |
| US8755249B2 (en) | 2014-06-17 |
| US20100157731A1 (en) | 2010-06-24 |
| CA2751717A1 (en) | 2010-07-01 |
| GB2477470A (en) | 2011-08-03 |
| GB2477470B (en) | 2013-02-06 |
| US8339897B2 (en) | 2012-12-25 |
| WO2010075412A3 (en) | 2010-10-07 |
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