Application of Manus R. Foster, Clyde W. Kerns and Raymond L. Sengbush

438 F.2d 1011, 58 C.C.P.A. 1001, 169 U.S.P.Q. (BNA) 99, 1971 CCPA LEXIS 387
CourtCourt of Customs and Patent Appeals
DecidedMarch 18, 1971
DocketPatent Appeal 8432
StatusPublished
Cited by14 cases

This text of 438 F.2d 1011 (Application of Manus R. Foster, Clyde W. Kerns and Raymond L. Sengbush) is published on Counsel Stack Legal Research, covering Court of Customs and Patent Appeals primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Application of Manus R. Foster, Clyde W. Kerns and Raymond L. Sengbush, 438 F.2d 1011, 58 C.C.P.A. 1001, 169 U.S.P.Q. (BNA) 99, 1971 CCPA LEXIS 387 (ccpa 1971).

Opinion

ALMOND, Judge.

This is an appeal from the decision of the Patent Office Board of Appeals affirming the rejection of claims 1-4, 7-13, 15-20, and 26-27 of appellants’ application entitled “Processing of Geophysical Data.” 1 No claims have been allowed.

The invention relates to processing seismograms to compensate for the effect of distortion present in obtaining the seismograms and to emphasize the characteristics of the geological formations producing the seismograms. Representations of geological formations are commonly obtained by producing a seismic impulse, for example, by exploding dynamite. The seismic energy travels through subsurface formations, is reflected from reflecting interfaces, and detected by sensitive receivers. A seismogram is produced by recording, on a magnetic tape for example, the electrical signals generated from the receiver. Appellants state that all such geophysical data include distortion, which often ob *1013 scures the desired characteristics of the geological formations.

Appellants have found that the distortion present in a particular seismogram can be characterized by autocorrelating the seismogram and then smoothing the spectrum of the resultant autocorrelation function. That is, the reflectivity component of the autocorrelation function has ragged spectral variations, while the distortion component has a comparatively smooth spectrum. Therefore, spectral smoothing of the autocorrelation function suppresses the reflectivity component. The resultant output characterizes the distortion present in the seismogram. One way of smoothing the spectrum of the autocorrelation function is by truncation. Having obtained the distortion, the inverse filter coefficients are determined by prior art techniques. When the seismogram is applied to this inverse filter, the distortion is removed. Appellants disclose that their process can be carried out by a digital computer or analog apparatus.

Appellants’ claims vary from method (claims 1-4, 7-13 and 15-18), to use of apparatus (claims 19-20), to apparatus (claims 26-27). Claims 4, 19, and 26 are reproduced as illustrative of each type of claim:

4. The method of processing geophysical data to compensate for the effect of distortion present in said geophysical data and to emphasize the characteristics of the geological formations producing said geophysical data comprising:

selecting a portion of said geophysical data,

correlating said portion of said geophysical data to obtain a signal having a distortion component representing said distortion and having a reflectivity component representing said characteristics of said geological formations, truncating said signal to produce spectral smoothing thereby separating said distortion component from said reflectivity component, inverting said distortion component to produce an inverse distortion operator,

deriving from said inverse distortion operator an inverse filter, and applying said geophysical data to said inverse filter to produce an output emphasizing said characteristics of said geological formations.

19. In the processing of geophysical data to compensate for the effect of distortion present in obtaining said geophysical data and to emphasize the characteristics of the geological formations producing said geophysical data, the new use of computing apparatus, said computing apparatus being interconnected to include:

a correlator,
a smoothing filter for smoothing the spectrum of the signal applied to the input,
an inverter producing as an output coefficients of a filter which is the inverse of the signal applied to the input, and an inverse filter, said new use comprising:
applying said geophysical data to said correlator to produce as an output a signal having a distortion component representing said distortion and a reflectivity component representing said characteristics of said geological formations, applying said last-named signal to said smoothing filter to smooth the spectrum of said signal thereby separating said distortion component from said reflectivity component, applying the output of said smoothing filter, representing said distortion component, to said inverter to produce as an output of said inverter the coefficients of a filter which is the inverse of said distortion component,
applying said coefficients to said inverse filter to provide an inverse filter having filtering which is the inverse of the distortion operator, and
*1014 applying said geophysical data to said inverse filter to produce an output emphasizing said characteristics of said geological formations.
26. Computing apparatus for processing seismograms to compensate for the effect of distortion present in obtaining said seismograms and to emphasize the characteristics of the geological formations producing said seismograms comprising: means for converting said seismo-grams to electrical signals of the type which can be operated upon by said computing apparatus,
a correlator, said electrical signals being applied to said correlator to produce as an output an electrical signal having a distortion component representing said distortion and a reflectivity component representing said characteristics of said geological formations,
a smoothing filter for smoothing the spectrum of the signal applied to the input, the output of said cor-relator being applied to said smoothing filter to smooth said spectrum thereby producing an output representing said distortion component and suppressing said reflectivity component,
an inverter producing as an output coefficients of a filter having characteristics which are the inverse of the signal applied to the input of said inverter, the output of said smoothing filter, representing said distortion component, being applied to said inverter to produce, as an output of said inverter, filter coefficients which are the inverse of said distortion component,
an inverse filter, said filter coefficients being applied to said inverse filter so that said inverse filter has filtering characteristics which are the inverse of said distortion, and
means for applying said seismo-grams to said inverse filter to produce an output emphasizing said characteristics of said geological formations.

It is noted that method claims 1-3 differ from method claim 4 in one aspect in that “electrical signals” are recited rather than “signals” alone. In addition, claims 9 and 18 recite only the method of characterizing the distortion and not the complete method of processing geophysical data, which includes the derivation of inverse filter coefficients and applying the data to the inverse filter.

While various statutory bases (35 U.S. C. §§ 100, 101

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438 F.2d 1011, 58 C.C.P.A. 1001, 169 U.S.P.Q. (BNA) 99, 1971 CCPA LEXIS 387, Counsel Stack Legal Research, https://law.counselstack.com/opinion/application-of-manus-r-foster-clyde-w-kerns-and-raymond-l-sengbush-ccpa-1971.