In re Taner

681 F.2d 787, 214 U.S.P.Q. (BNA) 678, 1982 CCPA LEXIS 140
Court of Customs and Patent Appeals·Decided June 10, 1982·No. Appeal No. 81-598·Published·Cited by 15 cases

Opinion

MARKEY, Chief Judge.

Taner et al. (Taner) appeal from a decision of the Patent and Trademark Office Board of Appeals (board) sustaining the rejection of Claims 1, 2, 4 through 15, 21, and 24 through 36 under 35 U.S.C. § 101 and the rejection of Claims 1, 2, 6, 7, 9, 21, 24, 25, 26, 28, 29, 31, and 36 under 35 U.S.C. § 103 in appellants’ application Serial No. 548,572, filed February 10, 1975, entitled “Seismic Exploration with Simulated Plane Waves.” We reverse.

Background

I. The Invention

Appellants’ invention relates to a method of seismic exploration by which substantially plane or substantially cylindrical seismic energy waves are simulated from substantially spherical seismic waves.

In traditional methods of seismic exploration, seismic sources generate and transmit into the earth seismic energy waves. The waves are propagated through the earth in spherical or near-spherical wavefronts and are reflected by subsurface formations. The reflections return to the earth’s surface and are detected by seismic receivers positioned over the area of exploration. The receivers convert the reflections into electrical signals which are then recorded on a record medium, e.g., magnetic tape or chart recorder. The recorded signals contain information on the geological substrata explored. For that information to be meaningful, it must, however, be corrected for various factors, such as spherical divergence of the waves as they are propagated through the substrata.

Appellants’ claimed process simulates substantially plane or cylindrical seismic en[788]*788ergy waves by summing the reflectional signals of the conventional spherical waves. The composite signal thus represents the response of subsurface formations to plane or cylindrical waves. Claims 1 and 24, the only independent claims, are illustrative:

1. A method of seismic exploration by simulating from substantially spherical seismic waves the reflection response of the earth to seismic energy having a substantially continuous wavefront over an extent of an area being explored having at least one dimension which is large relative to a seismic wavelength, comprising the steps of:
(a) imparting the spherical seismic energy waves into the earth from a seismic source at a source position;
(b) generating a plurality of reflection signals in response to the seismic energy waves at a set of receiver positions spaced in an array over an extent having at least one dimension which is large relative to a seismic wavelength; and
(c) summing the reflection signals to form for the source position a signal simulating the reflection response of the earth to seismic energy having a substantially continuous wavefront over at least one dimension which is large relative to a seismic energy wavelength.
24. A method of seismic exploration by simulating from substantially spherical seismic waves the reflection response of the earth to seismic energy having a substantially continuous wavefront over an extent of an area being explored having at least one dimension which is large relative to a seismic wavelength, comprising the steps of:
(a) imparting the spherical seismic energy waves into the earth from a set of seismic sources at source positions spaced in an array over an extent having at least one dimension which is large relative to a seismic wavelength;
(b) generating a reflection signal at a receiver position in response to each of the seismic energy waves; and
(c) summing the reflection signals to form for the receiver position a signal simulating the reflection response of the earth to seismic energy having a substantially continuous wavefront over at least one dimension which is large relative to a seismic energy wavelength.1

According to appellants’ specification, the combining of signals to simulate plane or cylindrical wavefronts makes possible a reduction in data correction and thereby reduces the expenditures of time and money required for seismic exploration.

II. The Rejections

A. 35 U.S.C. § 101

In his final rejection, the examiner stated that because appellants’ claims define a method of seismic data treatment which is not limited to any apparatus, the claims preempt all implementations of the claimed “mathematical and manipulative” operations upon seismic data, and, as such, fall outside the statutory categories of § 101.

In sustaining that rejection, the board undertook to apply the test established by this court in In re Freeman, 573 F.2d 1237, 197 U.S.P.Q. 464 (CCPA 1978), as modified by In re Walter, 618 F.2d 758, 205 U.S.P.Q. 397 (CCPA 1980). The board found that the claims directly recite a mathematical algorithm, i.e., summing, and that because “there is no close relationship between the algorithm .. . and the other process steps except that the signals to be summed are generated by the precedent process steps,” the claims preempt that algorithm. The board concluded therefore that the claims are nonstatutory. That the claims limit the algorithm to geophysical exploration and thus do not literally preempt the algorithm was not in the board’s view sufficient to save the claims from characterization as nonstatutory. Citing In re Christensen, 478 [789]*789F.2d 1392, 178 U.S.P.Q. 35 (CCPA 1973), which it viewed as directly on point, the board characterized appellants’ claims as directed to the solution of a mathematical equation. In the board’s view, the precedent steps merely served to supply the equation with required data and, as in Christensen, could not “convert the unpat-entable method to patentable subject matter.” 478 F.2d at 1394, 178 U.S.P.Q. at 37-38.

On reconsideration, the board reviewed its decision in light of Diamond v. Diehr, 450 U.S. 175, 101 S.Ct. 1048, 67 L.Ed.2d 155, 209 U.S.P.Q. 1 (1981), concluding that its original analysis conformed with Diehr. One board member dissented, viewing appellants’ claims not “as an attempt to patent the concept of summing signals in general but rather to be drawn to a technique of forming a new type of seismic recording which simulates the response of subsurface formations to cylindrical or plane waves.”

B. 35 U.S.C. § 103

Three references were cited and relied upon by the examiner in making the § 103 rejection:

Smith, Jr. (Smith) 3,256,501 June 14,1966

Laurent 3,775,737 Nov. 27,1973

Miller, Dr. G. Kirby, “High Pressure Transducer,” Technical Report GTE Sylvania, Jan. 10, 1973.

Free access — add to your briefcase to read the full text and ask questions with AI

In re Taner, 681 F.2d 787, 214 U.S.P.Q. (BNA) 678, 1982 CCPA LEXIS 140 (ccpa 1982).

681 F.2d 787 (In re Taner) — published by Counsel Stack Legal Research, free access to 12M+ legal documents.

Related

In Re Bilski
545 F.3d 943 (Federal Circuit, 2008)
In Re Karen I. Trovato and Leendert Dorst
42 F.3d 1376 (Federal Circuit, 1994)
In Re Rex D. Schrader and Eugene D. Klingaman
22 F.3d 290 (Federal Circuit, 1994)
In Re Ralph R. Grams and Dennis C. Lezotte
888 F.2d 835 (Federal Circuit, 1989)
In re Abele
684 F.2d 902 (Customs and Patent Appeals, 1982)
In re Pardo
684 F.2d 912 (Customs and Patent Appeals, 1982)