In Re D. Raymond Young and John C. Wride

927 F.2d 588, 18 U.S.P.Q. 2d (BNA) 1089, 1991 U.S. App. LEXIS 3386, 1991 WL 26685
CourtCourt of Appeals for the Federal Circuit
DecidedMarch 5, 1991
Docket90-1368
StatusPublished
Cited by21 cases

This text of 927 F.2d 588 (In Re D. Raymond Young and John C. Wride) is published on Counsel Stack Legal Research, covering Court of Appeals for the Federal Circuit primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
In Re D. Raymond Young and John C. Wride, 927 F.2d 588, 18 U.S.P.Q. 2d (BNA) 1089, 1991 U.S. App. LEXIS 3386, 1991 WL 26685 (Fed. Cir. 1991).

Opinion

RADER, Circuit Judge.

Raymond Young and his co-inventor John Wride (collectively Young) appeal from the October 31, 1989 and April 18, 1990 decisions of the Board of Patent Appeals and Interferences (Board). These decisions affirmed the final rejection of all claims in their application. The Board held Young’s claimed invention obvious under 35 U.S.C. § 103. This court affirms.

BACKGROUND

Young’s application discloses a method and apparatus for generating an acoustic pulse in water. Acoustic pulse technology facilitates offshore seismic exploration. The acoustic pulse generates a large gas bubble in the ocean above geological formations on the ocean floor. The rapid expansion and collapse of the gas bubble create a shock wave in the water. The shock wave propagates through the water into the formations below the ocean bed. As the shock wave passes downward through these formations, each interface between adjoining earth strata reflects a portion of the shock wave. These reflections move upward through the ocean. Hydrophones at the ocean’s surface can monitor these reflections. From these monitored reflections, geologists can generate a “seismic section” map which shows the configuration of strata in the ocean bed.

Today’s most common sources of seismic shock waves are air guns. These air guns feature a chamber for storing and releasing on command highly compressed air. A high-pressure hose charges the gun with compressed air for rapid firing during a seismic survey.

Acoustic pulse technology suffers from problems with bubble oscillation. Upon release of the compressed air, the bubble undergoes a rapid initial expansion and collapse. Several more expansions and collapses follow the initial collapse, but with diminishing amplitude. Each of these expansion-collapse events creates an additional shock wave. The geological strata reflect each of these additional shock waves. The multiple reflections, in turn, blur the resolution of the seismic section. Most blurring comes from the first oscillation after the initial bubble collapse.

*590 Acoustic pulse technology uses a “primary-to-bubble ratio” to measure susceptibility to oscillation. This ratio compares the shock wave intensity of the initial expansion-collapse to the intensity of the first oscillation. A high ratio means the secondary shock waves are less likely to blur the seismic section.

Young tries to raise the primary-to-bubble ratio above prior art air gun sources by reducing the amplitude of the first oscillation. Young seeks this result by spacing at least three air guns in a characteristic array. The array separates the guns from each other by a critical distance. The distance, D, is at least 1.2 times greater than R, but less than or equal to twice R. R is the maximum radius of the initial air bubble from each gun. * With this spacing, the bubbles from each .gun intersect before any single bubble reaches its maximum radius. This intersection dampens the overall oscillation. Young's independent claims each include a spacing limitation within this range.

Independent claim 1 is illustrative:

A method of producing a seismic pulse in a body of water, including the steps of:
(a) disposing in the water a set of at least three air guns, each adapted to produce in the water a gas bubble having maximum radius substantially equal to the quantity R, where the guns are disposed at depths such that each produces, when fired, a bubble of maximum radius R, and the guns are disposed such that each gun is separated from each of the nearest guns thereto in the set by a critical distance, D, where D is substantially equal to V 2R; and
(b) firing the air guns substantially simultaneously to produce a seismic pulse in the water.

Young’s dependent claims define the number of the guns or their placement relative to each other or to the ocean surface.

The examiner rejected each of the claims as obvious under 35 U.S.C. § 103 in light of five prior art references. The examiner relied primarily on U.S. Patent No. 2,619,-186 to Carlisle (the “Carlisle patent” or “Carlisle”) to reject Young’s claims. Car-lisle is the only reference cited by the examiner or Board which suggests the air gun spacing in Young’s claims.

Young contested the Board’s and the examiner's consideration of Carlisle. Young argued that Carlisle concerns reducing bubble oscillation for chemical explosives, not air guns. Young also argued that an article by Knudsen published six years after Carlisle in the journal Geophysics expressly discredits the teachings of Carlisle. W. Knudsen, Elimination of Secondary Pressure Pulses in Offshore Exploration (A Model Study), 23 Geophysics No. 3 at 440 (July 1958) (Knudsen). Therefore, Young contended, a person of ordinary skill in the seismic exploration art would not have considered Carlisle when developing an improved seismic array.

The Board rejected Young’s arguments. The Board held that the examiner appropriately applied Carlisle notwithstanding the teachings of Knudsen. On appeal, Young asserts as error only the propriety of applying Carlisle as a reference in light of Knudsen’s allegedly contrary teachings.

DISCUSSION

This court must decide whether the Board properly affirmed the examiner’s rejection over Carlisle. Young has not challenged the other references cited in the examiner’s rejection. Further, Young has not argued the merits of any particular claim apart from the others. Therefore, all claims stand or fall together with representative independent claim 1. See In re Kaslow, 707 F.2d 1366, 1376, 217 USPQ 1089, 1096 (Fed.Cir.1983).

The Carlisle patent — “Seismic Exploration Method” — issued on November 25, 1952. Carlisle concerns minimizing bubble oscillation for chemical explosives used in marine seismic exploration. Carlisle controls bubble oscillation by spacing seismic sources to achieve a reduction of the secondary pressure pulse. Carlisle specifieal *591 ly teaches spacing the seismic sources close enough to allow the bubbles to intersect before reaching their maximum radius. Carlisle spaces the bubble centers closer than two maximum bubble radii, or less than “2.0 R” in Young’s notation. Carlisle, col. 3, lines 57-60. Carlisle explains:

[T]he secondary energy normally available from these sources is dissipated by their mutual intersection and tends to eliminate the secondary seismic impulses created when the walls of the bubbles collapse.

Id. at lines 60-64. Thus, Carlisle expressly teaches the spacing limitation in each of Young’s claims.

Notwithstanding Carlisle’s teachings, Young argues that the Knudsen article discredits Carlisle. Knudsen describes a series of tests which evaluated four proposed techniques for suppressing bubble oscillation. Carlisle was one of the four.

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927 F.2d 588, 18 U.S.P.Q. 2d (BNA) 1089, 1991 U.S. App. LEXIS 3386, 1991 WL 26685, Counsel Stack Legal Research, https://law.counselstack.com/opinion/in-re-d-raymond-young-and-john-c-wride-cafc-1991.