Gerald C. Summers v. Charles B. Vogel

332 F.2d 810, 52 C.C.P.A. 716
CourtCourt of Customs and Patent Appeals
DecidedJune 11, 1964
DocketPatent Appeal 7143
StatusPublished
Cited by7 cases

This text of 332 F.2d 810 (Gerald C. Summers v. Charles B. Vogel) 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
Gerald C. Summers v. Charles B. Vogel, 332 F.2d 810, 52 C.C.P.A. 716 (ccpa 1964).

Opinion

WORLEY, Chief Judge.

Summers appeals from the decision of the Board of Patent Interferences awarding priority of invention in Interference No. 88,790 to Vogel. Summers, the junior party, is involved on the basis of his application, Serial No. 287,853, filed May 15, 1952. Although Vogel’s application involved in the interference is Serial No. 493,999, filed March 4, 1955, he was made senior party on the basis of his application Serial No. 284,867, filed on April 29, 1952, of which the former is a continuation-in-part.

Both parties submitted testimony, that of Summers being in the form of a stipulation accompanied by affidavits and exhibits.

The board regarded the preliminary statement of Summers as limiting the earliest date he can establish for conception, if the evidence on his behalf be found sufficient, to April 4, 1952. It also noted that Summers alleged no actual reduction to practice prior to his filing date. Observing that Vogel thus needs only to establish conception of the invention in issue prior to April 4, 1952, in order to prevail, the board considered Vogel’s evidence. Finding that evidence sufficient to prove conception, the board awarded priority to Vogel without finding it necessary to consider the evidence of Summers.

The invention in issue relates to a system for making seismic measurements in the logging of earth formations traversed by a borehole. It is defined by the sole count as follows:

“In a system for seismic measurements, surface apparatus comprising a recording unit, subsurface apparatus adapted to be lowered into a borehole, means supporting said subsurface apparatus in said borehole, said subsurface apparatus comprising an acoustic wave source and two receivers spaced from each other *811 along a vertical line, said receivers being mounted to one side of said wave source, a single electric circuit means connecting both said receivers to said recording unit, means for energizing said wave source to produce an acoustic impulse reaching said two receivers in succession, means in each receiver for translating said impulse into an electric signal to be transmitted by said circuit means to said recording unit, and switching means in said subsurface apparatus actuated upon the production of said acoustic impulse for disconnecting the receiver nearest to said wave source from said circuit means.”

The general nature and purpose of the type of system involved here is explained by Summers in his brief:

“In the search for oil, considerable information as to the nature and character of the earth’s formations can be obtained by measuring the velocity at which sound will travel through the formations. These velocity measurements indicate at once whether or not a subsurface formation comprises high-velocity consolidated strata, such as a limestone, or whether it may comprise low-velocity material, such as sand.
“As early as 1938, the measurement of the velocity of sound along the earth’s formations surrounding a borehole was proposed. The Wyckoff patent No. 2,233,992 1 * * * * includes a full disclosure of such system which includes a cable * * for the lowering of three transducer units into the borehole. One unit is a source of sound periodically energized. The sound from this source traverses the formations adjacent the borehole and the time of travel from the source to a first detector is determined by the response from the first detector. A second detector spaced from the first detector provides additional information on the time of travel from the transmitter to this more remote detector.
“By the simple algebraic equations of the Wyckoff patent * * it is shown that by subtracting the time of travel of a sound pulse from the transmitter to the near receiver from the time of travel from the transmitter to the far receiver, there is obtained the difference which represents the time required for the pulse to travel from the first receiver or detector to the second receiver or detector. This time A T is then independent of the path through the liquid in the borehole and represents only the time of travel along the earth’s formations surrounding the borehole.”

The Vogel application in interference includes a disclosure of a three transducer system of the type referred to above with the transducers arranged in longitudinally spaced relationship in an elongated tubular casing adapted to be lowered into a borehole by means of a cable attached to one end of the housing. The transducer at one end of the housing is the source of sound or transmitter with the result that the two receiving transducers or receivers are at different distances from the transmitter on one side thereof as in the prior art system discussed in the above quotation from Summer’s brief. Included in the'housing is electric and electronic equipment necessary for the operation of the transmitter and receivers. Connections are made from that equipment through the cable to apparatus maintained at the surface outside the borehole.

The surface apparatus includes a main power supply, a synchronizing network including all necessary synchronizing, calibrating and sweep circuits, a cathode ray oscilloscope energized from the output of the synchronizing network, a depth indicator connected to a Selsyn generator operated in coordination with the position of the housing in the borehole, and a camera electrically connected to the out *812 put of the synchronizing network and the depth indicator to provide photographs showing the time relationship of the signals from the receivers in response to the output signals from the transmitter. Filter circuits are provided to effect the separation of energizing power from the power supply, actuating impulses from the synchronizing network and incoming signals from the receivers.

The transmitter specifically disclosed provides the required sound signals by producing spark discharges at desired intervals. It is provided with alternating current from the power supply at the surface, which current is rectified to charge a capacitor, and includes timing and relay circuits which are actuated by energizing signals delivered thereto at proper time intervals from the surface to cause the capacitor to discharge through the spark gap.

The spark discharge produces a sound impulse of steep wave front which travels to the borehole wall and through the wall towards the two receivers, parts of the impulse energy passing to the receivers in sequence to produce electrical signals there in and those signals being transmitted through the cable to the surface for display in timed relationship on the oscilloscope.

The most significant feature by which the present system distinguishes over the prior art system appears to be the means meeting the last recitation of the count reading as follows:

“ * * * and switching means in said subsurface apparatus actuated upon the production of said acoustic impulse for disconnecting the receiver nearest to said wave source from said circuit means.”

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Bluebook (online)
332 F.2d 810, 52 C.C.P.A. 716, Counsel Stack Legal Research, https://law.counselstack.com/opinion/gerald-c-summers-v-charles-b-vogel-ccpa-1964.