Application of Giorgio G. Soli

317 F.2d 941, 50 C.C.P.A. 1288
CourtCourt of Customs and Patent Appeals
DecidedJune 6, 1963
DocketPatent Appeal 6999
StatusPublished
Cited by8 cases

This text of 317 F.2d 941 (Application of Giorgio G. Soli) 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 Giorgio G. Soli, 317 F.2d 941, 50 C.C.P.A. 1288 (ccpa 1963).

Opinion

RICH, Judge.

This appeal is from the decision of the Patent Office Board of Appeals affirming the examiner’s rejection of method claim 13, the sole claim in application Ser. No. 587,521, filed May 28, 1956, for “Petroleum and Natural Gas Prospecting.”

The basis for and the general nature of appellant’s invention is disclosed in the specification as follows:

“The method is based on the fact that, in many instances in oil and gas areas, gaseous hydrocarbons are slowly escaping through the sedimentary formations to the surface. These gases serve as a steady supply of carbon and energy to hydrocarbon-oxidizing bacteria, resulting in the intensive multiplication of these micro-organisms.
****** “The present invention is directed to a method of determining the presence and relative amounts of hydrocarbon-oxidizing bacteria in the soil, these bacteria being an indication of the presence of petroleum hydrocarbons. A feature of the invention is utilization of the ability of hydrocarbon-oxidizing bacteria to grow and produce turbidity [i. e., a murky or muddied condition] in a liquid mineral culture medium in which a hydrocarbon gas is dissolved.”

Claim 13 reads as follows (the breakdown being ours):

“13. A method of prospecting for subterranean hydrocarbon deposits comprising the steps of “[1] collecting samples of soil at various depths in certain locations in a prospective area,
“[2] incubating at least one culture of each of said soil samples in a mineral nutrient liquid medium in the presence of an atmosphere of methane,
“[3] simultaneously incubating at least another of said cultures of each of the same soil sample in a mineral nutrient liquid medium in the presence of an atmosphere of propane,
“ [4] simultaneously incubating an additional culture of said *943 same soil sample in a mineral nutrient liquid medium in the presence of atmospheric air,
“[5] determining the amount of hydrocarbon-oxidizing bacteria in said cultures by
“(a) a measurement of the amount of turbidity of said nutrient medium caused by the growth of said bacteria exposed to said methane and propane atmospheres, and
“(b) using said culture incubated in the presence of atmospheric air as a control for said first-mentioned cultures,
“[6] the ratio of soil to culture medium being kept to a minimum.”

The Patent Office has rejected this claim as unpatentable over the combined teachings of the following references:

Taggart 2,349,472 May 23, 1944 Strawinski 2,665,237 Jan. 5, 1954 Porter, Bacterial Chemistry and Physiology, John Wiley & Sons, Inc., 1946, page 95.

Both Taggart and Strawinski disclose methods of prospecting for subterranean hydrocarbon deposits which include collecting samples of soil at various depths in certain locations in a prospective area and thereafter employing various means to analyze the amount of and/or kind of hydrocarbon-oxidizing bacteria in such samples. The pertinence of the Porter reference will be discussed later.

Appellant’s several arguments as to why the references of record would not render his invention obvious to one skilled in the art will be considered as they relate to the above-designated sections of his claim.

Section [1]: Soil Sampling Depth. Appellant argues in his brief “Particular attention is given [in appellant’s invention] to the depth of sampling in relation to the amount of organic matter in the soil, since appreciable amount of such organic matter could unfavorably affect the final results. The amount of organic matter decreases with depth; therefore, the deeper the samples within certain limits, the more reliable the . results. Decomposition of organic matter in the first layers of soil could give rise to methane gas, which would support methane-oxidizing bacteria, which, in turn, would furnish false positive results as far as the presence of oil and gas at greater depths is concerned. For this reason alone, it is submitted, appellant’s claim is patentable over Taggert [sic], who specifies 6 inches of surface soil, and Strawinski, who also specifies surface soil at a slightly greater depth. [Strawinski designates this depth as “below six inches, preferably at depths of 24" or more.”]”

It is clear that the disclosure in appellant’s specification does not make soil-sampling depth critical. At one portion thereof it states that soil samples should be taken “at a depth not less than 6 feet.” Another portion thereof states, however, merely that soil samples should be collected “at a depth where organic matter is reduced to a minimum.” In view of these facts and additionally in view of the fact that we can see no distinction of substance between a depth of soil sampling which may be less than 6 feet and one, as disclosed in Strawinski, which may be two feet “or more” we are not persuaded, by appellant’s argument that we should “interpret” the claim in the light of his specification disclosure, that even such an “interpretation” would distinguish the claim from the prior art. All the claim contains by way of limitation is “various depths.” It appears to include depths of the prior art.

Sections [2] and [3]: Simultaneously Incubating in Different Atmospheres Portions of the Same Soil Sample in a Liquid Medium.

Appellant’s specification discusses this aspect of his invention as follows:

“ * * * this invention is directed to the simultaneous isolation of bac *944 teria able to use methane and to bacteria which attack ethane or propane but which may not be able to use methane. Since we know that neither ethane nor propane are commonly found in soil as a result of decomposition of organic matter, the separate use of methane and propane (or ethane) as test gasses on the same soil sample is an important part of this invention.”

To this end appellant places a measured amount of a liquid “culture medium” into five vials. 1 These vials are then “innoculated” with measured amounts of soil. Two of the vials are then filled with methane, two with propane. The contents of the fifth vial will be discussed, infra. The vials are then incubated for two weeks at a temperature of approximately 28° to 30°C.

As to the reason why methane and propane atmospheres should not be mixed, the specification says:

“If growths occurred only in the cultures incubated under an atmosphere of methane, the results for these particular soil samples are held as questionable, for the presence of bacteria able only to oxidize methane, cannot be taken as a positive indication of petroleum hydrocarbons for reasons explained above. If bacterial growth occurred both in methane and propane-exposed cultures, then the results are recorded as positive.” 2

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Bluebook (online)
317 F.2d 941, 50 C.C.P.A. 1288, Counsel Stack Legal Research, https://law.counselstack.com/opinion/application-of-giorgio-g-soli-ccpa-1963.