The Rôle And Fate Of The Connate Water In Oil And Gas Sands (c465335a-74c0-4363-a34d-e8e12d72d82a)

The American Institute of Mining, Metallurgical, and Petroleum Engineers
C. W. Washburne
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
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4
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200 KB
Publication Date:
Jan 9, 1915

Abstract

Continued discussion of the paper Of ROSWELL H. JOHNSON, presented at the New York meeting, February, 1015, and printed in Bulletin No. 98, February; 1915, pp. 221 to 226. See also Bulletin No. 101, May, 1915, pp. 1157 to 1162, and No. 103, July, 1915, pp. 1449 to 1450. C. W. WASHBURNE, New York, N. Y. (communication to the Secretary*).-Mr. Johnson recognizes that connate waters must be driven, outward toward the earth's surface. He considers the ascent due to the settling and packing of the underlying sediments and to the formation of gas within the rocks, supplemented by abyssal pressures. The origin of the methane in the sedimentary strata probably is not simple. There are three possible modes of origin: (1) as marsh gas formed near the surface and entrapped in the sediments; (2) from abyssal sources; (3) by the decomposition of organic matter buried in the sediments. The abyssal source is generally negligible, and in all cases doubtful. The third origin is the most important in the gas fields. A fourth mode of origin, by the dissociation of liquid hydrocarbons, frequently has been suggested, but it is improbable, because crude oils are exothermic. Therefore they have no tendency, to split or decompose at low temperatures, as do endothermic substances, such as coal, which is geologically by the loss of methane, water, and carbon dioxide. This cannot happen to a hydrocarbon until its temperature of dissociation (" cracking point") is reached, which is over 250'.C. for the most easily cracked hydrocarbons and over 400° C. for others. Engler says that the dissociation of fats and waxes into oils is an endothermic process, thereby unconsciously nullifying his own theory of the dissociation of these substances at low temperatures. However, recently I have found reason to think that heat is liberated by the disruption of the molecules of fats and waxes, as it is in the molecular decomposition of the substances of wood, coal, etc. If this tentative opinion is correct, and Engler wrong, then it seems that the Engler-Höfer hypothesis of the origin of oil becomes not only possible, but even probable.
Citation

APA: C. W. Washburne  (1915)  The Rôle And Fate Of The Connate Water In Oil And Gas Sands (c465335a-74c0-4363-a34d-e8e12d72d82a)

MLA: C. W. Washburne The Rôle And Fate Of The Connate Water In Oil And Gas Sands (c465335a-74c0-4363-a34d-e8e12d72d82a). The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1915.

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