Access to Energy

DEVONIAN SHALE

As for gas from geopressurized zones (AtE May 1977), there are all the expected problems: It is a dilute source, yielding about 1.5 Mcf of methane for every 10 barrels of hot brine, whose energy is not easily harnessed; and the spent water must be disposed of. But the rewards would be enormous for the US, a century, and perhaps a millenium, of natural gas at present rates of consumption. Proving this resource viable will also be important to the rest of the world: 45 countries may have geopressurized zones, and the hot brine can be flashed into steam, which can then be condensed into drinking water. But for the present, geopressurized methane is only the subject of a DOE research program.

There is, however, yet another source of natural gas Devonian shale. Devonian is the name of the geological age some 350 million years ago when ferns and forests had just been invented (mammals were still 300 million years away). In those days, there was a mountain range west of the present Atlantic coast line, and rivers flowed westward to a great compound delta into the sea, which was then in the Ohio-Kentucky region, at times merging with the seas in the Michigan and Illinois basins. The delta was in what is now the Appalachian Basin, and the rivers deposited mud, silt and sand, which became Devonian shale; every year, the rivers would also wash organic material, mostly derived from plants, into this sea, and these sediments became deep brown layers called Brown shale within the Devonian shale. The couplets of dark (organic) and light (inorganic) shale are reminiscent of annual tree rings, and even more of the annual layers in Colorado and Wyoming oil shale, except that the organic layers in oil shale are kerogen, whereas Brown shale is coal like matter. The couplets in Devonian shale are very thin - there are as many as 46 to an inch of thickness.

This is what resulted from stratification in a stagnant condition, preventing the organic matter from being oxidized and destroyed. Over the next hundreds of millions of years, it was covered with about 3,000 ft of overburden and turned into coal; also, the carbohydron molecules, or some of them, were cracked in much the same way as in a refinery, until they were down to the simplest form methane, the main ingredient of natural gas. Almost all of it is trapped in the thin layers of Brown shale.

And it's still there in the Appalachian region, over an area of more than 200,000 square miles stretching from New York to Alabama. Natural gas is being produced from it in several places, mainly to both sides of the West Virginia Kentucky border. The total amount of readily recoverable gas is 15 to 25 trillion cf. of the order of the entire present annual US production (19.5 Tcf in 1976). And as always with a resource, there is more at a price.

Curiously, the Brown shale contains not only methane, but also uranium. The reasons are unknown, except that it got there at the time of the deposition, not later. The uranium content is only between 5 and 7 per mille, which is not good enough for commercial exploitation (as yet), but it does have the advantage of indicating the precise location of the Brown shale on gamma-ray logs of drilled wells.



 • The Wonderchild
 • CONSERVING TUSCALOOSA GAS
 • DEVONIAN SHALE
 • GETTING IT OUT
 • ENERGY OR EXTINCTION?
 • THE WAR AGAINST THE AUTOMOBILE
 • AND ABOVE ALL, SOCIAL PRIVILEGES
 • NUCLEAR NOTES
Vol. 5, No. 5

Newsletter: Access to Energy Newsletter Archive
Volume: Volume 5
Issue/No.: Vol. 5, No. 5

Date: January 01, 1978 02:50 PM
Title: The Wonderchild

Copyright © 2004 - Access to Energy Newsletter Archive
All rights reserved.