Posted on 05/29/2002 8:18:56 AM PDT by jimkress
Edited on 05/25/2004 3:03:02 PM PDT by Jim Robinson. [history]
On the subject of the interesting Thomas Gold, I recall reading of his early concerns that the lunar surface might consist of electrostatically charged dust lcking sufficient strength to support the landings of spacecraft. It was his only hypothesis to have later been conclusively disproven.
"INTERNATIONAL-BANKERS"
m
Supplies of oil may be inexhaustible
REALLY???????.....
Ask the small, "mom & pop" INDEPENDENT dealership 'owners', of the 1950's, 60's, 70's, 80's,.........
and,...."NONE" in the 90's!!!!!!!!
Follow the (their) $$$$...MONEY...$$$$
So: How did the "oil-productive" plants get 10,000 to 15,000 feet deep? How did they get under the sea beds in such wide areas - when many of these regions are on "stable" continental shelves; not getting shalloer or deeper since the Cambrian days.
If the coal beds came from the earliest Cambrian era swamps (and of course fossiles and plant matter in the coal prove dates very accurately).... where/when did the "plants/microbes/methane (?) that formed the oil fields come from ..... how did it get so deep?
So - If coal (under natural conditions) is to mimic this process: Then there must be a continuos, massive source of free hydrogen molecules passing through over and around the coal .... not just a little bit either: but enough to so that at least two H atoms (not as gassous H2 either!) are present for each C atom.
Result, of course, is going to depnd on what liquids and what light gasses form: methane, ethane, ethanols, etc. would all result from different numbers of free H atoms available to react. But if free H atoms are present ... why atay near the coal bed? Wouldn't you expect them to float away?
Perhaps the surface "pre-coal" swamps DID have the hydrogen float away ... and ONLY the extremely deep deposits were "captured" under enough rock to trap enough hydrogen to react with the pro-coal molecules under enough pressure. ?
I wouldn't hold my breath waiting for oil to magically reappear in most oil reservoirs.
While organic matter in shales may be currently undergoing diagenisis to form oil, most reservoirs I am familiar with have not exhibited any sort of rapid fillup after depletion. There may be isolated examples where a reservoir is receiving spilloff from another oil reservoir below or maybe even a few cases where enough oil is migrating from huge nearby shale beds to replenish a small reservoir in a few years or decades.
Oil contains the remnants of biological compounds from the source matter from whence it came. If I remember correctly, chlorophyll remnants are there as porphyrins; remants of flowering plants show up as oleanane, etc., etc. Despite Sinclair's old ads, dinosaurs are not major sources of oil; most of it comes from remains of marine and terrigenous (land) organisms found in shale and some carbonates.
I don't put too much stock in Gold's ideas.
Coal beds are often deposited in lagoons near the ocean and are often found near the shales that produce the oil. Organic matter was deposited in a much more concentrated form in the coals than it was in the shales. Both coal and shale can generate oil with burial, but US coals are generally thought to primarily be gas generators.
In general, the deeper one goes, the hotter it gets and the more pressure in situ fluids come under. Over geologic time, the deposited organic matter (lignins, cell wall material, etc.) breaks down into oil. With additional burial, i.e., hotter temperatures, the oil eventually breaks down into gas. Both can migrate to shallower formations and be trapped there.
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a.cricket
You must live in New England. (Psst, topsoil is washing off uncovering rocks. Sorry to disillusion you.)
:-)
T. Gold VitaThomas Gold
Thomas Gold
Biographical InformationProfessor Emeritus of Astronomy at Cornell University;
founder and for 20 years director of Cornell Center for Radiophysics and Space Research.Fellow, Royal Society (London)
Member, National Academy of Sciences (US)
Member, American Academy of Arts and Sciences
Member, American Philosophical Society
Fellow, American Geophysical Union
Honorary Fellow, Trinity College, Cambridge
Gold Medal, Royal Astronomical Society (UK)
Doctor of Science, Cambridge University
Honorary M.A. Harvard UniversityPrevious employment:
John L. Wetherill Professor of Astronomy, Cornell University; Chairman, Department of Astronomy
Assistant Vice President for Research, Cornell University
Robert Wheeler Willson Professor of Applied Astronomy, Harvard University
Chief Assistant to British Astronomer Royal
Lecturer in advanced physics, Cambridge University
Radar development work, British Admiralty during World War II280 publications in various fields of science, including cosmology, mechanism of mammalian hearing, nature of pulsars as rotating neutron stars, aspects of solar system research, origin of planetary hydrocarbons. For 7 years a member of the President's Space Science Panel (US).
Invited Lectureships:
Vanuxem Lecture, Princeton University
Welch Lecture, University of Toronto
Milne Lecture, Oxford University
George Darwin Lecture, Royal Astronomical Society, London
Lindsay Lecture, National Aeronautics and Space Administration
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