how exactly do "fossils" make "fuel" - jerome corsi ph.d

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  • 8/14/2019 How exactly do "fossils" make "fuel" - Jerome Corsi Ph.D

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    w exactly do 'fossils'
    make 'fuel'? http://www.worldnetdaily.com/news/article.asp?ARTICLE_ID=47448

    4 18/5/2008 19:0

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    How exactly do 'fossils'make 'fuel'?

    Posted: November 17, 2005

    1:00 am Eastern

    By Jerome R. Corsi 2008 WorldNetDaily.com

    Editor's note: Craig Smith and Jerome Corsi will be on Gordon Liddys

    show today at 11:00 a.m., EST.

    Let's examine closely the alleged chemical processes by which decaying

    plants and dinosaurs are supposed to decay into "fossil fuel."

    Richard Heinberg, one of the core faculty of New College of California

    (Santa Rosa) the "peak-production" adherent who is author of

    "Powerdown: Options and Actions for a Post-Carbon World" tells us that

    "the assertion that all oil is abiotic requires extraordinary support,

    because it must overcome abundant evidence" that ties "specific oil

    accumulations to specific biological origins through a chain of

    well-understood processes that have been demonstrated, in principle,under laboratory conditions." So, if what Heinberg asserts is true, we

    should have no problem discovering the precise laboratory-proven

    formula under which ancient plant and animal life decay into

    hydrocarbon fuel.

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    Seppo Korpela, of the Ohio State University Department of Mechanical

    Engineering, gives us a precise description of the chemical process

    involved. He argues that fossil fuels form when "the early sedimentary

    layers" at the bottom of a basin are deprived of oxygen such that the

    organic matter in them did not decay, "as it does in the common setting

    of kitchen compost." Then, "anaerobic bacteria" can "go to work andturn the organic material into the substance kerogen. Kerogen can be

    thought of as immature oil." The term "anaerobic" refers to a process

    occurring in the absence of oxygen. When kerogen is found at depths of

    between 6,000 and 13,000 feet, and when the temperature and pressure

    are "right," the kerogen "in the source rock will be cracked into oil. This

    zone is called the oil window. At depths greater than 13,000 ft.

    temperatures are so high that oil is cracked into gas."

    Kerogen, it turns out, is not a chemist's term. Kerogen is a loose,

    geological term (deriving from the ancient Greek word keros, meaning

    wax) that an industry oil glossary defines as follows:

    Kerogen. The naturally occurring, solid, insoluble organic

    material that occurs in source rocks and can yield oil upon

    heating.

    Webster's Dictionary defines kerogen in a somewhat circular fashion:

    "bituminous material occurring in shale and yielding oil when heated."

    Yet, Webster's defines bitumen as "any of various mixtures of

    hydrocarbons (as tar) often together with their nonmetallic derivatives

    that occur naturally or are obtained as residues after heat-refining

    naturally occurring substances (as petroleum)." Kerogen is not a term

    typically found in chemistry textbooks or specifically used by

    professional chemists. Use of the term kerogen is generally a signal that

    you are dealing with a petroleum geologist or engineer, not a chemical

    scientist.

    Ker Than, a staff writer for LiveScience.com, provides the common

    sense explanation for how kerogen is supposed to transform into "fossil

    fuel."

    In the leading theory, dead organic material accumulateson the bottom of oceans, riverbeds or swamps, mixing with

    mud and sand. Over time, more sediment piles on top and

    the resulting heat and pressure transforms the organic layer

    into a dark and waxy substance known as kerogen.

    Left alone, the kerogen molecules eventually crack,

    breaking into shorter and lighter molecules composed

    almost solely of carbon andhydrogen atoms. Depending onhow liquid or gaseous this mixture is, it will turn into either

    petroleum or natural gas.

    Chemical textbooks typically do not provide chemical formulae for

    kerogen. What we do find in chemical textbooks are many descriptions

    of how hydrocarbons form when carbon and hydrogen atoms bond toeach other by the covalent bonds. So methane is CH4, the first member

    of what becomes an alkane series, such that members having two-,

    three-, and four-carbon atoms are ethane, propane and butane,

    respectively. We have yet to find a chemistry textbook that refers to

    "kerogen" or describes any combination of ancient algae, tiny Mesozoic

    sea animals, or dinosaurs as necessary or sufficient ingredients in theformation of common saturated hydrocarbons such as methane, ethane,

    propane or butane. Methane is also commonly found on planets such as

    Saturn (and its moon Titan) where science has never recorded the

    presence of living plants or animals.

    Sometimes chemistry textbooks revert to the common wisdom and

    provide a loose verbal description of "natural gas" as having been

    formed by "the anaerobic decay of plants and animals" (as we notedbefore, "anaerobic" refers to a process occurring in the absence of

    oxygen). The textbooks, however, fail to reference any laboratory

    experiment where this process has been demonstrated.

    The transformation from "kerogen" to "fossil fuels" appears to be more a

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    matter of faith, rather than an observed process that can be described in

    a precise chemical formula such that we can replicate in a laboratory the

    process by which the compound is produced. This is a common

    complaint of scientists who propose the abiotic, deep-earth theory of the

    origin of oil. Astronomer Thomas Gold, stated the point succinctly on

    page 85 of his 1998 book, "The Deep Hot Biosphere: The Myth of Fossil

    Fuels." "Nobody has yet synthesized crude oil or coal in the lab from a

    beaker of algae or ferns."

    Published scientific analyses attempting to describe "the notion of

    kinetic cracking of kerogen into petroleum" tend to start with thefundamental definitional problem. Consider this example:

    It is important to keep in mind that the name kerogen, in

    opposition with usual chemical nomenclature, does not

    represent a substance with a given chemical composition.

    Indeed kerogen is a generic name, in the same sense as

    lipids or proteins.

    The resulting theoretical discussions, while generally elaborate, typically

    remain unspecified in rigorous chemical formulae that identify chemical

    transformation processes. These technical discussions of how kerogen

    produces oil from source rock generally end up describing field-oven

    heating devices typically designed to analyze rock samples, such as the

    Rock-Eval prolysis device, into which geologists can cook "source rock"

    in the field to see if the specimen rock looks like other "source rock"

    where oil has already been found. Again, the result is practical field

    geology, not rigorous laboratory science specifying chemical formulae

    identifying how flora and protoplasm turn into hydrocarbons.

    In sharp contrast, methane has been synthetically produced in a rigorous

    laboratory setting with a full specification of the chemical formulae

    involved in the combination of iron oxide, calcium carbonate, and water

    to produce methane at pressure conditions of the Earth's upper mantle.The scientists conducting the experiment concluded:

    The observation of methane formation at mantle pressures

    is significant because it demonstrates the existence ofabiogenic pathways for the formation of hydrocarbons in

    the Earth's interior and suggests that the hydrocarbon

    budget of the bulk Earth may be larger than conventionally

    assumed.

    Scientists have also recently analyzed spectrographic data validating the

    formation of methane on Mars by fluid-rock interaction in the crust, with

    no evidence of biologic or organic processes involved.

    Scientists proposing the abiotic theory of oil have argued that the

    "Fossil-Fuel" theory fundamentally violates the second law of

    thermodynamics, a principle which specifies that energy disperses when

    permitted, such that the energy flow never reverses. For example,

    consider that when you release the neck of a balloon the air escapes; theair never naturally rushes to concentrate into a balloon without being

    forced to do so. Thomas Gold stated the principle on page 46 of his 1998

    book:

    It would be surprising indeed if the Earth had obtained its

    hydrocarbons only from a source that biology had taken

    from another carbon-bearing gas carbon dioxide which

    would have been collected from the atmosphere by

    photo-synthesizing organisms for manufacture into

    carbohydrates and then somehow reworked by geology into

    hydrocarbons.

    In other words, the "fossil fuel" from ancient flora or protoplasm would

    demand that somehow the air went back into the balloon, a reverseflow-of-energy direction contrary to the second law of thermodynamics.

    In other words, dead dinosaurs and ancient forests follow naturally the

    law of entropy, "dust into dust," not the re-energized "fossil fuel" notion

    of "dust into oil." We still lack the laboratory demonstrations authors

    such as Richard Heinberg claimed we would find. Has anyone ever

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    w exactly do 'fossils'
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    taken a flask of downed flora or dead protoplasm and produced a

    hydrocarbon fuel out of the mixture, or is this a process for alchemy?

    Jerome R. Corsi is a staff reporter for WND. He received a Ph.D.

    from Harvard University in political science in 1972 and has

    written many books and articles, including his latest best-seller,"The Late Great USA." Corsi co-authored with John O'Neill the No.

    1 New York Times best-seller, "Unfit for Command: Swift Boat

    Veterans Speak Out Against John Kerry." Other books include

    "Showdown with Nuclear Iran," "Black Gold Stranglehold: The

    Myth of Scarcity and the Politics of Oil," which he co-authored with

    WND columnist Craig. R. Smith, and "Atomic Iran."

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