re: atmospheres

From: Keenan.Dungey@furman.edu
Date: Fri Apr 28 2000 - 14:14:33 EDT

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    Consulting my environmental chemistry textbook (_Chemistry of the
    Environment_, Thomas G. Spiro and William M. Stigliani, Prentice Hall: New
    Jersey (1996)) I found a more recent reference to the carbon cycle which
    answers three of your four questions. p. 127 has a figure from NASA and J.
    T. Houghton et al., eds. (1990). _Climate Change: The IPCC Scientific
    Assessment_ (Cambridge, UK: Cambridge University Press). If I'm reading
    the figure correctly, the answers to your questions are (a Tg is 10^12 g):

              amt C (10^3 Tg) annual change (10^3 Tg)
    atmosphere 740 3
    land biomass 550 2
    soil 1500
    fossil fuels 10000
    ocean surface 1000 2
    ocean biomass 3
    deep waters 38000

    The concentration of CO2 in air at ground level is approx. 350 ppm (parts
    per million) (p. 119). This varies seasonally with plant respiration (p.
    126). Humans are contributing the the concentration of CO2 in the
    atmosphere through combustion of fossil fuels and deforestation at a rate
    of 0.5 - 1 ppm/yr.

    BTW, there was an excellent NOVA/Frontline two hour special on global
    warming on PBS a couple of weeks ago. The video is available for purchase
    on their web site, pbs.org.

    To start to answer your fourth question, the concentration of CO2 and CH4
    in the earth's part atmosphere has been estimated from Antarctic ice cores
    (p. 130 and Houghton ref.)

    I hope this helps.

    Keenan

    ----Original Message-----
    Date: Thu, 27 Apr 2000 05:36:29 -0000
    From: "glenn morton" <mortongr@flash.net>
    Subject: Re: Atmospheres

    - ----- Original Message -----
    From: "Stein A. Stromme" <stromme@mi.uib.no>
    To: "glenn morton" <mortongr@flash.net>
    Cc: <asa@calvin.edu>
    Sent: Thursday, April 27, 2000 6:34 AM
    Subject: Re: Atmospheres

    > [glenn morton]
    >
    > | I have been doing some research into the composition of the ancient
    > | atmospheres.
    >
    > Glenn, as always, your posts are very interesting. In particular, I
    > take the opportunity to thank you for the Waco conference notes.
    >
    > Perhaps you (or someone else on the list) know answers to the
    > following questions about the carbon cycle:
    >
    > How much carbon is there on earth? How is it distributed between CO2
    > in atmosphere and oceans, biomass in ocean and on land, fossil fuels,
    > and other forms? Can one quantify the fluctuations and flows between
    > these forms? And, as your expressed interest above indicates, the
    > history?

    While kind of old, there is an article on the carbon cycle in the Sept.
    1970
    Scientific American.

    As to the distribution of carbon in the biosphere this also is an old
    source
    I have. The main change to this over the years is the discovery of bacteria
    deep in the earth whose mass might outweigh that of above ground life. I
    can't find it right now but I think there are 10-100 times more living
    matter in bacteria below the ground than above. This would multiply the
    living things category by that amount.

    petroleum nonreservoir 200 x 10^18 g carbon
    Petroleum reservoir 1 x 10^18 g carbon
    Coal 15 x 10^18 g carbon
    Carbonate rocks 51,000 x 10^18 g carbon
    living things .3 x 10^18 g carbon
    J.M. Hunt, "Distribution of Carbon in Crust of Earth," Bull. AAPG, Nov.
    1972, p. 2273-2277. p.2274



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