. Carbon and the biosphere; proceedings of the 24th Brookhaven symposium in biology, Upton, , May 16-18, 1972. Carbon cycle (Biogeochemistry). or O h- o < LL I H O cc < h- g 00 1 1 1 1 1 1 1 1 1 1 I I I I I <Nmo/Nao = 1 ' ' 10) <Nmo/Nao = = 2) (Observed fraction) // // — 0 — 1 1 // // 1 / — — 1 1 1 1 1 If — — / — / 04 1 1 // I 1/ 1 1 1 I I I I I I I 20 40 60 80 100 C02 FRACTION, % Fig. 22 Biota growth factor vs. fraction of industrial C02 remaining in the lower atmosphere, for various atmosphere-to-ocean transfer times and ocean- surface-layer sizes. The observed fracti
. Carbon and the biosphere; proceedings of the 24th Brookhaven symposium in biology, Upton, , May 16-18, 1972. Carbon cycle (Biogeochemistry). or O h- o < LL I H O cc < h- g 00 1 1 1 1 1 1 1 1 1 1 I I I I I <Nmo/Nao = 1 ' ' 10) <Nmo/Nao = = 2) (Observed fraction) // // — 0 — 1 1 // // 1 / — — 1 1 1 1 1 If — — / — / 04 1 1 // I 1/ 1 1 1 I I I I I I I 20 40 60 80 100 C02 FRACTION, % Fig. 22 Biota growth factor vs. fraction of industrial C02 remaining in the lower atmosphere, for various atmosphere-to-ocean transfer times and ocean- surface-layer sizes. The observed fraction in 1970 (42%) is indicated by a vertical line in this figure. Atmosphere-to-ocean transfer time: —, 5 years; -, 7 | STANDARD RELATIVE SIZE OF TROPOSPHI E (N lo/Nao» Fig. 23 The underestimate of the fraction of industrial C02 remaining in the lower atmosphere (troposphere) owing to neglect of the finite transfer time between the upper and lower Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Brookhaven National Laboratory; Woodwell, G. M; Pecan, Erene V. [Washington] Technical Information Center, U. S. Atomic Energy Commission; [available from National Technical Information Service, Springfield, Va. ]
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