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Pap. 1350, 781–790 (1987). Surtsey, Iceland: Averages of samples collected Oct. 15, 1964, 21. Feb. 1965, 31 Mar. , G. Elisson, Geochim. Cosmochim. M. J. Volcanol. Geotherm. Res. 8, 191–198 (1980). Mt. , Philos. Trans. R. Soc. Lond. , J. Volcanol. Geotherm. Res. 6, 165–178 (1979). , F. Le Guern, Geochim. Cosmochim. , J. Volcanol. Geotherm. Res. 7, 415–441 (1980). M. M. Nohl, J. Volcanol. Geotherm. Res. 14, 223–245 (1982). St. Helens, USA: Fumarole on N40°W radial fissure, average of four samples obtained on 27.
K. 7 The Biosphere 39 UNESCO, World Water Balance and Water Resources of the Earth. Studies and Report in Hydrology, No. 7 The Biosphere The biosphere, which encompasses all forms of life present on the globe, generally is taken to include all living organisms as well as dead (and decaying) organic material. The biosphere owes its existence largely to the energy captured from sunlight by organisms that make use of the photosynthetic process to combine carbon dioxide and water to form organic material.
16 a Formula expressions indicate the dependence on temperature and pressure. 01325 × 105 Pa) b cp – cv = Rg/Mdry air c The quantity is essentially independent of pressure. 4 (K) (Sutherland constant). 0370b a Data source: (a) Glueckauf (1951); the CO2 content was extrapolated from the data reviewed by Callendar (1940) and did not correspond to the true value at that time. 002%), and the further removal of nitrogen to obtain the fraction of argon (the predominant rare gas). Other rare gases were determined by mass spectrometry in the non-condensable fraction of liquefied air.