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Wagner earth

Fig. 5.9 Circuit diagram of a shielded conjugate Schering bridge with a Wagner earth and a guarded specimen holder. Fig. 5.9 Circuit diagram of a shielded conjugate Schering bridge with a Wagner earth and a guarded specimen holder.
Kunstman H, Jung G, Wagner S, Clottey H (2007) Integration of atmospheric sciences and hydrology for the development of decision support systems in sustainable water management. Phys Chem Earth 33 165-174... [Pg.144]

Metals are obtained by the treatment of oxides and sulfide ores found in the earth. However, there is an initial difficulty—the desirable ores are often mixed up with those of little commercial value, and the problem is to obtain the desired ore free from those of lesser worth. For many years now, largely due to the initiative of Australian workers, it has been possible to find organic substances which, when added to a suspension of mixed ores, pick out the desired one, and (when air is bubbled into the system) float it to the surface, from which it can be raked off, i.e., separated and made available for chemical or electrochemical extraction of the metal. It turns out that the basis of this mineral flotation technology involves the Wagner and Traud mixed-potential concept and is thus indirectly related to corrosion theory. [Pg.270]

Powell T. G. (1988) Developments in concepts of hydrocarbon generation from terrestrial organic matter. In Petroleum Resources of China and Related Subjects, Circum-Pacific Council for Energy and Mineral Resources, Earth Science Series (eds. H. C. Wagner, L. C. Wagner, F. F. H. Wang, and F. L. Wong), vol. 10, pp. 807 - 824. [Pg.3684]

SRB are essentially ubiquitous in aqueous environments that contain organic carbon and sulfate (e.g., subsurface aquifers and lake sediments). Moreover, analysis of a key gene associated with sulfate reduction (dissimilatory sulfite reductase) indicates that microbial sulfate reduction is an ancient trait, suggesting that organisms may have contributed to sulfide mineral formation throughout much of Earth history (Wagner et al. 1998). SRB are tolerant to environmental extremes of heat (some are hyperthermophiles) and salinity (some are halophiles). [Pg.10]

Wagner GA, Reimer GM (1972) Fission track tectonics The tectonic interpretation of fission track apatite ages. Earth Planet Sci Lett 14 263-268... [Pg.630]

Perhaps the first Russian scientist to use the term biosphere was E. J. Petty (1854-1899). He used the expression in 1882 and understood it as the totality of all organisms. His pupil D. Koropchevsky (1842-1903) gave the first definition of the bipsphere (in Russia) as a living cover of the Earth based on the works of F. Ratzel and G. Wagner (1840-1923) (Vassoevich, Ivanov, 1977, p. 64). [Pg.28]

Harris GW, Wagner D.A. 1967. Outflow from breached earth dams. Salt Lake City Department of Civil Engineering, University of Utah. [Pg.136]

Wagner SF, Wamke C, Menesklou W, Argirusis C, Damjanovic T, Borchardt G, Ivers-Tiffee E (2006) Enhancement of oxygen surface kinetics of SrXi03 by alkaline earth metal oxides. Solid State Ionics 177 1607... [Pg.75]

Electronic Transport Theory of Liquid Non-Simple and Amorphous Metals, in Proc. 5th Int. Conf. on Liquid and Amorphous Metals, eds C.N.J. Wagner and W.L. Johnson (North-Holland, Amsterdam) pp. 1267-1272. Johansson. B., and N. M4rtensson, 1987, Thermodynamic Aspects of 4f Levels in Metals and Compounds, in Handbook on the Physics and Chemistry of Rare Earths, eds K.A. Gschneidner Jr and L. Eyring (North-Holland, Amsterdam) ch. 69. [Pg.405]


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See also in sourсe #XX -- [ Pg.162 ]




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