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Recent advances in accelerator technology have reduced the cost and size of an RBS instrument to equal to or less than many other analytical instruments, and the development of dedicated RBS systems has resulted in increasing application of the technique, especially in industry, to areas of materials science, chemistry, geology, and biology, and also in the realm of particle physics. However, due to its historical segregation into physics rather than analytical chemistry, RBS still is not as readily available as some other techniques and is often overlooked as an analytical tool. [Pg.477]

Fig. 9-3 Conceptual model to describe the interaction between chemical weathering of bedrock and down-slope transport of solid erosion products. It is assumed that chemical weathering is required to generate loose solid erosion products of the bedrock. Solid curve portrays a hypothetical relationship between soil thickness and rate of chemical weathering of bedrock. Dotted lines correspond to different potential transport capacities. Low potential transport capacity is expected on a flat terrain, whereas high transport is expected on steep terrain. For moderate capacity, C and F are equilibrium points. (Modified with permission from R. F. Stallard, River chemistry, geology, geomorphology, and soils in the Amazon and Orinoco basins. In J. I. Drever, ed. (1985), "The Chemistry of Weathering," D. Reidel Publishing Co., Dordrecht, The Netherlands.)... Fig. 9-3 Conceptual model to describe the interaction between chemical weathering of bedrock and down-slope transport of solid erosion products. It is assumed that chemical weathering is required to generate loose solid erosion products of the bedrock. Solid curve portrays a hypothetical relationship between soil thickness and rate of chemical weathering of bedrock. Dotted lines correspond to different potential transport capacities. Low potential transport capacity is expected on a flat terrain, whereas high transport is expected on steep terrain. For moderate capacity, C and F are equilibrium points. (Modified with permission from R. F. Stallard, River chemistry, geology, geomorphology, and soils in the Amazon and Orinoco basins. In J. I. Drever, ed. (1985), "The Chemistry of Weathering," D. Reidel Publishing Co., Dordrecht, The Netherlands.)...
Stallard, R. F. (1985). River chemistry, geology, geomorphology, and soils in the Amazon and Orinoco basins. In "The Chemistry of Weathering" (J. I. Drever, ed.), pp. 293-316. D. Reidel Publishing Co., Dordrecht, Holland, NATO ASI Series C Mathematical and Physical Sciences 149. [Pg.228]

Pearson, FJ. and Coplen, T.B. 1978 Stable isotope studies of lakes. In Lerman, A., ed., Lakes-Chemistry, Geology, Physics. New York, Springer-Verlag 325-339. [Pg.139]

Eugster, H.P. and Hardie, L.A. "Saline Lakes" chapter 8 of Lakes Chemistry, Geology, Physics, Abraham Lerman ed., Springer-Verlag, New York, 1978. [Pg.346]

He was the thirteenth child of a Stockholm merchant. After graduating from the University of Upsala in 1863, he studied for a time in C.-A. Wurtz s laboratory in Paris, and in 1874 he became a professor at Upsala. True lover of Nature that he was, he could never confine his activities closely to one branch of science, but was interested alike in chemistry, geology, botany, and hydrography. He wrote his scientific papers in a lucid, pleasing style, and also produced literature of esthetic value (14). [Pg.710]

A. G. Wedd, in Sulfur Its Significance in Chemistry, Geology, Biology, Cosmology and Technology , Stud. Inorg. Chem., 1984, 5, 81. [Pg.1414]

Jones, B.F. and Bowser, C.J. (1978) The mineralogy and related chemistry of lake sediments. In Takes, Chemistry, Geology and Physics (ed. Lerman, A.). Springer-Verlag, Berlin, pp. 179-235. [Pg.225]

Eugster, h. p. Hardie, l. A. in Lakes--chemistry, geology, physics Lerman, A. Ed. Springer-Verlag New York, 1978 pp 237-294. [Pg.152]

Unlike laboratory chemistry, geological chemistry occurs in thermodynamically open systems. That is to say, there is flagrant exchange of materials and energy between the system and the environment Not only is the system as a whole not isolated from the environment, but the materials of interest are rarely isolated from each other. To further the complexity, interaction of mineral catalysts with those forms of energy most likely to affect surface-mediated reactions has barely been characterized in model systems. [Pg.5]

Oceanography, the study of the oceans, is a combination of the sciences of biology, chemistry, geology, physics, and meteorology. [Pg.639]

At the turn of the 19 and 20 centuries, the visible frontiers between the traditional natural sciences like chemistry, geology, and biology showed a tendency to carry out new interdisciplinary research and to create new sciences. The genetic soil science that has arisen in the 1880s in Russia was in fact a precursor to the said tendency. [Pg.6]

Imboden, D. M., and A. Lerman (1978), Chemical Models of Lakes, in A. Lerman, Ed., Lakes Chemistry, Geology, Physics, Springer, New York. [Pg.41]

Alkali and Alkaline Earth Metals presents the current scientific understanding of the physics, chemistry, geology, and biology of these two families of elements, including how they are synthesized in the universe, when and how they were discovered, and where they are found on Earth. The book also details how humans use alkalis and alkaline earths and the resulting benefits and challenges to society, health, and the environment. [Pg.14]

Stumm, W. Baccini, P. (1978) Man-made chemical perturbation of lakes. In Lakes - Chemistry, Geology, Physics, ed. A. Lerman, pp. 91-126. New York Springer-Verlag. [Pg.26]


See other pages where Chemistry geological is mentioned: [Pg.343]    [Pg.478]    [Pg.427]    [Pg.431]    [Pg.59]    [Pg.73]    [Pg.406]    [Pg.25]    [Pg.29]    [Pg.568]    [Pg.311]    [Pg.415]    [Pg.228]    [Pg.181]    [Pg.335]    [Pg.283]    [Pg.389]    [Pg.483]    [Pg.2674]    [Pg.114]    [Pg.149]    [Pg.492]    [Pg.10]    [Pg.238]    [Pg.307]    [Pg.403]   


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