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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]

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]

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]

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]

There are many other benefits of pluralism, some of which have already been discussed in detail by Hasok Chang (2012, chap. 5.2) or mentioned before. First of all, if we acknowledge that biology, physics, chemistry, geology and so on (as well as correspondingly their various research fields) have different subject matter and different research aims that require different methods, it is obvious that monism can pick only a single aspect and disregard the rest. Pluralism instead allows a non-hierarchical division of labor, which in most fields of society is the most effective and successful approach. Moreover, as new kinds of issues arise, either out of the research process or by societal demand, science can flexibly adjust by... [Pg.69]

In this way, music restricted the possibilities of speech. Physics shaped speech in other ways, too. Sound waves are shaped by the physics of the atmosphere, so high-altitude languages have more ejective consonants that chck loudly in dry air. (This is either to make the sound carry farther or to minimize water loss.) When the sound waves hit another human s ear and are transmitted to the brain, the shapes of the brain waves match the shapes of the sound waves. Even the letters used to represent the words, in all languages, match natural shapes in the environment, which are themselves formed by chemistry, geology, and biology. [Pg.243]

Mankind, or I should say, the western scientists have invented the disciplines biology, chemistry, geology, and physics, etc. Nature does not concern herself with its subdivisions imposed by us. Nature is a whole we scientists in a discipline look at only certain aspects of it or only from a certain viewpoint. However, there is an increasing realization of the need to understand the nature as a whole, because everything is related to everything else as seen in environmental issues, for example (see Chap. 22). Thus, we see more and more interdisciplinary endeavors. And all these disciplines deal with materials, and materials are chemicals, and thus chemistry permeates all these other disciplines. Hence, chemistry is often called the Central Science T... [Pg.221]

Kennish, M. J., ed. 2001. Practical Handbook of Marine Science, 3rd ed. Boca Raton, FL CRC Press. This handbook contains information on physical oceanography, marine biology, marine chemistry, geology, and pollution. It contains over 800 tables and figures. [Pg.144]

J.S. Turner, editors, in Proceedings of the NATO Conference on Instabilities in Chemistry, Geology, and Materials Science, Austin, Texas IT983)(in press). [Pg.98]

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]

We assume that our readers have a background in science attainable by completing a university level course in introductory chemistry. We also expect our readers to be involved in one of the disciplines integral to the study of biogeochemical cycles. This includes appropriate subdisciplines of chemistry, biology, and geology, and the sciences that deal with soils, atmospheres, and oceans. [Pg.551]

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]

Chemists use many different liquid solvents, but we focus most of our attention on water. When water Is the solvent, the solution Is said to be aqueous. A rich array of chemistry occurs in aqueous solution, including many geological and biochemical processes. Aqueous solutions dominate the chemistry of the Earth and the biosphere. The oceans, for instance, are rich broths of various cations and anions, sodium and chloride being the most abundant. The oceans can be thought of as huge aqueous solvent vessels for the remarkably complex chemistry of our world. Blood is an... [Pg.169]

After a consideration of optical transitions in which MMCT plays a role, and after a characterization of the excited states involved, a short review of mixed-valence compounds and their spectroscopy is in order. For more extended reviews we refer to Refs. [60,97], At least 40 elements of the periodic table form mixed-valence species which are of importance in solid state physics and chemistry, inorganic chemistry, materials science, geology and bioinorganic chemistry. It is usually their colors which are their most striking property (see also above), but they have more intriguing properties, for example electrical and magnetic properties. [Pg.175]

The second major component of the education of a modern materials chemist in materials synthesis is, of course, in phase equilibria, possibly through the treatment of quaternary systems and P—T—X (pressure—temperature—composition) equilibria. This subject was essentially eliminated from chemistry departments and is taught in the materials and geological science departments. Every student (and professor) aspiring to be a materials chemist will have to master this subject. [Pg.60]

Injection/Confining-Zone Lithology and Chemistry provides information on the geology and chemistry of the injection zone formation fluids. [Pg.836]

The injection well is in the same area as the Monsanto well, so the geology and native water chemistry are very similar to that described before. Figure 20.13 shows the stratigraphy of the immediate area... [Pg.841]


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