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Trace elements distribution

The book focuses on the biogeochemistry of trace elements in arid and semiarid zone soils and includes an introductory chapter on the nature and properties of arid zone soils. It presents an updated overview and a comprehensive coverage of the major aspects of trace elements and heavy metals that are of most concern in the world s arid and semi-arid soils. These include the content and distribution of trace elements in arid soils, their solution chemistry, their solid-phase chemistry, selective sequential dissolution techniques for trace elements in arid soils, the bioavailability of trace elements, and the pollution and remediation of contaminated arid soils. A comprehensive and focused case study on transfer fluxes of trace elements in Israeli arid and semi-arid soils is presented. The book concludes with a discussion of a quantitative global perspective on anthropogenic interferences in the natural trace elements distributions. The elements discussed in this book include Cd, Cu, Cr, Ni, Pb, Zn, Hg, As, Se, Co, B, Mo and others. This book is an excellent reference for students and professionals in the environmental, ecological, agricultural and geological sciences. [Pg.1]

TRACE ELEMENT DISTRIBUTION IN ARID ZONE SOILS... [Pg.47]

GLOBAL PERSPECTIVES OF ANTHROPOGENIC INTERFERENCES IN THE NATURAL TRACE ELEMENT DISTRIBUTION... [Pg.303]

Greenland, L. P. (1970). An equation for trace element distribution during magmatic crystallization. Amer. Mineral., 55, 455-65. [Pg.530]

Hagen, H. Neumann, E.-R. (1990). Modeling of trace-element distribution in magma chambers using open-system models. Comput. Geosci., 16, 549-56. [Pg.530]

O Nions, R. K. Powell, R. (1977). The thermodynamics of trace-element distribution. In Thermodynamics in Geology, ed. D. G. Fraser, pp. 349-63. Dordrecht Reidel. [Pg.534]

We note that the defect energy contribution associated with extrinsic disorder varies considerably as a function of the partial pressure of oxygen of the system. These energy amounts may significantly affect the intracrystalline disorder, with marked consequences on thermobarometric estimates based on intracrystalline distribution. As we will see in detail in chapter 10, most of the apparent complexities affecting trace element distribution may also be solved by accurate evaluation of the defect state of the phases. [Pg.205]

Figure 10.6 Onuma diagrams for crystal/melt trace element distributions. Ionic radii of Whittaker and Muntus (1970). (A) Augite/matrix distribution, data of Onuma et al. Figure 10.6 Onuma diagrams for crystal/melt trace element distributions. Ionic radii of Whittaker and Muntus (1970). (A) Augite/matrix distribution, data of Onuma et al.
The formulation of this coefficient derives from the consideration that solid/liquid trace element distribution can be ascribed to the existence of simple exchange equilibria of the type... [Pg.681]

Figure 10,9 Effect of normalization on trace element distribution of Sr (A) and Ba (B) between plagioclase and silicate liquid. Distribution curves are based on various experimental evidence (Ewart et al., 1968 Ewart and Taylor, 1969 Berlin and Henderson, 1968 Carmichael and McDonald, 1961 Philpotts and Schnetzler, 1970 Drake and Weill, 1975). Ab albite Or orthoclase An anorthite. Figure 10,9 Effect of normalization on trace element distribution of Sr (A) and Ba (B) between plagioclase and silicate liquid. Distribution curves are based on various experimental evidence (Ewart et al., 1968 Ewart and Taylor, 1969 Berlin and Henderson, 1968 Carmichael and McDonald, 1961 Philpotts and Schnetzler, 1970 Drake and Weill, 1975). Ab albite Or orthoclase An anorthite.
Mason R. A. (1982). Trace element distributions between the perthite phases of alkali feldspars from pegmatites. Min. Mag., 45 101-106. [Pg.843]

Environmental applications of FIFFF have been carefully collected in a review by Gimbert et al. [35]. Separations of nanoparticles belong to the FIFFF tradition and this sector has recently found new, fully deserved impulse for microparticle separations. The FIFFF technique has been applied to analyze humic material and submicron Fe colloids. Coupled with ICP-MS, FIFFF has been applied to detect the major and trace element chemistry of aquatic colloids in groundwaters and to determine the trace element distribution in soil and compost-derived humic and colloidal fractions in municipal wastewater. Recently, the ICP-AES has also been proposed as a specific detector for FIFFF to analyze inorganic nanoparticles (Figure 12.12). [Pg.352]

R. J. Reeder and J. C. Grams, Sector zoning in calcite cement Implications for trace element distributions in carbonates, Geochim. Cosmochim. Acta, 51,1987,187-94... [Pg.235]


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Trace element distribution in arid zone soils

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