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Application mineralogy

D.L. Bish and D.W. Ming, Eds., Natural Zeolites Occurrence, Properties, Applications, Mineralogical Society of America and the Geochemical Society, Washington, D.C., 2001. [Pg.10]

Klein and Hurlbut, Manual of Mineralogy (John Wiley Sons, New Yralc, 1983) P. J. Heaney, C. T. Prewitt, and G. V. Gibbs (eds.) Silica. Physical behavior, geochemistry and materials applications (Mineralogical Society of America, Washington D.C., 1994). [Pg.52]

Sylvester, P. (ed.) (2001) Laser-Ablation-ICPMS in the Earth Sciences Principles and Applications, Mineralogical Association of Canada, Ottawa. [Pg.447]

The combination of physical and chemical characteristics of nodules make impossible the application of methods of physical beneficiation such as flotation and magnetic separation to produce concentrates of valuable metals, and so chemical processing must be used. Their processing also tends to be much more energy-intensive, vis-a-vis that of conventional land-based ores. Deep-sea manganese nodules are quite unlike any terrestrial ores, both with respect to their physical characteristics and to their mineralogical and chemical compositions new processes are, therefore, required. [Pg.570]

The technique of DDIF provides a quantitative characterization of the complex pore space of the rocks to supplement conventional mineralogy, chemistry and petrology analyses. A combination of DDIF, Hg intrusion, NMR T2 and image analysis has become the new paradigm to characterize porous rocks for petroleum applications [62, 61]. [Pg.351]

Applications The main application fields of PIXE are earth science, air pollution studies (aerosol analysis), mineralogical studies, forensic science, arts and archaeology. In the external-beam PIXE technique, the proton beam is taken out to ambient air. This mode finds application in the analysis of art objects (paintings, books, etc.). [Pg.642]

On the basis of this comparison study, at present, it is still difficult to adopt a universal selective sequential dissolution procedure, which may be used everywhere and be suitable for all soils with diversified physical, chemical and mineralogical properties. The application of the SSD procedure must consider individual soil characteristics, such as soil type and properties. The two typical SSD procedures were developed to address soils formed in two climates. The Rehovot procedure was developed to be suitable for the calcareous soils in arid and semi-arid zone soils, whereas the Bonn procedure was created to primarily handle the acid and neutral soils in humid zones. In general, the Bonn procedure appears to be unsuited for calcareous soils in arid and semi-arid zones. The Rehovot procedure has limitations in handling acid and neutral soils, especially forest soils with higher content of organic matter. [Pg.122]

Weare, J.H., 1987, Models of mineral solubility in concentrated brines with application to field observations. In I. S.E. Carmichael and H.P Eugster (eds.), Thermodynamic Modeling of Geological Materials Minerals, Fluids and Melts. Reviews in Mineralogy 17,143-176. [Pg.533]

Averill, SA. 2001. The application of heavy indicator mineralogy in mineral exploration with emphasis on base metal indicators in glaciated metamorphic and plutonic terrains. In McClenaghan, M.B., Bobrowsky, P.T. Hall, GE M. Cook, S.J. (eds) Drift Exploration in Glaciated Terrain, Geological Society of London, Special Publication No. 185, 69-81. [Pg.47]

The capability of simultaneous acquisition of X-ray Fluorescence (XRF) spectra has been added. This new instrument, capable of both mineralogical and chemical applications (Klingelhofer et al. 2008) is briefly described and then a few examples of extraterrestrial and terrestrial applications are presented. [Pg.299]

A miniaturized MB spectrometer MIMOS II was developed for the robotic exploration of Mars, where it provided fundamental information about mineralogical composition and alteration processes, helped to classify rocks and soils, aided geologic mapping, was instrumental in assessing habitability of past and present environments, and identified potential construction resources for future human explorers. The applicability of the instrument as a process monitor for oxygen production and prospecting tool for lunar ISRU has been demonstrated. The characterization of air pollution sources and the study of mixed-valence materials as a function of depth in soil are examples of terrestrial in situ applications. MIMOS lla with additional XRF capability will open up new applications. [Pg.301]

Under Lespieau s directorship, the Ecole Normale laboratory was open to students in physics and mineralogy as well as chemistry.33 The primary research program was the synthesis and study of nonsaturated organic compounds, along with the application to hydrocarbons of physical methods like Raoulf s techniques. With his former student, Maurice Bourguel, Lespieau was one of the first people in France to apply Raman spectroscopy to organic analysis.34... [Pg.165]

Chapter 1 is intended to provide an overview of basic concepts of stable isotope geochemistry that are applicable to the chapters that follow on specific topics and isotopic systems. There are a number of excellent reviews of stable isotope geochemistry that have tended to focus on H, C, O, and S, including two prior volumes of Reviews in Mineralogy and... [Pg.1]

High-resolution methods of substanees investigations allow understand not only strueture of those or that material but may be used more mueh widely in application fields. One of them may be mineralogical-geological reconstructions which get possibility to discover new mineral deposits and new natural raw materials [1],... [Pg.523]

Burns, R. G. Mineralogical Applications of Crystal Eield Theory, Cambridge University Press New York, 1970, 1993 p 464. [Pg.294]

Figure 1,17 Absorption spectrum of a forsteritic olivine under polarized light. Ordinate axis represents optical density (relative absorption intensity, ///q). From R. G. Burns (1970), Mineralogical Applications of Crystal Field Theory. Reprinted with the permission of Cambridge University Press. Figure 1,17 Absorption spectrum of a forsteritic olivine under polarized light. Ordinate axis represents optical density (relative absorption intensity, ///q). From R. G. Burns (1970), Mineralogical Applications of Crystal Field Theory. Reprinted with the permission of Cambridge University Press.

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See also in sourсe #XX -- [ Pg.3 , Pg.1421 ]




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