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Mineralization models

Gaskova, O. L., and M. B. Bukaty. 2008. Sorption of different cations onto clay minerals Modelling approach with ion exchange and surface complexation. Phy. Chem. Earth, Parts A/B/C 33 1050-1055. [Pg.161]

G. McCarthy, W. White, D. Smith, A. Lasaga, R. Ewing, A. Nicol, and R. Roy, ed. R. Roy, Mineral Models for Crystalline Hosts for Radionuclides in Radioactive Waste Disposal, The Waste Package, vol. 1. [Pg.242]

A.A. Alva-Argaez, C. Kokossis and R. Smith, 2007, A conceptual decomposition of MINER models for the design of water-using systems, Int. J. ofEnv. and Pollution, 29(1-3), 177-205. [Pg.48]

Bruun, S., J. Luxhpi, J. Magid, A. de Neergaard, and L. S. Jensen, 2006. A nitrogen mineralization model based on relationships for gross mineralization and immobilization. Soil Biol. Biochem. 38 2712-2721. [Pg.723]

To test the dominance of electrostatic effects in the mineralization model, a mutant of CCMV was constructed (subE) in which all the basic residues on the N-terminus of the coat protein were substituted for glutamic acid (E), thus dramatically altering the electrostatic character of the interior of the assembled protein cage." This mutant was able to catalyze the oxidative hydrolysis of Fe(II) to form an iron oxide nanoparticle encapsulated within the protein cage of the modified virus. High-rcsolution spectral imaging allowed the elemental composition of a protein-mineral composite material to be resolved (1 nm spatial resolution, Fig. 3). This clearly showed that the mineral nanoparticle was completely encapsulated within the protein cage structure. This mutant is able to bind Fe(lT), facilitate its autoxidation... [Pg.1565]

Quantum mechanical calculations view a molecule as a collection of point nuclei and electrons with fixed masses and charges. The energy terms include the kinetic energy of each particle and the coulombic energies between the particles (repulsion between nuclei, attraction between the nucleus and an electron, and repulsion between electrons). Here we will review some basic equations of quantum mechanics to understand quantum mechanical methods, such as Hartree-Fock, semiempirical, and density functional theory methods, that have been most widely used for the clay mineral modeling where simulation size is greater than the molecular cluster with several atoms. [Pg.56]

Table 6. Average concentration of asphaltene solution in pores of mineral model adsorbents. Table 6. Average concentration of asphaltene solution in pores of mineral model adsorbents.
You, F., Grossmann, I. E. (2010). Integrated Multi-echelon supply chain design with inventories under uncertainty MINER models, computational strategies. AIChE Journal, 56, 419 40. [Pg.304]

Fig. 2. Stmcture of the mineral 2eohte chaba2ite is depicted by packing model, left, and skeletal model, right. The sihcon and aluminum atoms He at the corners of the framework depicted by soHd lines. In this figure, and Figure 1, the soHd lines do not depict chemical bonds. Oxygen atoms He near the midpoint of the lines connecting framework corners. Cation sites are shown in three different locations referred to as sites I, II, and III. Fig. 2. Stmcture of the mineral 2eohte chaba2ite is depicted by packing model, left, and skeletal model, right. The sihcon and aluminum atoms He at the corners of the framework depicted by soHd lines. In this figure, and Figure 1, the soHd lines do not depict chemical bonds. Oxygen atoms He near the midpoint of the lines connecting framework corners. Cation sites are shown in three different locations referred to as sites I, II, and III.
Fig. 3. Model of the crystal structure of the mineral mordenite showing the main channel formed by 12-membered ring and small channels which contain some of the sodium cations. Synthetic types of mordenite exhibit the adsorption behavior of a 12-membered ring, whereas the mineral does not, probably... Fig. 3. Model of the crystal structure of the mineral mordenite showing the main channel formed by 12-membered ring and small channels which contain some of the sodium cations. Synthetic types of mordenite exhibit the adsorption behavior of a 12-membered ring, whereas the mineral does not, probably...
Fig. 4. Model of the ciystal structure of zeolites X, Y, and the mineral faujasite. At the tight is shown the tetrahedral arrangement of tmncated octahedra surrounding one large cavity. On the left the packing model of zeohte X is shown, containing three types of Na cations. Fig. 4. Model of the ciystal structure of zeolites X, Y, and the mineral faujasite. At the tight is shown the tetrahedral arrangement of tmncated octahedra surrounding one large cavity. On the left the packing model of zeohte X is shown, containing three types of Na cations.
The Hercules viscometer was originally designed for paper and paperboard coatings, but its use has been extended to paints, adhesives, mineral slurries, emulsions, and starch solutions. The iastmment, noted for being robust and rehable, is particularly well suited for quaUty control and product formulation. It is capable of measuting viscosity over a moderate range 1-10 mPa-s) up to high shear rates (115,000 ). A more recent model is the... [Pg.189]

L. G. Austin, K. R. WeUer, and I. L. Kim, "Phenomenological Modelling of the High Pressure Grinding RoUs," XTTII International Mineral Processing Congress, Sydney, AustraUa, May 1993, pp. 87—95. [Pg.148]

There are numerous synthetic and natural compounds called antioxidants which regulate or block oxidative reactions by quenching free radicals or by preventing free-radical formation. Vitamins A, C, and E and the mineral selenium are common antioxidants occurring naturally in foods (104,105). A broad range of flavonoid or phenoHc compounds have been found to be functional antioxidants in numerous test systems (106—108). The antioxidant properties of tea flavonoids have been characterized using models of chemical and biological oxidation reactions. [Pg.373]

Measuring process parameters on full-scale plants is notoriously difficult, but is needea for control. Usually few of the important variables are accessible to measurement. Recycle of material makes it difficult to isolate the effects of changes to individual process units in the circuit. Newer plants have more instrumentation, including on-line viscosimeters [Kawatra and Eisele, International ]. Mineral Processing, 22, 251-259 (1988)], mineral composition by on-line X-ray fluorescence, belt feeder weighers, etc., but the information is always incomplete. Therefore it is helpful to have models to predict quantities that cannot be measured while measuring those that can. [Pg.1839]

Herbst et al. [International J. Mineral Proce.ssing, 22, 273-296 (1988)] describe the software modules in an optimum controller for a grinding circuit. The process model can be an empirical model as some authors have used. A phenomenological model can give more accurate predictions, and can be extrapolated, for example from pilot-to full-scale apphcation, if scale-up rules are known. Normally the model is a variant of the popiilation balance equations given in the previous section. [Pg.1840]

Figure 4.25. Experimental configuration for optical pyrometry of shock temperatures induced in transparent minerals. Upon impact of projectile with driver plate, a shock wave is driven into the driver plate and then into the sample. Optical radiation from the sample is detected via six lens/interference filter channels and an array of six photodiodes. Signals from photodiode circuits are recorded on oscilloscopes operating in single sweep model. (After Ahrens et al. (1982).)... Figure 4.25. Experimental configuration for optical pyrometry of shock temperatures induced in transparent minerals. Upon impact of projectile with driver plate, a shock wave is driven into the driver plate and then into the sample. Optical radiation from the sample is detected via six lens/interference filter channels and an array of six photodiodes. Signals from photodiode circuits are recorded on oscilloscopes operating in single sweep model. (After Ahrens et al. (1982).)...
Hanna, S. R., Schulman, L. L., Paine, R. J., and Pleim, J. E., "User s Guide to the Offshore and Coastal Dispersion (OCD) Model," DOI/SW/MT-88/007a. Environmental Research Technology, Concord, MA for Minerals Management Service, Reston, VA, 1988. (NTIS Accession Number PB88-182 019.)... [Pg.341]


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Using regional geochemistry, geology, aeromagnetics, Landsat, and digital elevation models (DEM) to define favourable areas for porphyry -style mineralization in southwestern Alaska

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