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Minerals, bonding

Schulten, H.-R. (2002). New approaches to the molecular structure and properties of soil organic matter Humic-, xenobiotic-, biological-, and mineral-bonds. In Soil Mineral-Organic Matter-Microorganism Interactions and Ecosystem Health. Developments in Soil Science,Vol. 28A, Violante, A., Huang, P. M., Bollag, J.-M., and Gianfreda, L., eds., Elsevier B. V., Amsterdam, pp. 351-381. [Pg.586]

Hydresol . [BASF AG] Niq)hthalene sulfonic or phenol-sulfonic adds/form-aldehyde condensates plasticizers for mine binders, for itt proving workability of mineral-bond mortar and ctmcrete. [Pg.176]

When the electric field of the radiation interacts with the electron cloud of the mineral bond, it induces a dipole moment m in that bond that is given by... [Pg.450]

The oxidation of simple internal alkenes is very slow. The clean selectiv oxidation of a terminal double bond in 40, even in the presence of an internt double bond, is possible under normal conditions[89,90]. The oxidation c cyclic alkenes is difficult, but can be carried out under selected condition Addition of strong mineral acids such as HCIO4, H2S04 and HBF4 accelerate the oxidation of cyclohexene and cyclopentene[48,91], A catalyst system 0 PdSO4-H3PM06W6Oii(j [92] or PdCF-CuCF m EtOH is used for the oxidatioi of cyclopentene and cyclohexene[93]. [Pg.28]

Adsorption Mechanisms. The following mechanisms of adsorption are responsible for the formation of mineral—reagent bonds. [Pg.48]

Hydrogen Bond Formation. This faciUtates adsorption if the mineral and the adsorbate have any of the highly electronegative elements S,0,N,F, and hydrogen. A weak (physical) bond is estabflshed between the sohd wall and the reagent through the alignment of the cited elements. [Pg.48]

Chemical Bond Formation (Chemisorption). This is the mechanism that leads to the formation of the strongest bonds between coUectors and mineral surfaces. Chemically adsorbed reagents usuaUy form surface compounds at the active waU sites. The flotation of calcite (CaCO ) and... [Pg.48]

Table 1 Hsts some of the physical properties of duoroboric acid. It is a strong acid in water, equal to most mineral acids in strength and has a p p o of —4.9 as compared to —4.3 for nitric acid (9). The duoroborate ion contains a neady tetrahedral boron atom with almost equidistant B—F bonds in the sohd state. Although lattice effects and hydrogen bonding distort the ion, the average B—F distance is 0.138 nm the F—B—F angles are neady the theoretical 109° (10,11). Raman spectra on molten, ie, Hquid NaBF agree with the symmetrical tetrahedral stmcture (12). Table 1 Hsts some of the physical properties of duoroboric acid. It is a strong acid in water, equal to most mineral acids in strength and has a p p o of —4.9 as compared to —4.3 for nitric acid (9). The duoroborate ion contains a neady tetrahedral boron atom with almost equidistant B—F bonds in the sohd state. Although lattice effects and hydrogen bonding distort the ion, the average B—F distance is 0.138 nm the F—B—F angles are neady the theoretical 109° (10,11). Raman spectra on molten, ie, Hquid NaBF agree with the symmetrical tetrahedral stmcture (12).
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.
Elemental composition, ionic charge, and oxidation state are the dominant considerations in inorganic nomenclature. Coimectivity, ie, which atoms are linked by bonds to which other atoms, has not generally been considered to be important, and indeed, in some types of compounds, such as cluster compounds, it caimot be appHed unambiguously. However, when it is necessary to indicate coimectivity, itaUcized symbols for the connected atoms are used, as in trioxodinitrate(A/,A/), O2N—NO . The nomenclature that has been presented appHes to isolated molecules (or ions). Eor substances in the soHd state, which may have more than one crystal stmcture, with individual connectivities, two devices are used. The name of a mineral that exemplifies a particular crystal stmcture, eg, mtile or perovskite, may be appended. Alternatively, the crystal stmcture symmetry, eg, rhombic or triclinic, may be cited, or the stmcture may be stated in a phrase, eg, face-centered cubic. [Pg.117]

The second largest use at 21% is for unsaturated polyester resins, which are the products of polycondensation reactions between molar equivalents of certain dicarboxyhc acids or thek anhydrides and glycols. One component, usually the diacid or anhydride, must be unsaturated. A vinyl monomer, usually styrene, is a diluent which later serves to fully cross-link the unsaturated portion of the polycondensate when a catalyst, usually a peroxide, is added. The diacids or anhydrides are usually phthahc anhydride, isophthahc acid, and maleic anhydride. Maleic anhydride provides the unsaturated bonds. The exact composition is adjusted to obtain the requked performance. Resins based on phthahc anhydride are used in boat hulls, tubs and spas, constmction, and synthetic marble surfaces. In most cases, the resins contain mineral or glass fibers that provide the requked stmctural strength. The market for the resins tends to be cychcal because products made from them sell far better in good economic times (see Polyesters,unsaturated). [Pg.485]


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See also in sourсe #XX -- [ Pg.404 ]




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APPLICATION OF BONDING MODELS TO SULFIDE MINERALS

Bonding studies of minerals

Chemical bonding studies of minerals

Mineral matter hydrogen bonding

Minerals, bonding complexes

Minerals, bonding interactions

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