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Oxygen diamond

FIGURE 10.9 Structure of HgBa2Ca2Cu308, depicting copper oxygen diamonds between the Ca layers and the copper oxygen layers forming the bases of the pyramids. The apices of the pyramids are in the harium oxygen layers. In the superconductor... [Pg.406]

FIGURE 10.8 The structure of 1-2-3 (a) the metal positions (c) idealized structure of YBa2Cu307-T (d) the extended structure of YBa2Cu307, depicting copper-oxygen planes, with the copper-oxygen diamonds in between. Key Cu, blue Ba, green Y, aqua 0, red. [Pg.416]

We have previously shown that Ir-loaded TiOz exhibited excellent catalytic activity without carbon deposition in a prolonged run [3]. The reaction was proposed to proceed through a two-step process, that is complete oxidation of methane to give CO2 and HzO, followed by reforming reactions. At a lower temperature of 600 C, Ni-AlzOz catalyst is not active. The use of oxidized diamond-supported catalyst was examined under oxidative conditions. Diamond is believed to be inert to chemical reactions. However, in the presence of oxygen diamond can be oxidized to carbon dioxide. If the oxidized diamond support could be utilized under oxidative conditions, application of diamond support could be expanded to many catalytic reactions. [Pg.1077]

Fig. 15.16 Measurements and results of a model calculation performed with CoTReM applying to the upper centimeters of a sediment core from equatorial West Africa (GeoB4906, 1251 m water depth) (after Pfeifer et al. 2002). The symbols in the left diagram represent measured values of pore-water concentrations (circles oxygen, diamonds nitrate, triangles manganese, squares iron, crosses sulfate). The unbroken lines denote the concentrations calculated by the model. The right diagram illustrates the assumed (bio)geochemical reactions which take place in various depths and display dissimilar turnover rates. (OM Organic matter). Fig. 15.16 Measurements and results of a model calculation performed with CoTReM applying to the upper centimeters of a sediment core from equatorial West Africa (GeoB4906, 1251 m water depth) (after Pfeifer et al. 2002). The symbols in the left diagram represent measured values of pore-water concentrations (circles oxygen, diamonds nitrate, triangles manganese, squares iron, crosses sulfate). The unbroken lines denote the concentrations calculated by the model. The right diagram illustrates the assumed (bio)geochemical reactions which take place in various depths and display dissimilar turnover rates. (OM Organic matter).
HK (HMIO) Type 1 contains 0.1 -0.2% N, type 11a is N-free, and type lib is very pure, generally blue in color. Electrical insulator (Eg = 7 eV). Burns in oxygen. Diamond... [Pg.461]

An oxygen diamond may be used for shipment of oxygen in the United States in place of the nonflammable gas and oxi-... [Pg.170]

W.E. Pickett, Negative electron-affinity and low work function surface cesium on oxygenated diamond(lOO). Phys. Rev. Lett. 73(12), 1664-1667 (1994)... [Pg.175]

Fig. 10.5. C Is core level XPS spectra for oxygenated diamond electrodes. Deconvoluted peaks are also depicted. Fig. 10.5. C Is core level XPS spectra for oxygenated diamond electrodes. Deconvoluted peaks are also depicted.
On the other hand, electrostatic attraction between carboxyl groups and positively charged redox species [Ru(NH3)e]2+ 3+ should increase with increasing pH. In fact, the redox behavior for these at GC depends on pH, and this effect is an example of the Frumkin effect [10]. However, the rate constants for redox reactions at oxygenated diamond electrodes do not obey the Frumkin effect (Fig. [Pg.227]

Therefore, it is supposed that there is a negligible amount of carboxyl groups on oxygenated diamond electrodes. [Pg.228]

Fig. 10.8. N Is core level spectra of XPS for DNPH-treated and untreated oxygenated diamond electrodes. Fig. 10.8. N Is core level spectra of XPS for DNPH-treated and untreated oxygenated diamond electrodes.

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See also in sourсe #XX -- [ Pg.170 ]




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