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Oxygen different temperatures

References to a number of other kinetic studies of the decomposition of Ni(HC02)2 have been given [375]. Erofe evet al. [1026] observed that doping altered the rate of reaction of this solid and, from conductivity data, concluded that the initial step involves electron transfer (HCOO- - HCOO +e-). Fox et al. [118], using particles of homogeneous size, showed that both the reaction rate and the shape of a time curves were sensitive to the mean particle diameter. However, since the reported measurements refer to reactions at different temperatures, it is at least possible that some part of the effects described could be temperature effects. Decomposition of nickel formate in oxygen [60] yielded NiO and C02 only the shapes of the a—time curves were comparable in some respects with those for reaction in vacuum and E = 160 15 kJ mole-1. Criado et al. [1031] used the Prout—Tompkins equation [eqn. (9)] in a non-isothermal kinetic analysis of nickel formate decomposition and obtained E = 100 4 kJ mole-1. [Pg.212]

C12-0059. One of the reasons that different aquatic life-forms thrive in water of different temperatures is the variation with temperature in the concentration of dissolved oxygen. Using data in Table 12-2. calculate the percentage change in the equilibrium oxygen concentration when water warms from 0.0 °C to 25.0 °C. [Pg.882]

The reaction was performed over the iron phosphate catalyst by changing the reaction temperature from 180 to 270°C and the amount of catalyst used from 1 to 36 g, while fixing the feed rates of pyruvic anhydride, oxygen, nitrogen, and water at 10.5, 13.4, 350, 480 mmol/h, respectively. The yields of citraconic anhydride obtained at different temperatures are plotted as a function of the conversion of pyruvic acid in Figure 5. And the yields of acetic acid at different temperatures are also plotted in Figure 6. [Pg.206]

Fig. 6IR spectra of the adsorbed species on the cataly.st after the reaction of CH4 with the oxygen species generated in a H2-O2 gas mixture at different temperatures. [Pg.404]

Other authors also determined by FTIR that organic nitrocompounds are formed as primary products of the NO CH4-SCR reaction on ZSM-5-based catalysts [121-124], They preadsorbed nitromethane on the sample placed in the IR cell and followed by IR its transformation into other intermediates under 02 and NO versus time at different temperatures. For Cu- and Co-ZSM-5, it was shown that around 300°C adsorbed nitromethane is easily converted into isocyanates and then melamine via polymerization of the former species. Both species easily interact with molecular oxygen, while no reaction with NO is observed and the reactivity depends on the temperature and the nature of the transition metal cation. [Pg.120]

Figure 5 Chemiluminescence oxidation runs for powder of poly(2,6-dimethyl-l,4-phenylene oxide) at different temperatures, oxygen (logarithmic time scale). Figure 5 Chemiluminescence oxidation runs for powder of poly(2,6-dimethyl-l,4-phenylene oxide) at different temperatures, oxygen (logarithmic time scale).
Being thermally decomposed onto the surface of carbon, this complex is expected to form very small catalytically active NiCo204 spinel centers. Thus, we have studied the catalytic activity of the products of pyrolysis at different temperatures toward two electrochemical reactions -reduction of oxygen in alkaline electrolyte and intercalation of lithium into carbons in aprotic electrolyte of Li-ion battery. To our knowledge, the catalytic effect of the metal complexes in the second reaction was not yet considered in the literature. [Pg.347]

Figure 9.4. Stem-Volmer plot of a fiberoptic oxygen sensor at different temperatures. , 43°C a, 37°C , 31°C , 25°C. The sensing capabilities of the fiberoptic sensor are limited by diffusion processes as suggested by the decreasing value of the lifetimes with increasing temperature. (From Ref. 21 with permission.)... Figure 9.4. Stem-Volmer plot of a fiberoptic oxygen sensor at different temperatures. , 43°C a, 37°C , 31°C , 25°C. The sensing capabilities of the fiberoptic sensor are limited by diffusion processes as suggested by the decreasing value of the lifetimes with increasing temperature. (From Ref. 21 with permission.)...
Significant curvature may be observed in the case of lifetime- (and intensity-) based sensors, mainly when the relation knri [Parameter]) is not linear. Figure 9.4 shows this type of nonlinear behavior for a fiberoptic oxygen sensor. The figure shows Stern-Volmer-type plots (r l versus [02]) at four different temperatures. The curvature is caused by the inability of the carrier to transport oxygen proportionally to the equilibrium partial pressure of oxygen. [Pg.266]

Basically, the fibers grab oxygen molecules from the air so that their atomic binding pattern is reorganized. In the industry, this stage is performed with the use of a number of different techniques. In some cases, the oven is divided into a number of chambers, each with different temperatures the speed at which the fibers enter and exit the chambers can also be controlled depending on the desired characteristics of the fibers [10]. In other methods. [Pg.197]

Free Energies and Nonadditivities (in kcal/mol) of the Cooperativities for Bindii of Oxygen to Human Adult lib at Different Temperatures ... [Pg.214]

Under atmospheric conditions, a low rank coal (0.5-1 mm particle size) from Spain was burned in a fluidized bed reactor at seven different temperatures (50 °C increments) beginning at 650 °C. The combustion experiment was also conducted at different amounts of excess oxygen (5 to 40%) and different flow rates (700 to 1,100 L/h). At 20% excess oxygen and a flow rate of 860 L/h, the amount of acenaphthene emitted ranged from 1,272.4 ng/kg at 650 °C to 6,800.0 ng/kg at 750 °C. The greatest amount of PAHs emitted was observed at 750 °C (Mastral et al., 1999). [Pg.50]

Under atmospheric conditions, a low rank coal (0.5-1 mm particle size) from Spain was burned in a fluidized bed reactor at seven different temperatures (50 °C increments) beginning at 650 °C. The combustion experiment was also conducted at different amounts of excess oxygen (5 to... [Pg.139]

Thus, separate levels of the oceanic crust are simultaneously enriched and depleted in relative to normal mantle values because of reaction with sea water at different temperatures. Muehlenbachs and Clayton (1976) and Gregory and Taylor (1981) concluded that the 0 enrichments are balanced by the depletions which acts like a buffer for the oxygen isotope composition of ocean water. [Pg.115]


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Oxygen different

Oxygen temperatures

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