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Other Temperature Regimes

Temperature may not always be raised in a linear fashion. In the case of CRT A (Controlled Rate Thermal Analysis), the heating rate is varied in such a manner as to produce a constant rate of mass loss. Alternatively a sinusoidal temperature rise is superimposed on the linear rise this is known as Modulated TG and allows the continuous calculation of activation energy and pre-exponential factor during a run. Sometimes a Temperature Jump (or stepwise isothermal) is used, where temperature is held constant for a time, then jumped rapidly to a higher constant temperature (usually quite close in temperature). All of these procedures are supposed to help in the determination of kinetics of reaction. Another system accelerates the temperature rise when no mass loss is experienced, i.e. between reactions. The rate is slowed to a low value during mass loss. Some manufacturers call this High Resolution TG and an example follows. [Pg.51]


Other temperature regimes can be analyzed in a similar manner, and predictions can be made about the influence on the solids content. Although the values obtained cannot be precise—the form of the phase diagram can only be guessed—the predicted trends are well observed, at least for milk fat, the only fat that has been extensively studied. [Pg.657]

The formation of a layer of metal oxide on the surface of this steel provides better corrosion resistance in oxidizing environments than under reducing conditions. Common steels 304, 304L, 347, 316 and 316L are used for equipment exposed to aqueous solutions of acids and other low-temperature corrosive conditions. For high-temperature regimes involving... [Pg.68]

Fig. 8-5 Soil and soil forming processes - a global view. The moisture and temperature regimes are generalized and intended only to show major pedoclimatic environments. Spodosols, for example, can also occur in a cryic regime and even in equatorial regions. Other orders could also occur in more than one moisture and temperature environment. (overleaf)... Fig. 8-5 Soil and soil forming processes - a global view. The moisture and temperature regimes are generalized and intended only to show major pedoclimatic environments. Spodosols, for example, can also occur in a cryic regime and even in equatorial regions. Other orders could also occur in more than one moisture and temperature environment. (overleaf)...
Fig. 3 A shows the effluent NH3 concentration observed for Ru/MgO as a function of reaction temperature for three different Pn, / Phj / Paf ratios at 20 bar total pressure. It is obvious that the reaction orders for N2 and H2 have opposite signs. Fig. 3B illustrates that the reaction orders for N2 and H2 partly compensate each other in the kineticaliy controlled temperature regime. Hence an increase in total pressure with a constant Pnj / Phj 1/3 ratio does not lead to a significant increase in conversion at lower temperatures. For the plication of alkali-promoted Ru catalysts under industrial synthesis conditions, it is necessary to find a compromise between kinetics and thermodynamics by increasing the Pn, / Phj ratio. The optimum observed for Cs-Ru/MgO prepared from CS2CO3 at 50 bar is at about Pnj / Phj 40 / 60 [15]. The high NH3 concentration of about 8 % obtained with 0.138 g catalyst using a total flow of 100 Nml/min clearly shows that Ru catalysts have indeed the potential to replace Fe-based catalysts in industrial synthesis [15]. Fig. 3 A shows the effluent NH3 concentration observed for Ru/MgO as a function of reaction temperature for three different Pn, / Phj / Paf ratios at 20 bar total pressure. It is obvious that the reaction orders for N2 and H2 have opposite signs. Fig. 3B illustrates that the reaction orders for N2 and H2 partly compensate each other in the kineticaliy controlled temperature regime. Hence an increase in total pressure with a constant Pnj / Phj 1/3 ratio does not lead to a significant increase in conversion at lower temperatures. For the plication of alkali-promoted Ru catalysts under industrial synthesis conditions, it is necessary to find a compromise between kinetics and thermodynamics by increasing the Pn, / Phj ratio. The optimum observed for Cs-Ru/MgO prepared from CS2CO3 at 50 bar is at about Pnj / Phj 40 / 60 [15]. The high NH3 concentration of about 8 % obtained with 0.138 g catalyst using a total flow of 100 Nml/min clearly shows that Ru catalysts have indeed the potential to replace Fe-based catalysts in industrial synthesis [15].
Summary of literature data on methane decomposition catalysts and preferred temperature range. Catalysts 1 = nickel, 2 = iron, 3 = carbon, and 4 = other transition metals (Co, Pd, Pt, Cr, Ru, Mo, W). The dotted line arbitrarily separates heterogeneous (catalytic) and homogeneous (noncatalytic, gas phase) temperature regimes of the methane decomposition reaction. [Pg.75]

The two different temperature regimes of occurring below 7a are separated from each other by a precisely determined crossover temperature T) (denoted by crosses in Fig. 6), which is defined by an inflection point in the product J c(T ) T as a function of T. As discussed later, this crossover or inflection temperature T) appears to conform to the phenomenology of the experimentally estimated mode coupling temperature T p (denoted also as T] ). [Pg.158]

Hydrogenation at 210 K led, as is usual on other metals, to the rapid removal of the (no) species, but a much slower removal of ethylidyne (55). In this temperature regime the gas phase was ethane with a trace of n-butane (55, 32). Condensation of butane may have been responsible for a weak temperature-dependent, methyl-rich spectrum of surface species after hydrogenation at 195 K (32). [Pg.53]

Although experimentally the low temperature regime is well within the experimental reach [1, 2], it has never been addressed theoretically so far. The important question whether the system is a metal or becomes an insulator, in other words, whether the conductivity of the granular metals at large conductances remain finite in the limit of T —> 0 is still open. [Pg.29]


See other pages where Other Temperature Regimes is mentioned: [Pg.51]    [Pg.51]    [Pg.187]    [Pg.126]    [Pg.269]    [Pg.182]    [Pg.35]    [Pg.123]    [Pg.275]    [Pg.413]    [Pg.266]    [Pg.131]    [Pg.319]    [Pg.105]    [Pg.322]    [Pg.3]    [Pg.269]    [Pg.192]    [Pg.232]    [Pg.227]    [Pg.124]    [Pg.478]    [Pg.139]    [Pg.187]    [Pg.436]    [Pg.114]    [Pg.119]    [Pg.131]    [Pg.173]    [Pg.200]    [Pg.204]    [Pg.208]    [Pg.128]    [Pg.257]    [Pg.25]    [Pg.90]    [Pg.138]    [Pg.187]    [Pg.21]    [Pg.307]    [Pg.76]    [Pg.223]   


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Temperature regimes

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