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Suspended phase transformation

Suspended phase transformations are those phase conversions that are predicted to take place at a defined Sj-S2-V triple point but do not, owing to some nonideality in the system. One can immediately see that only through the occurrence of a suspended transformation could a metastable polymorph be obtained in the first place. In the case of two solids, slow conversion kinetics can permit the transition point to be exceeded when moving in either direction along the 8,-82 transition curve, permitting the isolation of the otherwise unobtainable metastable phase. [Pg.59]

The sol is made of a stable suspended solution of metal salts or solvated metal precursors containing solid particles of nanometer diameter. Polycondensation or polyesterification results in the appearance of particles in a new phase called the gel . Aging, drying and dehydration are steps required to achieve solid-form ultra-fine particles. Coarsening and phase transformation occur simultaneously with aging. Gel drying is associated with the... [Pg.380]

On the top of the chamber there is a cylindrical extension C which is cooled in order to effect condensation of mercury vapour. Six iron anodes A (there may be twelve or even eighteen of them) are suspended from ring R which covers the top of the chamber. Current for the rectifier is supplied by a three-phase transformer the secondary windings of which have their middles connected in a neutral point in this way the secondary windings have six ends connected to six anodes A by choking coils D in series. [Pg.195]

One of the best known examples of suspended transformation is found with the polymorphs formed by quartz [23]. The three principal polymorphic forms are quartz, tridymite, and cristobalite, which are enantiotropically related to each other. The ordinary transition point for the quartz/tridymite transition is 870°C, while the ordinary transition point for the tridymite/cristobalite transition is 1470°C. The melting point of cristobalite is at 1705°C, which exceeds all of the solid phase transition points. However, the phase transformations of these forms are extremely sluggish, and consequently each mineral form can be found in nature existing in a metastable form. [Pg.59]

Ordinarily, the rate-determining step during phase conversion is the formation of nuclei of the new phase. If suitable nuclei cannot be formed at the conditions of study, then the phase transformation is effectively suspended until the nuclei either form spontaneously or are added by the experimenter. 8ynthetic chemists have long used seed crystals of their desired phase to obtain a sufficient crop of that material and to suppress the formation of unwanted by-products. This procedure is especially important during the resolution of enantiomers and diastereomers by direct crystallization. [Pg.59]

If a weight is suspended from a rubber band, and the band is then heated (taking care not to burn it), the rubber band will contract appreciably. All materials other than polymers will undergo thermal expansion upon heating (assuming that no phase transformation has occurred over the temperature range). [Pg.3]

The microbial transformations of the wastewater described in the concept shown in Figure 5.5 deal with the COD components defined in Section 3.2.6. The figure also depicts the major processes that include the transformations of the organic matter (the electron donors) in the two subsystems of the sewer the suspended wastewater phase and the sewer biofilm. The air-water oxygen transfer (the reaeration) provides the aerobic microbial processes with the electron acceptor (cf. Section 4.4). Sediment processes are omitted in the concept but are indirectly taken into account in terms of a biofilm at the sediment surface. Water phase/biofilm exchange of electron donors and dissolved oxygen is included in the description. [Pg.106]

Specific research subjects have emerged with respect to improved descriptions of specific phenomena. Some time ago, it was speculated that gas-solid interactions and turbulence effects on reaction kinetics would be important areas of advance in the modeling art. Gas-solid interactions include both chemical formation of aerosols and reactions on surfaces of pre-existing suspended particulate matter. Because of differing effects of a material in the gas phase and in some condensed phase, it will be important to characterize transformation processes. The achex (Aerosol Characterization hYperiment) program recently carried out under the direction of Hidy will provide an extensive data base with which to test new ways of treating the gas-solid interaction problem. [Pg.695]

Special consideration shonld be given to the transformation of contaminants in sediments and gronndwater. Under saturated conditions, the solid phase may function as a sink, reservoir, and reactor for contaminants. Contaminant presence, persistence, and transformation in the water phase is controlled by the chemistry of the water body, the surface properties of the materials forming the solid phase (sediments or suspended particles), and environmental conditions (temperature and aerobic or anaerobic stams). [Pg.286]

Klupinski et al. (2004) conclude that the reduction of nitroaromatic compounds is a surface-mediated process and suggest that, with lack of an iron mineral, reductive transformation induced only by Fe(II) does not occur. However, when C Cl NO degradation was investigated in reaction media containing Fe(II) with no mineral phase added, a slow reductive transformation of the contaminant was observed. Because the loss of C Cl NO in this case was not described by a first-order kinetic model, as in the case of high concentration of Fe(II), but better by a zero-order kinetic description, Klupinski et al. (2004) suggest that degradation in these systems in fact is a surface-mediated reaction. They note that, in the reaction system, trace amounts of oxidize Fe(II), which form in situ suspended iron oxide... [Pg.328]

In these chapters, we focus on equilibrium situations and the associated problem of calculating the distribution of a compound between the different phases, when no net exchange occurs anymore. There are many situations in which it is correct to assume that phase transfer processes are fast compared to the other processes (e.g., transformations) determining a compound s fate. In such cases, it is appropriate to describe phase interchanges with an equilibrium approach. One example would be partitioning of compounds between a parcel of air and the aerosols suspended in it. Another case might be partitioning between the pore water and solids in sediment beds. [Pg.55]

The individual mass transfer and reaction steps outlined in Fig. 4.15 will now be described quantitatively. The aim will be firstly to obtain an expression for the overall rate of transformation of the reactant, and then to examine each term in this expression to see whether any one step contributes a disproportionate resistance to the overall rate. For simplicity we shall consider the gas to consist of just a pure reactant A, typically hydrogen, and assume the reaction which takes place on the interior surface of the catalyst particles to be first order with respect to this reactant only, i.e. the reaction is pseudo first-order with rate constant A ,. In an agitated tank suspended-bed reactor, as shown in Fig. 4.20, the gas is dispersed as bubbles, and it will be assumed that the liquid phase is well-mixed , i.e. the concentration CAL of dissolved A is uniform throughout, except in the liquid films immediately surrounding the bubbles and the particles. (It will be assumed also that the particles are not so extremely small that some are present just beneath the surface of the liquid within the diffusion film and are thus able to catalyse the reaction before A reaches the bulk of the liquid.)... [Pg.235]

Figure 9. A. Thermotropic fluorescence spectra of E. coli DH1 cells using the hydrophobic probe, N-phenyl-1 -naphthylamine (NPN). (a) Mid-log phase cells (b) stationary phase cells (c) cells made genetically transformable by the method of Hanahan.146 NPN was added to 4 mL of cell culture to a final concentration of 1 pM and the thermotropic fluorescence spectra were recorded.24 Measurements were made at increasing temperature (ca. 2 °C per min). Excitation 360 nm emission 410 nm. Measurements were made at increasing temperature (ca. 2 °C per min). B. Effects of physical treatments on the thermotropic transitions in genetically competent E. coli DH1. (a) Thermotropic transitions at descending temperature (b) cells pelleted at low speed and suspended in supernatant (c) as in b but suspended in equal volume of distilled water (d) as in (b) but suspended in 10 mM phosphate buffer, pH 7.4. Excitation 360 nm emission 410 nm. Fluorescent probe was NPN. Measurement (a) was made at decreasing temperature and (b), (c), (d) at increasing temperatures (ca. 2 °C per min). Figure 9. A. Thermotropic fluorescence spectra of E. coli DH1 cells using the hydrophobic probe, N-phenyl-1 -naphthylamine (NPN). (a) Mid-log phase cells (b) stationary phase cells (c) cells made genetically transformable by the method of Hanahan.146 NPN was added to 4 mL of cell culture to a final concentration of 1 pM and the thermotropic fluorescence spectra were recorded.24 Measurements were made at increasing temperature (ca. 2 °C per min). Excitation 360 nm emission 410 nm. Measurements were made at increasing temperature (ca. 2 °C per min). B. Effects of physical treatments on the thermotropic transitions in genetically competent E. coli DH1. (a) Thermotropic transitions at descending temperature (b) cells pelleted at low speed and suspended in supernatant (c) as in b but suspended in equal volume of distilled water (d) as in (b) but suspended in 10 mM phosphate buffer, pH 7.4. Excitation 360 nm emission 410 nm. Fluorescent probe was NPN. Measurement (a) was made at decreasing temperature and (b), (c), (d) at increasing temperatures (ca. 2 °C per min).
Rivers transport material in several phases dissolved, suspended particulate and bed load. Physical and chemical processes within an estuary infiuence the transportation and transformation of this material, thereby affecting the net supply of material to the oceans. Several definitions and geomorphologic classifications of estuaries have been reviewed by Pe-rillo (1995). From a chemical perspective, an estuary is most simply described as the mixing zone between river water and seawater characterised by sharp gradients in the ionic strength and chemical composition. Geographic distinctions can be made between drowned river valleys, fjords and bar-built estuaries. They can alternatively be classified in terms of the hydrodynamic regime as ... [Pg.219]


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See also in sourсe #XX -- [ Pg.58 , Pg.69 ]




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Suspended phase

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