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Two-component Mixing

A frequently cited example of protection from atmospheric corrosion is the Eiffel Tower. The narrow and, for that age, thin sections required a good priming of red lead for protection against corrosion. The top coat was linseed oil with white lead, and later coatings of ochre, iron oxide, and micaceous iron oxide were added. Since its constmction the coating has been renewed several times [29]. Modern atmospheric corrosion protection uses quick-drying nitrocellulose, synthetic resins, and reaction resins (two-component mixes). The chemist Leo Baekeland discovered the synthetic material named after him, Bakelite, in 1907. Three years later the first synthetic resin (phenol formaldehyde) proved itself in a protective paint. A new materials era had dawned. [Pg.9]

Saddle point. 170 Salt effects. 206-214 Scavenging (see Reactions, trapping) Second-order kinetics. 18-22, 24 in one component, 18-19 in two components (mixed), 19-22 Selectivity. 112 Sensitivity analysis. 118 Sensitivity factor, 239-240 Sequential reactions (see Consecutive reactions)... [Pg.280]

For the two-component mixed phases the surface and Coulomb contributions can be estimated along the lines of the analysis performed in Ref. [47] for the interface between nuclear and CFL matter. We find a gain in bulk energy of at most 6 MeV/fm3 which is already weight out by Coulomb and surface energy for relatively small values of the surface tension a 10 MeV/fm2. Note... [Pg.200]

Figure 20. Calculated Fe isotope composition of seawater from different ocean basins based on a simple two-component mixing between Fe from aerosol particles and Fe from mid-oceanic-ridge (MOR) hydrothermal solutions. Atmospheric Fe fluxes (Jatm) for different ocean basins from Duce and Tindale (1991) MOR hydrothermal Fe flux ( mor) to different ocean basins were proportioned relative to ridge-axis length. Modified from Beard et al. (2003a). Figure 20. Calculated Fe isotope composition of seawater from different ocean basins based on a simple two-component mixing between Fe from aerosol particles and Fe from mid-oceanic-ridge (MOR) hydrothermal solutions. Atmospheric Fe fluxes (Jatm) for different ocean basins from Duce and Tindale (1991) MOR hydrothermal Fe flux ( mor) to different ocean basins were proportioned relative to ridge-axis length. Modified from Beard et al. (2003a).
The principle of two-component mixing can be applied to isotope geochemistry. [Pg.118]

Single spiking method is essentially a problem of two-component mixing. The ratio of the abundances of two isotopes A and B of an element in the mixture is (Faure, 1986)... [Pg.225]

Uptake of Ca2+ from the intestine is stimulated by vitamin D.447 Vitamin D3 is converted to the 25-hydroxy derivative in the liver (equation 11) by a two component mixed-function hydroxylase.448 The metabolically active 1,25-dihydroxy form is synthesized by further hydroxylation in the kidney. This latter stage involves the renal 25-hydroxyvitamin D3- 1-hydroxylase in a reaction which is controlled by Ca2+, parathyroid hormone and phosphate. This renal hydroxylase contains a flavoprotein, an iron-sulfur protein (with an Fe2S2 cluster) and cytochrome P-450.447... [Pg.596]

Figure 11.7 Potential energy diagrams for a two-component mixed valence device with (a) negligible, (b) weak and (c) strong electronic coupling. The dashed curves represent unperturbed zero-order states. The horizontal axis represents generalised nuclear coordinates, including contributions from both ligand atom positions and solvent sphere. Figure 11.7 Potential energy diagrams for a two-component mixed valence device with (a) negligible, (b) weak and (c) strong electronic coupling. The dashed curves represent unperturbed zero-order states. The horizontal axis represents generalised nuclear coordinates, including contributions from both ligand atom positions and solvent sphere.
Heterogeneous accretion models for the formation of the Earth advocate the initial accretion of refractory, less-oxidized components that make up the bulk of the planet (some 50-80%), followed by the accretion of a lower-temperature, more oxidized component (e.g., perhaps comparable to carbonaceous chondrites). The overall nature of the initially refractory material is not well characterized, but it could have affinities to ordinary or enstatite chondrites. These two-component mixing models seek to reconcile the observational constraints from chemical and isotopic studies of the silicate Earth. As of early 2000s, we do not have sufficient data to identify in detail the nature of these two components of accretion if they existed. [Pg.1261]

Two-component mixing models. Isotope hydrograph separation normally involves a two-component mixing model for the stream. The model assumes that water in the stream at any time during storm or snowmelt runoff is a mixture of two components new water and old water. [Pg.2585]

Although the simple two-component mixing model approach to stream hydrograph separation does not directly identify the actual runoff... [Pg.2585]

The universal applicability of the simple two-component mixing model has been frequently challenged (Kennedy et al., 1986 Rodhe, 1987 Sklash, 1990 McDonnell et al., 1991 Bishop, 1991 Kendall and McDonnell, 1993). These challenges address the five assumptions governing the use of the two-component mixing model given in Sklash and Farvolden (1982) and listed above. [Pg.2588]

The size of the sample is now specified in practice by its mass M and no longer by the number of particles rip, as shown in Eq. (21-63). The variance in random mixture for the case of two-component mixes can be given by... [Pg.2279]

Figure 5 (a) Flow pattern in the precipitation vessel from a two-component mixing nozzle, (b) Distribution of fluid density in this system at 20 MPa and 323.1 K in the vessel. [Pg.106]

Figure 16 Supersaturation profiles during precipitation of acetaminophen by means of a two-component mixing nozzle at (a) Re = 1000 and (b) Re = 30,000. Pressure is 20 MPa, temperature 323.1 K. The volumetric flow ratio between CO2 and the ethanol solution is constant at 0/Qa 100. Figure 16 Supersaturation profiles during precipitation of acetaminophen by means of a two-component mixing nozzle at (a) Re = 1000 and (b) Re = 30,000. Pressure is 20 MPa, temperature 323.1 K. The volumetric flow ratio between CO2 and the ethanol solution is constant at 0/Qa 100.
To ensure that this is so, the effect of adding a dispersing and binding agent to two-component mixed slurry were measured. [Pg.345]

The term mixed micelle means a micelle composed of two (or more) surfactant components, with each surfactant component able to form micelles on its own. As far as we are aware, only two-component mixed micelles have been studied. Nishikido has recently reviewed most of the work... [Pg.385]

Table I. Activity Coefficients of DML and DOL in Two-Component Mixed Monolayers with CHOL Comparison with Regular Solution Heats of Mixing... Table I. Activity Coefficients of DML and DOL in Two-Component Mixed Monolayers with CHOL Comparison with Regular Solution Heats of Mixing...

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