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UNIFORM PARTICLES WITH A LARGE SURFACE AREA FORMED
UNIFORM PARTICLES WITH A LARGE SURFACE AREA FORMED

... The precipitation of ferric sulfate with HMTA using method C yielded ammonium– hydronium jarosite at pH ⬃ 2 and schwertmannite at pH ⬃ 5 (see Table 3), but the primary particles did not aggregate into large spheres at all. This comparison clearly demonstrates the indispensable role of urea that prom ...
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... What is the number of protons, neutrons, and electrons in the nitrogen-14 –3 ion? (3 pts) a) 7 protons; 7 neutrons; 7 electrons b) 7 protons; 7 neutrons; 10 electrons c) 8 protons; 6 neutrons; 14 electrons ...
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... that their equilibrium constants are adequately separated. The error will not be more than 5% provided that the ratio of successive constants is not greater than 100 ( Stumm and Morgan 1970). Clearly reactions a to CZcan be treated independently from reactions e to h with little error, but the ‘reac ...
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... 1. Describe the properties of solutions. (15.1) 2. Describe and identify the different components of solutions. (15.1) 3. Identify the different types of solutions. (15.1) 4. Describe and give examples of alloys. (15.1) 5. Describe soluble, insoluble, miscible, and immiscible systems. (15.1) 6. Desc ...
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... any bowed string instrument will suffice for this thought experiment): the bow is drawn and a sound is produced. But the physical attributes of the motion here described are not as mono-dimensional as they first may appear; instead, it better considered as a composite action formed from several acti ...
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< 1 ... 15 16 17 18 19 20 21 22 23 ... 71 >

Spinodal decomposition



Spinodal decomposition is a mechanism for the rapid unmixing of a mixture of liquids or solids from one thermodynamic phase, to form two coexisting phases. As an example, consider a hot mixture of water and an oil. At high temperatures the oil and the water may mix to form a single thermodynamic phase in which water molecules are surrounded by oil molecules and vice versa. The mixture is then suddenly cooled to a temperature at which thermodynamic equilibrium favours an oil-rich phase coexisting with a water-rich phase. Spinodal decomposition then occurs when the mixture is such that there is essentially no barrier to nucleation of the new oil-rich and water-rich phases. In other words, the oil and water molecules immediately start to cluster together into microscopic water-rich and oil-rich clusters throughout the liquid. These clusters then rapidly grow and coalesce until there is a single macroscopic oil-rich cluster, the oil-rich phase, and a single water-rich cluster, the water-rich phase.Spinodal decomposition can be contrasted with nucleation and growth. There the initial formation of the microscopic clusters involves a large free energy barrier, and so can be very slow, and may occur as little as once in the initial phase, not throughout the phase, as happens in spinodal decomposition.Spinodal decomposition is of interest for two primary reasons. In the first place, it is one of the few phase transformations in solids for which there is any plausible quantitative theory. The reason for this is the inherent simplicity of the reaction. Since there is no thermodynamic barrier to the reaction inside of the spinodal region, the decomposition is determined solely by diffusion. Thus, it can be treated purely as a diffusional problem, and many of the characteristics of the decomposition can be described by an approximate analytical solution to the general diffusion equation.In contrast, theories of nucleation and growth have to invoke the thermodynamics of fluctuations. And the diffusional problem involved in the growth of the nucleus is far more difficult to solve, because it is unrealistic to linearize the diffusion equation.From a more practical standpoint, spinodal decomposition provides a means of producing a very finely dispersed microstructure that can significantly enhance the physical properties of the material.
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