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Crystal defect formation

The most developed and widely used approach to electroporation and membrane rupture views pore formation as a result of large nonlinear fluctuations, rather than loss of stability for small (linear) fluctuations. This theory of electroporation has been intensively reviewed [68-70], and we will discuss it only briefly. The approach is similar to the theory of crystal defect formation or to the phenomenology of nucleation in first-order phase transitions. The idea of applying this approach to pore formation in bimolecular free films can be traced back to the work of Deryagin and Gutop [71]. [Pg.84]

Dehydrogenation is considered to occur on the corners, edges, and other crystal defect sites on the catalyst where surface vacancies aid in the formation of intermediate species capable of competing for hydrogen with ethylbenzene. The role of the potassium may be viewed as a carrier for the strongly basic hydroxide ion, which is thought to help convert highly aromatic by-products to carbon dioxide. [Pg.198]

In addition, we have shown that further defect formation can be induced by external reacting species, and that these act to form specific types of defects, depending upon the chemical nature of the crystal lattice. [Pg.110]

Although we win not treat the other types of pairs of defects, it is well to note that similar equations can also be derived for the other intrinsic defects. What we have really shown is that external reactants can cause further changes in the non-stoichiometry of the soUd. Let us now consider ionized defects. It should be clear that an external gaseous factor has a major effect upon defect formation. The equations given above are very complicated and represent more closely what actually happens in the real world of defect formation in crystals. [Pg.118]

Grain boundaries form junctions between grains within the particle, due to vacancy and line-defect formation. This situation arises because of the 2nd Law of Thermodjmamics (Entropy). Thus, if crystallites are formed by precipitation from solution, the product will be a powder consisting of many small particles. Their actual size will depend upon the methods used to form them. Note that each crystallite can be a single-crystal but, of necessity, will be limited in size. [Pg.252]

When writing defect formation equations, the strategy involved is always to add or subtract elements to or from a crystal via electrically neutral atoms. When ionic crystals are involved, this requires that electrons are considered separately. Thus, if one considers NiO to be ionic, formation of a VNi would imply the removal of a neutral Ni atom, that is, removal of a Ni2+ ion together with two electrons. Similarly, formation of a VQ would imply removal of a neutral oxygen atom, that is, removal of an O1 2- ion, followed by the addition of two electrons to the crystal. An alternative way to express this is to say the removal of an O2- ion together with 2h. Similarly, only neutral atoms are added to interstitial positions. If ions are considered to be present, the requisite number of electrons must be added or subtracted as well. Thus, the formation of an interstitial Zn2+ defect would involve the addition of a neutral Zn atom and the removal of two electrons. [Pg.31]

Results have shown that the properties of solids can usually be modeled effectively if the interactions are expressed in terms of those between just pairs of atoms. The resulting potential expressions are termed pair potentials. The number and form of the pair potentials varies with the system chosen, and metals require a different set of potentials than semiconductors or molecules bound by van der Waals forces. To illustrate this consider the method employed with nominally ionic compounds, typically used to calculate the properties of perfect crystals and defect formation energies in these materials. [Pg.70]

The energy of formation of a defect in a typical metal varies from approximately 1 x 10 19 J to 6x 10—19 J. (a) Calculate the variation in the fraction of defects present, n([/ V, in a crystal as a function of the defect formation energy, (b) Calculate the variation in the fraction of defects present as a function of temperature if the defect formation energy is 3.5 x 10-19 J. [Pg.80]

We turn first to the (4 + 4) photodimerization of anthracenes, which has been most extensively studied in this context. In many anthracenes it has been possible to show that in the starting crystals defects are present at which the structure is appropriate for formation of the observed dimer in others it has been argued that the presence of such defects is very plausible. The weakness of this interpretation, at this stage, is that in no case has it yet proved possible to establish that the reaction indeed occurs at these defect sites. [Pg.174]

At present the iron-based alloys diffusion saturation by nitrogen is widely used in industry for the increase of strength, hardness, corrosion resistance of metal production. Inexhaustible and unrealized potentialities of nitriding are opened when applying it in combination with cold working [1-3], It is connected with one of important factors, which affects diffusion processes and phase formation and determines surface layer structure, mechanical and corrosion properties, like crystal defects and stresses [4, 5], The topical question in this direction is clarification of mechanisms of interstitial atoms diffusion and phase formation in cold worked iron and iron-based alloys under nitriding. [Pg.491]

The solubility and the hydrolysis constants enable the concentration of iron that will be in equilibrium with an iron oxide to be calculated. This value may be underestimated if solubility is enhanced by other processes such as complexation and reduction. Solubility is also influenced by ionic strength, temperature, particle size and by crystal defects in the oxide. In alkaline media, the solubility of Fe oxides increases with rising temperature, whereas in acidic media, the reverse occurs. Blesa et al., (1994) calculated log Kso values for Fe oxides over the temperature range 25-300 °C from the free energies of formation for hematite, log iCso fell from 0.44 at 25 °C to -10.62 at300°C. [Pg.208]

The effect of these substituents has not been fully explained. It is not, in most cases, due to formation of a protective layer of the substituent at the surface because (M = trivalent substituent) and Fe usually dissolve congruently. Crystal defects (e. g. vacancies) created by substitution should accelerate dissolution, but this is not... [Pg.331]


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