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Chapter VII Reactivity at Dislocation….<br />

represents their uniform speed away from the source, by simple geometry the<br />

resulting pit will have slope,<br />

255<br />

(7.10)<br />

The slope tan can be measured experimentally, but more attention is<br />

required to measure Vd.<br />

There are many other heterogeneities at which surface “holes” may be<br />

nucleated [27] giving rise to a finite value of surface dissolution or the polishing<br />

rate Vp; that describes the dissolution of the surface area free from dislocation<br />

and is directed normal to the surface.<br />

The rate of pit deepening is given by, dD/dt = Vd - Vp, using this in the earlier<br />

equation,<br />

(7.11)<br />

For etch pits formed at a constant rate, this expression can be transferred into a<br />

linear expression,<br />

Where, d is the measured depth of a pit after time t.<br />

(7.12)<br />

It is well-known that inorganic salts in solutions exist in the form of complexes<br />

whose chemical constitution depends on the concentration of the salt in solutions<br />

as well as on the concentration of another substance having an anion common<br />

with the additive salt [28, 29]. The instability constant of a series of complexes of<br />

salt, in general, regularly decreases, i.e., each successive complex is more<br />

stable [30]. The enhanced nucleation rate along the dislocation line, due to the

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