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Callister - An introduction - 8th edition

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12.5 Imperfections in Ceramics • 473<br />

Figure 12.21 Schematic diagram<br />

showing Frenkel and Schottky defects<br />

in ionic solids. (From W. G. Moffatt,<br />

G. W. Pearsall, and J. Wulff, The<br />

Structure and Properties of Materials,<br />

Vol. I, Structure, p. 78. Copyright ©<br />

1964 by John Wiley & Sons, New York.<br />

Reprinted by permission of John Wiley<br />

& Sons, Inc.)<br />

Schottky defect<br />

Frenkel defect<br />

1:1. A ceramic compound is nonstoichiometric if there is any deviation from this<br />

exact ratio.<br />

Nonstoichiometry may occur for some ceramic materials in which two valence<br />

(or ionic) states exist for one of the ion types. Iron oxide (wüstite, FeO) is one such<br />

material, because the iron can be present in both Fe 2 and Fe 3 states; the number<br />

of each of these ion types depends on temperature and the ambient oxygen pressure.<br />

The formation of an Fe 3 ion disrupts the electroneutrality of the crystal by<br />

introducing an excess 1 charge, which must be offset by some type of defect. This<br />

may be accomplished by the formation of one Fe 2 vacancy (or the removal of two<br />

positive charges) for every two Fe 3 ions that are formed (Figure 12.22). The crystal<br />

is no longer stoichiometric because there is one more O ion than Fe ion; however,<br />

the crystal remains electrically neutral. This phenomenon is fairly common in<br />

iron oxide, and, in fact, its chemical formula is often written as Fe 1–x O (where x is<br />

some small and variable fraction substantially less than unity) to indicate a condition<br />

of nonstoichiometry with a deficiency of Fe.<br />

Concept Check 12.2<br />

Can Schottky defects exist in K 2 O? If so, briefly describe this type of defect. If they<br />

cannot exist, then explain why.<br />

[The answer may be found at www.wiley.com/college/callister (Student Companion Site).]<br />

Fe 2+<br />

Vacancy<br />

Figure 12.22 Schematic<br />

representation of an Fe 2<br />

Fe 3+ vacancy in FeO that results<br />

from the formation of two<br />

Fe 3 ions.<br />

Fe 2+<br />

O 2–

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