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Introduction to Nanotechnology

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2.1. STRUCTURE 17<br />

of the large anions A"- with the small cations C"+ located in the tetrahedral sites of<br />

the anion FCC lattice. If the anions <strong>to</strong>uch each other, their radii have the value<br />

a. = a/21/2, where a is the lattice parameter, and the radius aT of the tetrahedral site<br />

aT = 0.2247~~ is given by Eq. (2.2). This is the case for the very small Ai3+ cation<br />

in the AlSb structure. In all other cases the cations in Table B.2 are <strong>to</strong>o large <strong>to</strong> fit in<br />

the tetrahedral site so they push the larger anions further apart, and the latter no<br />

longer <strong>to</strong>uch each other, in accordance with Fig. 2.9. In a covalent model for the<br />

structure consisting of neutral a<strong>to</strong>ms A and C the a<strong>to</strong>m sizes are comparable, as the<br />

data in Table B.2 indicate, and the structure resembles that of Si or Ge. To compare<br />

these two models, we note that the distance between a<strong>to</strong>m A at lattice position 0 0 0<br />

and its nearest neighbor C at position is equal <strong>to</strong> tau, and in Table B.3 we<br />

compare this crystallographically evaluated distance with the sums of radii of ions<br />

A"-, C"+ from the ionic model, and with the sums of radii of neutral a<strong>to</strong>ms A and C<br />

of the covalent model using the data of Table B.2. We see from the results on Table<br />

B.3 that neither model fits the data in all cases, but the neutral a<strong>to</strong>m covalent model<br />

is closer <strong>to</strong> agreement. For comparison purposes we also list corresponding data for<br />

several alkali halides and alkaline-earth chalcogenides that crystallize in the cubic<br />

rock salt or NaCl structure, and we see that all of these compounds fit the ionic<br />

model very well. In these compounds each a<strong>to</strong>m type forms a FCC lattice, with the<br />

a<strong>to</strong>ms of one FCC lattice located at octahedral sites of the other lattice. The<br />

octahedral site has the radius aoct = 0.4141 la, given by Eq. (2.1), which is larger<br />

than the tetrahedral one of Eq. (2.2).<br />

Since the alkali halide and alkaline-earth chalcogenide compounds fit the ionic<br />

model so well, it is significant that neither model fits the structures of the<br />

semiconduc<strong>to</strong>r compounds. The extent <strong>to</strong> which the semiconduc<strong>to</strong>r crystals exhibit<br />

ionic or covalent bonding is not clear from crystallographic data. If the wavefunction<br />

describing the bonding is written in the form<br />

where the coefficients of the covalent and ionic wavefunction components are<br />

normalized<br />

2<br />

acov +ai?,, = 1<br />

then a:ov is the fractional covalency and ai?,, is the fractional ionicity of the bond. A<br />

chapter (Poole and Farach 2001) in a book by Karl Boer (2001) tabulates the<br />

effective charges e* associated with various 11-VI and 111-V semiconducting<br />

compounds, and this effective charge is related <strong>to</strong> the fractional covalency by the<br />

expression<br />

8-N+e*<br />

4ov =<br />

8

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