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Defects in inorganic photorefractive materials and their investigations

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<strong>Defects</strong> <strong>in</strong> <strong>in</strong>organic <strong>photorefractive</strong> <strong>materials</strong> <strong>and</strong> <strong>their</strong> <strong>in</strong>vestigations 15<br />

4.2 Extr<strong>in</strong>sic defects<br />

At first the dop<strong>in</strong>gs are treated which prevent or reduce the formation of Nb Li<br />

dur<strong>in</strong>g crystal growth from Li-deficient melts, such as Mg or Zn with concentrations<br />

<strong>in</strong> the percent range. Further <strong>in</strong>formation on such ’optical damage<br />

resistant’ dop<strong>in</strong>gs is given <strong>in</strong> Chapter 6. As has been mentioned above, the reduction<br />

of crystals of this type leads to the formation of almost free electrons,<br />

transformed to Nb 4+<br />

Nb<br />

polarons by coupl<strong>in</strong>g to the lattice. This is an <strong>in</strong>dication<br />

for the absence of Nb Li as trapp<strong>in</strong>g centers. Several additional dop<strong>in</strong>gs <strong>in</strong> such<br />

crystals were <strong>in</strong>vestigated by EPR. The correspond<strong>in</strong>g signals are characterized<br />

by <strong>their</strong> large width, result<strong>in</strong>g from the addition of the dop<strong>in</strong>g-<strong>in</strong>duced<br />

disorder to the <strong>in</strong>tr<strong>in</strong>sic one. Table 1 conta<strong>in</strong>s also <strong>in</strong>formation on the extr<strong>in</strong>sic<br />

defects <strong>in</strong>vestigated <strong>in</strong> such crystals. It was found that additional extr<strong>in</strong>sic<br />

ions tend to be <strong>in</strong>corporated at the Nb-sites of the lattice; apparently it is<br />

more favorable that the Mg ions, rather abundant <strong>in</strong> the melt, replace Li ions.<br />

Fig. 7. Comparison of EPR signals of LN:Cr <strong>and</strong> LN:Fe <strong>in</strong> congruent <strong>and</strong> stoichiometric<br />

LN. Top: ’New’ Cr 3+<br />

Nb<br />

signals (a), characterized by a weak axial crystal<br />

field typical for Nb replacement, as compared to those (b) of ’old’ Cr 3+<br />

Li<br />

with typical<br />

strong axial crystal field [88]. Bottom: In congruent LN the ’old’ Fe 3+<br />

Li<br />

(d) is observed.<br />

In stoichiometric material two additional types of Fe 3+ spectra arise (c) <strong>and</strong><br />

all l<strong>in</strong>es become more narrow [64].<br />

Here it has to be noted that it is rather difficult to determ<strong>in</strong>e from basic arguments<br />

at which site, Li or Nb, cation dop<strong>in</strong>gs will enter LN. Both sites have

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