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Optical-absorption measurements to 100-kbar hydrostatic pressure have been performed on CdS in a diamond anvil cell. The results indicate that the energy gap is direct in the wurzite phase and indirect in the rock-salt phase, which becomes stable above {~} 28 kbar. The initial dEgdP≈0, followed by red shift above 60 kbar in the rock-salt phase, is interpreted in terms of a changeover from Σᵥ→Xc to Lᵥ→Xc gap. The measured gap of 1.7 eV and the above assignments would be consistent with the band-structure calculations for the rock-salt phase of CdS.
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Batlogg et al. (1983) studied this question.
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