Abstract
By simply changing the isotopes of the Si atoms that neighbor an oxygen atom in crystalline silicon, the measured decay rate of the asymmetric-stretch vibration () of oxygen () in silicon changes by a factor of . These data establish that decays by creating one symmetric-stretch, local-vibrational mode of the structure. If the residual energy () is less than the maximum frequency of the host lattice, as for in natural silicon, then it is emitted as one lattice mode, and depends on the density of one-phonon states at . If , as for in single-isotope silicon, two lattice modes are created in addition to , increasing . Prediction of for a particular defect clearly requires a detailed knowledge of that defect.
- Received 17 March 2006
DOI:https://doi.org/10.1103/PhysRevLett.96.225503
©2006 American Physical Society