Abstract

A charge-density-wave ground state satisfactorily accounts for the experimentally observed occupied valley degeneracy, high cyclotron mass and stress-dependent anisotropic conductivity in inversion layers at the Si(111)-Si${\mathrm{O}}_{2}$ interface. We make specific predictions about anisotropic optical transitions, the observation of which would distinguish the density-wave model from any alternative explanations of the experimental data.

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.