Abstract

Our investigations on porous Si (π-Si) show that on increase of pressure it undergoes crystalline phase transitions instead of pressure-induced amorphization, as suggested earlier, and the amorphous phase appears only on release of pressure. This amorphous phase, when subjected to higher pressures, transforms reversibly to a higher-coordinated primitive hexagonal phase, showing a kind of memory effect which may be the only example of its kind in the elemental solids. First-principles calculations and thermodynamic arguments help understand these observations.

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.