The experimentally observed negative Poisson's ratios in the silicate α-cristobalite are explained through a two-dimensional ‘rotation of rigid units’ model involving ‘rotating rectangles’ hence providing a new insight into the way nature can achieve this unusual property.
J. N. Grima, R. Gatt, A. Alderson and K. E. Evans, J. Mater. Chem., 2005, 15, 4003 DOI: 10.1039/B508098C
To request permission to reproduce material from this article, please go to the Copyright Clearance Center request page.
If you are an author contributing to an RSC publication, you do not need to request permission provided correct acknowledgement is given.
If you are the author of this article, you do not need to request permission to reproduce figures and diagrams provided correct acknowledgement is given. If you want to reproduce the whole article in a third-party publication (excluding your thesis/dissertation for which permission is not required) please go to the Copyright Clearance Center request page.
Read more about how to correctly acknowledge RSC content.
Please wait while we load your content...