Abstract
Many nonmetals and metal dioxides , including the dense form of stishovite, crystalize in a rutile structure at low pressure and transform to a denser structure under high pressure. Structures and transformations in dioxides hence serve as an archetype for applications in materials science and inside the Earth and terrestrial planets. Despite its significance, however, the deformation behavior of compounds in the structure is very poorly constrained. Here we use radial x-ray diffraction in a diamond-anvil cell and study as a representative system of the family. We identify the dominant slip systems and constrain texture evolution in -structured phases. After phase transition to a structure above 3.5 GPa, the dominant (010)[100] and secondary {110}[001] and {011}[0-11] slip systems induce a 121 texture in compression. Further compression increases the activity of the slip system, with an enhanced 001 texture at . During pressure release, the 001 texture becomes dominant over the original 121 texture. This clearly demonstrates the effect of pressure on the deformation behavior and slip systems of -structured dioxides. Finally, transforms back to a rutile structure upon pressure release, with a significant orientation memory, highlighting the martensitic nature of the to rutile structural transformation. These findings provide key guidance regarding the plasticity of -structured dioxides, with implications in materials and Earth and planetary science.
- Received 14 December 2021
- Accepted 15 April 2022
DOI:https://doi.org/10.1103/PhysRevMaterials.6.053603
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