High-pressure phase transitions and melt structure of PbO2 : An analog for silica
Source abstract
Abstract
In situ x-ray diffraction measurements and inverse Monte Carlo simulations of pair distribution functions were used to study the structural response of $\mathrm{Pb}{\mathrm{O}}2$ under pressure and to characterize the local structure of liquid $\mathrm{Pb}{\mathrm{O}}2$. Two phase transitions are observed upon room-temperature compression of crystalline $\mathrm{Pb}{\mathrm{O}}2$ up to \ensuremath{\sim}65 GPa. The starting mixture of rutile structured $\ensuremath{\beta}\text{\ensuremath{-}}\mathrm{Pb}{\mathrm{O}}2$ and orthorhombic $\ensuremath{\alpha}\text{\ensuremath{-}}\mathrm{Pb}{\mathrm{O}}2$ undergoes a transition to a ${\mathrm{ZrO}}2$-type orthorhombic phase with space group $Pbca$ at \ensuremath{\sim}21 GPa. Above 42 GPa, the $Pbca$ phase transforms to a cotunnite-type phase with space group $Pnam$. In this paper, we also report short-range order in liquid $\mathrm{Pb}{\mathrm{O}}2$, showing \ensuremath{\sim}8--9-fold and 4--5-fold coordination around Pb and O atoms, respectively.
Source: openalex_inverted_index · Quality: baseline
Research context
OpenAlex topics: High-pressure geophysics and materials · Crystal Structures and Properties · X-ray Diffraction in Crystallography
SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.
Affiliations
Earth and Planetary Sciences Department, University of California, Santa Cruz, California 95064, USA
Advanced Light Source, Lawrence Berkeley National Laboratory, Berkeley, California 94720, USA
Department Earth and Planetary Science, University of California, Berkeley, California, USA
Department Astronomy and Miller Institute for Basic Research in Science, University of California, Berkeley, California, USA
Funding
U.S. Department of Energy · National Science Foundation
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