Answers are grounded in this paper and cite their sources.
We have synthesized the orthocarbonate Sr 3 [CO 4 ]O in a laser-heated diamond anvil cell at 20 and 30 GPa by heating to ≈3000 (300) K. Afterward, we recovered the orthocarbonate with [CO 4 ] 4– groups at ambient conditions. Single-crystal diffraction shows the presence of [CO 4 ] 4– groups, i.e., sp 3 -hybridized carbon tetrahedrally coordinated by covalently bound oxygen atoms. The [CO 4 ] 4– tetrahedra are located in a cage formed by corner-sharing OSr 6 octahedra, i.e., octahedra with oxygen as a central ion, forming an antiperovskite-type structure. At high pressures, the octahedra are nearly ideal and slightly rotated. The high-pressure phase is tetragonal ( I 4/ mcm ). Upon pressure release, there is a phase transition with a symmetry lowering to an orthorhombic phase ( Pnma ), where the octahedra tilt and deform slightly.
No takes yet. Share an insight, caveat, or question.
Spahr et al. (2021) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: