Mechanical activation (i.e., tumbling) of quartz sand
in a carbon
dioxide (CO2) atmosphere leads to triboelectric charging
of the sand grains, driving a process that ultimately sequesters and
removes CO2 from the ambient atmosphere. Supported by diffuse
reflectance FTIR and 13C solid-state NMR experiments and
density functional theory (DFT) calculations, we propose that CO2 is inserted into the quartz lattice to form an anchored CO3 species, a process that otherwise requires high temperature
and pressure to proceed synthetically. The products of the reaction
are stable for at least 6 months at ambient temperature and pressure,
but CO2 is liberated at temperatures above 150 °C.
The prospect of using this method to remove CO2 from the
atmosphere and, ultimately, to help mitigate the adverse effects of
greenhouse gases and global warming is briefly discussed.