(Phys.org) —Capturing carbon dioxide and storing it in underground rock formations is one proposed solution to mitigate climate change. New knowledge about the chemical reactions between stored carbon dioxide and forsterite (Mg2SiO4) is helping determine how much confidence can be placed in using igneous rocks with magnesium-rich olivines for long-term carbon sequestration. Scientists at Pacific Northwest National Laboratory determined that the carbon dioxide and forsterite react to form hydrated dypingite [(Mg5(CO3)4•5H2O)], which precipitates from solution.
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