This article from Phys org explains how researchers used advanced simulations to study the distribution of nickel (Ni) and cobalt (Co) within the mineral forsterite, found in mafic and ultramafic rocks. They discovered that these critical elements preferentially incorporate into specific sites within the mineral’s structure. This research is significant for improving the economic viability of extracting these elements from abundant but lower-grade ores, which could also contribute to reducing CO2 emissions during the process.
For more details, you can read the full article here: