“…27,33,103,[108][109][110][111][112][113][114][115][116] Rather, Cu from CuO nanoparticles is often modeled as complexed by SOM, neoformed as Cu x S, or adsorbed by iron or aluminum oxides. 27,33,109,116 However, reducing conditions such as those that lead to Cu x S formation are less likely to occur in soils from arid or Mediterranean climates. 107,113 Further, soils in these climates, and more generally, soils that have undergone minimal mineral weathering, are dominated by phyllosilicate minerals and are unlikely to contain significant amounts of iron or aluminum oxides.…”