i wasnt too sure as to where to post this question as it does deal with chemistry, but also geology. so here it is in chemistry- other.
in the pyroxene silicate mineral series, there is a solid solution between enstatite (MgSiO3) and ferrosilite (FeSiO3). I know the rules for solid solution- same size, charge, temp/pressure and availability of the ions. So, i know Mg and Fe are similar in size and charge and can substitute for one another in the solution in a constant temperature/pressure situation. why? why would Mg go into the site, rather than Fe? can it really be the availability of the ions or is there something obvious im missing here? i feel like the reason cant be that obvious. but, i cant think of any other reason why. the size difference in the ionic radius is so small (Fe's is 8% bigger and its under the 15% limit) it should not make a difference. furthermore, i guess i want to know why a solid solution is occurring at all. why not some other mineral with the same size or charge or why dont all minerals have solid solutions. any help is appreciated, even and especially if its telling me what to read or teach myself, lol.