“…Even when this is accounted for, effects of other common constituents of natural waters are usually not. For example, chloride, nitrate, sulphate, silicate and phosphate anions can participate in the Fe(III) precipitation process (Dousma et al, 1978(Dousma et al, , 1979Rose et al, 1996Rose et al, , 1997aSchwertmann et al, 1999;Doelsch et al, 2003), a fact that may also contribute to the sub-optimal fit of solubility models to data.…”