Titanium (Ti) is relatively abundant, but the minerals that contain it are not very soluble in water, and mineralized titanium is thus considered inert. The most stable oxidation state is +4, and most titanium in minerals is found as TiO2 or bound in iron-titanium oxides.
Iron-rich lateritic soils in tropical environments tend to have the highest concentrations of Ti; Hawaiian soils have Ti concentrations of up to 15%. The worldwide average soil content of Ti is about 0.33%, and soil solutions average 30 mg/L. The primary factor determining the bioavailability of Ti is pH, and titanium is more soluble at pH values below 4. Gray hair grass grown in soil at pH 3.1 had a Ti content of 142 mg/kg in the leaves, but when grown in soil with identical Ti content with a pH of 4.9, the leaf titanium content was reduced to only 2.4 mg/kg.