The presence of iron oxides in clay or silica raw materials is detrimental to the manufacturing of high quality ceramics. Although iron has been traditionally removed by physical mineral processing, acid washing has been tested as it is more effective, especially for extremely low iron (of less than 0.1% w/w). However, inorganic acids such as sulphuric or hydrochloric acids easily contaminate the clay products with SO42- and Cl-, and therefore should be avoided as much as possible. On the other hand, if oxalic acid is used, any acid left behind will be destroyed during the firing of the ceramic products. The characteristics of dissolution of iron oxides were therefore investigated in this study. The dissolution of iron oxides in oxalic acid was found to be very slow at temperatures within the range 25-60 degrees C, but its rate increases rapidly above 90 degrees C. The dissolution rate also increases with increasing oxalate concentration at the constant pH values set within the optimum range of pH2.5-3.0. At this optimum pH, the dissolution of fine pure hematite (Fe2O3) (105-140 mu m) follows a diffusion-controlled shrinking core model. The rate expression expressed as 1-(2/3)x-(1-x)(2/3) where x is a fraction of iron dissolution was found to be proportional to [oxalate](1.5). The addition of magnetite to the leach liquor at 10% w/w hematite was found to enhance the dissolution rate dramatically. Such addition of magnetite allows coarser hematite in the range 0.5-1.4 nun to be leached at a reasonable rate. (c) 2006 Elsevier B.V. All rights reserved.