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The breakthrough curves of the particles of magmatic rock to uptake Fe ions from aqueous solution were investigated using a fixed-bed sorption column. The effect of inlet Fe concentration, feed flow rate, bed height, initial solution pH and particle size on the breakthrough characteristics of the sorption system were investigated. The highest experimental bed capacities for Fe ions was obtained to be 3.65 mg.g at inlet Fe concentration of 75 ppm, bed height of 5 cm and flow rate of 5 mL.min, pH of 5 and particle size of 0.25-0.5 mm, respectively. The results indicated that magmatic rock material is a suitable sorbent for the uptake of Fe ions from an aqueous solution.

Determination of Breakthrough Curves for the Uptake of Fe3 Using Magmatic Rock Material in Fixed Bed Column