Characterizing kinetics of transport and transformation of selenium in water–sediment microcosm free from selenium contamination using a simple mathematical model

Abstract

This study developed a seven-compartment model for predicting the fate of selenium (Se) in an aquatic environment containing a water–sediment boundary. Speciation of Se in water–sediment microcosms under microaerobic conditions was measured to evaluate first-order kinetics of Se transportation and transformation. The microcosm consisted of a 10-ml solution containing 1 mM soluble Se as selenate (Se 6+) or selenite (Se 4+) and 8 g wet sediment that was free from Se contamination, sampled from the Senri, Yamato, or Yodo Rivers in Osaka, Japan. Stepwise reaction coefficients describing transportation and transformation were determined using an inverse method on this model which includes: selenate ( Se W 6 + ) and selenite ( Se W 4 + ) in ponded water; selenate ( Se S 6 + ) and selenite ( Se S 4 + ) , elemental Se (Se 0), organic Se (Se 2−) in sediment; and gaseous Se (DMSe). During this 1-month experiment, soluble Se was transported from ponded water to the sediment and Se was transformed sequentially to other Se species through biochemical reactions. Experimental and kinetic analyses indicated quantitatively that the Yamato River microcosm, with its high organic matter content, had a high adsorption rate of soluble Se. The Yodo River microcosm had a low adsorption rate for Se 6+ and a low Se reduction rate. The Senri River microcosm had an apparent high volatilization rate of DMSe. The model developed in this study is extremely useful for predicting fate of Se in aquatic environment in the field.