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Chapter 9
            Phyto-transport and Assimilation of Selenium



            Xiao-Zhang Yu and Ji-Dong Gu











            9.1  Selenium in the Environment


            Selenium (Se) is one of the most widely distributed elements in the earth’s crust and
            geographic distribution of Se in the environment is extremely variable (Hansen
            et al. 1998). In China, the average abundance of Se in the earth’s crust is
                       1
            0.058 mg kg , which is slightly lower than that in other parts of the world (Xia
            and Tang 1990). While there are natural sources of Se, anthropogenic inputs of Se-
            containing chemicals into the environment are greater in amounts than natural
            contribution (Wu 2004). This has resulted in the elevated Se levels in natural
            ecosystems impacted by anthropogenic processes. Therefore, the risks derived
            from industrial activities and discharges have drawn widespread concern world-
            wide. Indeed, ample evidence showed that the increasing levels of Se have caused
            soil, air, and water pollution as well as changes in the structures of natural
            communities and ecosystems at organism levels (Ohlendorf et al. 1986; Banuelos
            et al. 1996).
              In nature, Se occurs in four oxidation states with the chemical forms of selenide
                                             0
                                                          4+
                                                                            6+
              2
            (Se ), elemental or “colloidal” Se (Se ), selenite (Se ), and selenate (Se )
            (Rosenfeld and Beath 1964). The most common and soluble species are selenate
            and selenite found mostly in seleniferous soils and agricultural drainage water
            (Banuelos and Lin 2005), whereas elemental Se dominates in anaerobic environ-
            ment (Terry et al. 2000). Selenide is the ionized form of hydrogen selenide (H 2 Se)
            and unstable in aqueous solutions (Barceloux 1999). Both selenate and selenite
            X.-Z. Yu (*)
            The Guangxi Key Laboratory of Theory and Technology for Environmental Pollution Control,
            College of Environmental Science and Engineering, Guilin University of Technology, Guilin
            541004, People’s Republic of China
            e-mail: yuxiaozhang@hotmail.com
            J.-D. Gu
            Laboratory of Environmental Toxicology, School of Biological Sciences, The University of Hong
            Kong, Pokfulam Road, Hong Kong, Hong Kong SAR, People’s Republic of China

            D.K. Gupta (ed.), Plant-Based Remediation Processes, Soil Biology 35,  159
            DOI 10.1007/978-3-642-35564-6_9, # Springer-Verlag Berlin Heidelberg 2013
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