“…Other iron solids present in water distribution pipes, such as hematite, magnetite, ilmenite, and green rusts can also serve as a source of ferrous iron for Cr(VI) reduction (Loyaux-Lawniczak et al, 2000;Kiyak et al, 1999;Khaodhiar, 1997;Peterson et al, 1997a;Peterson et al, 1997b;Peterson, 1996;White & Peterson, 1996;Eary & Rai, 1989;Anderson et al, 1984). Cr(VI) can also be reduced by many reduced sulfur compounds, including thiols (Szulczewski et al, 2001), iron sulfide (Kim et al, 2001;Patterson et al, 1997;Zouboulis et al, 1995), metabisulfite (Patterson et al, 1994), sodium sulfide and sodium sulfite (Lai & McNeill, 2006;Brandhuber et al, 2004), and hydrogen sulfide (Kim et al, 2001;Pettine et al, 1998a) as well as stannous chloride (Lai & McNeill, 2006;Brandhuber et al, 2004), ascorbic acid (Xu et al, 2004), and a variety of organic compounds (Buerge & Hug, 1998;Hug et al, 1997;Deng & Stone, 1996;Wittbrodt & Palmer, 1996;Wittbrodt & Palmer, 1995;Popov et al, 1992;James & Bartlett, 1983;Bartlett & Kimble, 1976;Schroeder & Lee, 1975). Cr(VI) can also be reduced under aerobic and anaerobic conditions by microbes; this can involve direct reduction by Cr-reducing bacteria as well as indirect reduction via production of hydrogen sulfide or ferrous iron by sulfate-reducing and iron-reducing bacteria, respec-tively (Boni & Sbaffoni, 2009;Somasundaram et al, 2009;Vainshtein et al, 2003;…”