“…The biotransformation of N, Fe and Mn is tightly coupled in the sub‐surface environment (Chu et al, 2015; Luther, Sundby, Lewis, Brendel, & Silverberg, 1997; Vandenabeele, Beer, Germonpré, Sande, & Verstraete, 1995), and the principal parameters and major functional microbial species for their biotransformation have been investigated in some studies (Boano et al, 2015; Ellis, Bouchard, & Lantagne, 2000; Konopka, Plymale, Carvajal, Lin, & McKinley, 2013; Mermillod‐Blondin, Mauclaire, & Montuelle, 2005; Tekerlekopoulou & Vayenas, 2007). Many iron‐oxidizing bacteria (IOB) and manganese‐oxidizing bacteria (MnOB), including Pseudomonas , Leptothrix , Gallionella , Streptomyces , Toxothrix and Crenothrix , have been reported (Li et al, 2013; Mckee, Vance, & Karthikeyan, 2016; Tekerlekopoulou, Vasiliadou, & Vayenas, 2006; Yang, Li, Chu, Ren, & Zhang, 2014). Moreover, the appearance of ammonium‐oxidizing bacteria (AOB) ( Nitrosomonas and Nitrosococcus ) and nitrite‐oxidizing bacteria (NOB) ( Nitrospira ) demonstrated that nitrification occurred during the transformation of ammonium and nitrite, respectively (Rivett, Buss, Morgan, Smith, & Bemment, 2008; Sheibley, Duff, Jackman, & Triska, 2003).…”