“…), where it accumulates and remains attached to the surface of mineral grains. This microorganism is an anaerobic, nitrate-dependent bacterium that rapidly uses the Fe(II) content of natural sediments as an electron donor under anoxic conditions and nitrate as the electron acceptor (Achenbach et al, 2001) to produce mixed-valence Fe(II)-Fe(III) byproduct precipitates, which are unstable iron minerals that correspond to green rusts (Chaudhuri et al, 2001;Lack et al, 2002;Weber et al, 2006;Nam et al;. Studies by different authors have confirmed the abiotic reductive dechlorination process of CT in the presence of green rusts (Liang and Butler, 2010;Yin et al, 2017), which are common natural electron donors in aquifers (Matocha, Dhakal and Pyzola, 2012) The high geological heterogeneity in the TZBA, with the presence of numerous interbedded layers of silty-clays, sands, and gravels with variable fine matrix content in this unit (see Section 4.1), accounts for the high textural heterogeneity observed, with abundant textural contrasts between fine and coarse materials.…”