文摘
This study investigates dual element isotope fractionation during aerobic biodegradation of 1,2-dichloroethane (1,2-DCA) via oxidative cleavage of a C鈥揌 bond (Pseudomonas sp. strain DCA1) versus C鈥揅l bond cleavage by SN2 reaction (Xanthobacter autotrophicus GJ10 and Ancylobacter aquaticus AD20). Compound-specific chlorine isotope analysis of 1,2-DCA was performed for the first time, and isotope fractionation (蔚bulkCl) was determined by measurements of the same samples in three different laboratories using two gas chromatography鈥搃sotope ratio mass spectrometry systems and one gas chromatography鈥搎uadrupole mass spectrometry system. Strongly pathway-dependent slopes (螖未13C/螖未37Cl), 0.78 卤 0.03 (oxidation) and 7.7 卤 0.2 (SN2), delineate the potential of the dual isotope approach to identify 1,2-DCA degradation pathways in the field. In contrast to different 蔚bulkC values [鈭?.5 卤 0.1鈥?(oxidation) and 鈭?1.9 卤 0.7 and 鈭?2.0 卤 0.9鈥?(SN2)], the obtained 蔚bulkCl values were surprisingly similar for the two pathways: 鈭?.8 卤 0.2鈥?(oxidation) and 鈭?.2 卤 0.1 and 鈭?.4 卤 0.2鈥?(SN2). Apparent kinetic isotope effects (AKIEs) of 1.0070 卤 0.0002 (13C-AKIE, oxidation), 1.068 卤 0.001 (13C-AKIE, SN2), and 1.0087 卤 0.0002 (37Cl-AKIE, SN2) fell within expected ranges. In contrast, an unexpectedly large secondary 37Cl-AKIE of 1.0038 卤 0.0002 reveals a hitherto unrecognized involvement of C鈥揅l bonds in microbial C鈥揌 bond oxidation. Our two-dimensional isotope fractionation patterns allow for the first time reliable 1,2-DCA degradation pathway identification in the field, which unlocks the full potential of isotope applications for this important groundwater contaminant.