“…28,30,56 Laboratory derived isotope trends are typically examined using the Rayleigh equation: δ 13 C -δ 13 C 0 ≈ εln(C/ C 0 ), where δ 13 C -δ 13 C 0 is the carbon isotope separation, for example, between TCE at time t and time zero, ε is the process-dependent bulk enrichment factor: (α−1)10 3 , and C/C 0 is the fraction of reactant remaining at time t. Thus, in batch studies bulk enrichment factors are determined by linear regression of δ 13 C -δ 13 C 0 versus ln(C/C 0 ) and this approach has shown promise for discriminating biotic and abiotic degradation pathways and for estimating the extent of TCE degradation. 27,28,30,31,56 Applying this method at PRB sites is challenging because multiple degradation processes are possible (so a unique value of ε cannot be assumed) and C 0 may vary widely in heterogeneous systems, e.g., in cases where influent TCE concentrations are not constant in time or space. We estimated C/C 0 by computing the molar ratio [TCE/(TCE+cis-DCE+VC +ethene+ethane)] in samples collected within and down-gradient of the PRB, assuming that measured daughter product concentrations correlate with the amount of degraded TCE and that concentrations of daughter products entering the PRB were negligible.…”