Current
approaches are often limited to evaluating the contribution
of pesticide dissipation processes in water–sediment systems
as both degradation and phase transfer, that is, sorption–desorption,
contribute to the apparent decrease of pesticide concentration. Here,
the dissipation of widely used herbicides acetochlor and S-metolachlor was examined in laboratory by water–sediment
microcosm experiments under oxic and anoxic conditions. Compound-specific
isotope analysis (CSIA) emphasized insignificant carbon isotope fractionation
in the sediment, indicating prevailing pesticide degradation in the
water phase. Conceptual modeling accounting for phase transfer and
biodegradation indicated that biodegradation may be underestimated
when phase transfer is not included. Phase transfer does not affect
carbon isotope fractionation for a wide spectrum of molecules and
environmental conditions, underscoring the potential of pesticide
CSIA as a robust approach to evaluate degradation in water–sediment
systems. CSIA coupled with the identification of transformation products
by high-resolution tandem mass spectrometry suggests the degradation
of acetochlor and S-metolachlor to occur via nucleophilic
substitution and the predominance of oxalinic acids as transformation
products under both anoxic and oxic conditions. Altogether, combining
the pesticide CSIA, the identification of transformation products,
and the use of conceptual phase-transfer models improves the interpretation
of pesticide dissipation in water–sediment systems.