“…The combined interpretation of solute concentrations and isotope ratios in sediment profiles and groundwater samples is a common approach to unravel natural transformations of nutrients and organic compounds, most prominently organic pollutants. − The interpretation relies on the phenomenon that kinetic isotope effects typically favor the transformation of molecules with light isotopes so that molecules with heavy isotopes become enriched in the remaining substrate. , Hence, an increase of isotope ratios, such as of 13 C/ 12 C or 15 N/ 14 N, along a transport path in groundwater or sediments can provide direct evidence of the natural transformation of a compound. This has been applied in the analysis of sulfate, , nitrate, and methane, among others, along with redox gradients and organic pollutants (e.g., BTEX, chlorinated ethenes, pesticides, and herbicides) − at contaminated sites. Conversely, the absence of isotope fractionation, despite a concentration decrease, is commonly interpreted as evidence of the absence of reactive turnover.…”