The stable isotope ratios of C-bonded H (δ2Hn values) can be used to locate soil samples for forensic purposes because of their close correlation with the δ2H values of precipitation. Post-sampling bacterial activity might change the δ2Hn values via glycolysis. We tested to which degree C-bonded H is replaced by H from ambient water under favorable and unfavorable growing conditions. We provided two heterotrophic bacteria (Bacillus atrophaeus, Escherichia coli) with glucose (favorable) or lysine (unfavorable) under aerobic conditions. We assessed the H incorporation from ambient water via 2H labeling. We found that the H incorporation into bacterial biomass in the glucose treatment was 79 ± 5.9% (B. atrophaeus) and 43 ± 3.0% (E. coli), likely as a consequence of glycolysis and conservation of the δ2H value in the anabolic mode of the tricarboxylic acid (TCA) cycle. Differences between species were possibly related with different compositions of metabolite mixtures. The bacteria did hardly grow with lysine while respiration continued, and we found no H incorporation because the catabolic mode of the TCA cycle, which was active when the bacteria grew on lysine, is associated with CO2 release and a complete cleavage of former C–2H bonds. Our results support the glycolysis pathway as a mechanism underlying the incorporation of ambient-water H into the C-bonded H pool of bacteria. Stressful conditions forcing bacteria into a catabolism-dominated metabolism disable the incorporation of ambient-water H, and δ2Hn values can be applied to identify the origin of soil samples in forensics.