Within the front end of the nuclear fuel cycle, many processes impart forensic signatures. Oxygen-stable isotopes (δ 18 O values) of uranium-bearing materials have been theorized to provide the processing and geolocational signatures of interdicted materials. However, this signature has been minimally utilized due to a limited understanding of how oxygen isotopes are influenced during uranium processing. This study explores oxygen isotope exchange and fractionation between magnesium diuranate (MDU), ammonium diuranate (ADU), and uranyl fluoride (UO 2 F 2 ) with steam (water vapor) during their reduction to UO x . The MDU was precipitated from two water sources, one enriched and one depleted in 18 O. The UO 2 F 2 was precipitated from a single water source and either directly reduced or converted to ADU prior to reduction. All MDU, ADU, and UO 2 F 2 were reduced to UO x in a 10% hydrogen/90% nitrogen atmosphere that was dry or included steam. Powder X-ray diffraction (p-XRD) was used to verify the composition of materials after reduction as mixtures of primarily U 3 O 8 , U 4 O 9 , and UO 2 with trace magnesium and fluorine phases in UO x from MDU and UO 2 F 2 , respectively. The bulk oxygen isotope composition of UO x from MDU was analyzed using fluorination to remove the lattice-bound oxygen, and then O 2 was subsequently analyzed with isotope ratio mass spectrometry (IRMS). The oxygen isotope compositions of the ADU, UO 2 F 2, and the resulting UO x were analyzed by large geometry secondary ion mass spectrometry (LG-SIMS). When reduced with steam, the MDU, ADU, and UO 2 F 2 experienced significant oxygen isotope exchange, and the resulting δ 18 O values of UO x approached the values of the steam. When reduced without steam, the δ 18 O values of converted ADU, U 3 O 8 , and UO x products remained similar to those of the UO 2 F 2 starting material. LG-SIMS isotope mapping of F impurity abundances and distributions showed that direct steam-assisted reduction from UO 2 F 2 significantly removed F impurities while dry reduction from UO 2 F 2 led to the formation of UO x that was enhanced in F impurities. In addition, when UO 2 F 2 was processed via precipitation to ADU and calcination to U 3 O 8 , F impurities were largely removed, and reductions to UO x with and without steam each had low F impurities. Overall, these findings show promise for combining multiple signatures to predict the process history during the conversion of uranium ore concentrates to nuclear fuel.