Acid mine drainage (AMD) affects the mobility of naturally occurring radioactive materials (NORM), but its influence on the distribution of U- and Th-series radionuclides in polymetallic mining districts and downstream estuaries remains poorly understood. Here, we characterize the spatial evolution and isotopic signatures of U- and Th-series radionuclides in the dissolved fraction along the Oraque–Meca–Odiel river–estuary system (SW Spain). This system shows a strong geochemical gradient, from highly acidic AMD headwaters (locally pH < 3; high sulfate and metal concentrations) through weakly acidic reaches (pH ≈ 4.5) to near-neutral estuarine waters (pH ≈ 7). 238 U and 232 Th activity concentrations were strongly enriched in AMD-impacted headwaters, reaching values in the order of 10 3 and 10 2 mBq L −1 , respectively, with 238 U exceeding global riverine background by more than two orders of magnitude. PHREEQC modeling indicated that modeled aqueous U(VI) was dominated by free uranyl and uranyl-sulfate species under strongly acidic conditions. In contrast, dissolved 232 Th decreased more strongly than U as pH increased, producing a clear U Th geochemical decoupling. This pattern is consistent with the generally higher particle reactivity of Th reported in previous studies and suggests transfer from the dissolved phase during downstream evolution. 234 U/ 238 U ratios were generally >1, indicating isotopic disequilibrium and preferential 234 U mobilization. The 230 Th/ 232 Th activity ratios remained close to unity, indicating limited isotopic fractionation within the dissolved Th pool. These results show that the spatial variations of dissolved U and Th across the investigated river-estuary system coincided with hydrochemical gradients and changing source contributions, while the selected confluences showed nominal element-specific departures from the adopted sulfate-based mixing predictions.
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