Radionuclides and the uranium isotope fingerprint of globally produced phosphate rocks, mineral fertilizers, and phosphogypsum waste and its potential effect on the environment
- PMID: 41056715
- DOI: 10.1016/j.jhazmat.2025.140033
Radionuclides and the uranium isotope fingerprint of globally produced phosphate rocks, mineral fertilizers, and phosphogypsum waste and its potential effect on the environment
Abstract
The occurrence of uranium (U), thorium (Th), and radium (Ra) in phosphate rocks (PRs) leads to enrichment of these radionuclides in produced fertilizers and phosphogypsum waste byproducts. This study presents a global dataset of U- and Th- series radionuclides (238U, 232Th, 226Ra, and 228Ra) and uranium isotope composition (δ238U) in PRs, fertilizers, and phosphogypsum. Results reveal systematic variations in U and Ra content and δ238U signatures based on geological age and phosphate rock type (igneous vs sedimentary). Sedimentary PRs are in 238U-226Ra secular equilibrium, with younger rocks (Miocene-Permian) exhibiting higher 226Ra activities (up to 1837 Bq/kg) than older rocks (≤241 Bq/kg). Fertilizers tend to be concentrated in 238U and depleted in 226Ra relative to source rocks, while phosphogypsum retains 226Ra. In a survey of P- and NPK-fertilizers (i.e., fertilizers that contain a mix of nitrogen, phosphorus, and potassium), we find that fertilizers preserve the U isotope signature of the source phosphate rocks, with δ238U ranging between -0.28 ‰ and -0.15 ‰ for young PRs and -0.70 ‰ and -0.34 ‰ for older PRs, which are different from the average continental crust (-0.29 ‰). Field data from an agricultural research station in North Carolina demonstrate that, despite high U and Ra input rates from P-fertilizer application, surface sandy soils retain little of these radionuclides. Fertilization did not significantly alter soil δ238U and the U and Ra levels were low, below environmental safety thresholds. These findings highlight the potential of fertilizer-derived radionuclide contamination in adjacent or underlying water resources and offers the δ238U fingerprints of fertilizers as a potential geochemical tracer for identifying fertilizer-derived U contamination in the environment.
Keywords: Fertilizer; Isotopes; Phosphate; Phosphogypsum; Radium; Soil; Uranium.
Copyright © 2025 Elsevier B.V. All rights reserved.
Conflict of interest statement
Declaration of Competing Interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
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