Journal
JOURNAL OF HAZARDOUS MATERIALS
Volume 181, Issue 1-3, Pages 193-203Publisher
ELSEVIER SCIENCE BV
DOI: 10.1016/j.jhazmat.2010.04.116
Keywords
Radioactivity; Chemical speciation; Morphology; Phosphate rock; Phosphogypsum
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Funding
- National Council of Science and Technology (CONACYT, Mexico)
- Seville University
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In this work, radiological, chemical, and also morphological characterization was performed in phosphate rock and phosphogypsum samples, in order to understand the behavior of toxic elements. Characterization was carried out using X-ray diffraction (XRD), X-ray fluorescence (XRF), gamma spectrometry and scanning electron microscopy with energy-dispersive X-ray analysis (SEM-EDX). Our results show that the phosphate rock was mainly composed of fluorapatite, calcite, perovskite, quartz, magnetite, pyrite and kaolinite, whereas phosphogypsum only exhibited dihydrated calcium sulfate. The activity concentration of U-series radioisotopes in phosphate rock was around 1640 Bq/kg. (226)Ra and (210)Pb tend to be distributed into phosphogypsum by up to 80%, whereas the fraction of U-isotopes is 10%. The most abundant trace elements in phosphate rock were Sr, Cr, V, Zn, Y, Ni and Ba. Some elements, such as Ba, Cd, Cu, La. Pb, Se, Sr, Th and Y, were enriched in the phosphogypsum. This enrichment may be attributed to an additional input associated to the sulfuric acid used for the phosphoric acid production. Furthermore, results from SEM-EDX demonstrated that toxic elements are not distributed homogeneously into phosphogypsum. Most of these elements are concentrated in particles <20 mu m of high porosity, and could be easily mobilized by leaching and/or erosion. (C) 2010 Elsevier B.V. All rights reserved.
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