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Schwertmannite is a poorly crystalline nanometric iron sulfate oxyhydroxide. This mineral shows a structural variability under different environments. Because of that, the determination of its structure and, consequently, of its physical–chemical properties is quite challenging. This article presents a detailed structural investigation of the structure of schwertmannite conducted under different approaches: X-ray absorption spectroscopy, Rietveld refinement, and a combined reverse Monte Carlo and Debye function analysis of the whole nanoparticle structure. The schwertmannite model presented here is, to the auhors' knowledge, the most complete model so far reported.

Supporting information

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Text file https://doi.org/10.1107/S160057671701336X/po5094sup1.txt
Structure of the whole Bigham particle after RMC refinement for the sample SynHT

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Text file https://doi.org/10.1107/S160057671701336X/po5094sup2.txt
Structure of the whole goethite particle after RMC refinement for the sample SynHT

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Text file https://doi.org/10.1107/S160057671701336X/po5094sup3.txt
Structure of the whole Bigham particle after RMC refinement for the sample Nat-Freeze

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Text file https://doi.org/10.1107/S160057671701336X/po5094sup4.txt
Structure of the whole goethite particle after RMC refinement for the sample Nat-Freeze

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Portable Document Format (PDF) file https://doi.org/10.1107/S160057671701336X/po5094sup5.pdf
Supplementary material


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