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Figure 2
The 295 K Mössbauer spectra of eighteenth-century Prussian blue samples. The solid green and red lines represent the iron(II) and iron(III) doublets of Prussian blue, respectively. In four of the six spectra shown, ferrihydrite dominates, as is shown by the solid blue line, which corresponds to a ferrihydrite quadrupole doublet.

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SYNCHROTRON
RADIATION
ISSN: 1600-5775
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