| Reference Type | Journal (article/letter/editorial) |
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| Title | X-ray diffraction studies of vivianite, metavivianite, and barićite |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Sameshima, T. | Author |
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| Henderson, G. S. | Author |
| Black, P. M. | Author |
| Rodgers, K. A. | Author |
| Year | 1985 (March) | Volume | 49 |
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| Issue | 350 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_49/49-350-81.pdf+ |
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| DOI | doi:10.1180/minmag.1985.049.350.11Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 3700 | Long-form Identifier | mindat:1:5:3700:0 |
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| GUID | 0 |
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| Full Reference | Sameshima, T., Henderson, G. S., Black, P. M., Rodgers, K. A. (1985) X-ray diffraction studies of vivianite, metavivianite, and barićite. Mineralogical Magazine, 49 (350) 81-85 doi:10.1180/minmag.1985.049.350.11 |
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| Plain Text | Sameshima, T., Henderson, G. S., Black, P. M., Rodgers, K. A. (1985) X-ray diffraction studies of vivianite, metavivianite, and barićite. Mineralogical Magazine, 49 (350) 81-85 doi:10.1180/minmag.1985.049.350.11 |
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| In | (1985, March) Mineralogical Magazine Vol. 49 (350) Mineralogical Society |
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| Abstract/Notes | AbstractVivianite specimens from various world localities yield X-ray powder patterns of two types: one corresponds with that shown by synthetic Fe3(PO4)2 · 8H2O and is not readily distinguished from that of barićite; the second shows reflections of monoclinic vivianite and triclinic metavivianite along with reflections of a bobierrite-type phase. The triclinic phase occurs as two twin-related lattices with twin plane 110 being the structural equivalent of 010 in the monoclinic phase. The relationship of the bobierrite-type lattice to the other two has not been established. The ternary pattern is produced by some coarse-grained vivianites on natural oxidation. Finer grained vivianites oxidise to an X-ray amorphous state without passing through a triclinic intermediate. |
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