Morphology and Optical Properties of Precipitated Vivianite, Fe3(PO4)2·8H2O

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Morphology and Optical Properties of Precipitated Vivianite, Fe3(PO4)2·8H2O. / Madsen, Hans Erik Lundager.

In: Journal of Crystal Growth, Vol. 55, No. 6, 1900226, 01.06.2020.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Madsen, HEL 2020, 'Morphology and Optical Properties of Precipitated Vivianite, Fe3(PO4)2·8H2O', Journal of Crystal Growth, vol. 55, no. 6, 1900226. https://doi.org/10.1002/crat.v55.6

APA

Madsen, H. E. L. (2020). Morphology and Optical Properties of Precipitated Vivianite, Fe3(PO4)2·8H2O. Journal of Crystal Growth, 55(6), [1900226]. https://doi.org/10.1002/crat.v55.6

Vancouver

Madsen HEL. Morphology and Optical Properties of Precipitated Vivianite, Fe3(PO4)2·8H2O. Journal of Crystal Growth. 2020 Jun 1;55(6). 1900226. https://doi.org/10.1002/crat.v55.6

Author

Madsen, Hans Erik Lundager. / Morphology and Optical Properties of Precipitated Vivianite, Fe3(PO4)2·8H2O. In: Journal of Crystal Growth. 2020 ; Vol. 55, No. 6.

Bibtex

@article{4057f619925746ddacc7f7a50c98233a,
title = "Morphology and Optical Properties of Precipitated Vivianite, Fe3(PO4)2·8H2O",
abstract = "Crystals of vivianite, Fe3(PO4)2∙8H2O, belonging to the monoclinic prismatic class 2/m , are grown by precipitation from aqueous solution at temperatures from 25 to 56 °C. At 25 °C aggregates are dominating, but at 35 °C and above single crystals are more common, being tabular along {010} and most often with parallelogram outline; in a few cases twins are observed. The outline is distinct and consistent with published lattice parameters, but at low temperature the {010} faces are very rough as judged from interference colors seen in the polarizing microscope. Lateral faces belonging to the {110} form are visible on crystals grown at 45 and 56 °C, and the widths of their projections on {010} as measured with a micrometer eyepiece served for estimating crystal thickness, making use of the face angle from lattice parameters. Optical parameters are determined by a combination of three methods: 1) measurement of birefringence with an Ehringhaus 6λ compensator, 2) Kamb's method for the optic axis angle determined by the angle‐of‐flight method in conoscopic illumination, and 3) visual interferometry using a polarizing microscope incorporating a Mach–Zehnder interference device. Reasonably precise values of principal refractive indices in the expected range are found.",
author = "Madsen, {Hans Erik Lundager}",
year = "2020",
month = jun,
day = "1",
doi = "10.1002/crat.v55.6",
language = "English",
volume = "55",
journal = "Journal of Crystal Growth",
issn = "0022-0248",
publisher = "Elsevier BV * North-Holland",
number = "6",

}

RIS

TY - JOUR

T1 - Morphology and Optical Properties of Precipitated Vivianite, Fe3(PO4)2·8H2O

AU - Madsen, Hans Erik Lundager

PY - 2020/6/1

Y1 - 2020/6/1

N2 - Crystals of vivianite, Fe3(PO4)2∙8H2O, belonging to the monoclinic prismatic class 2/m , are grown by precipitation from aqueous solution at temperatures from 25 to 56 °C. At 25 °C aggregates are dominating, but at 35 °C and above single crystals are more common, being tabular along {010} and most often with parallelogram outline; in a few cases twins are observed. The outline is distinct and consistent with published lattice parameters, but at low temperature the {010} faces are very rough as judged from interference colors seen in the polarizing microscope. Lateral faces belonging to the {110} form are visible on crystals grown at 45 and 56 °C, and the widths of their projections on {010} as measured with a micrometer eyepiece served for estimating crystal thickness, making use of the face angle from lattice parameters. Optical parameters are determined by a combination of three methods: 1) measurement of birefringence with an Ehringhaus 6λ compensator, 2) Kamb's method for the optic axis angle determined by the angle‐of‐flight method in conoscopic illumination, and 3) visual interferometry using a polarizing microscope incorporating a Mach–Zehnder interference device. Reasonably precise values of principal refractive indices in the expected range are found.

AB - Crystals of vivianite, Fe3(PO4)2∙8H2O, belonging to the monoclinic prismatic class 2/m , are grown by precipitation from aqueous solution at temperatures from 25 to 56 °C. At 25 °C aggregates are dominating, but at 35 °C and above single crystals are more common, being tabular along {010} and most often with parallelogram outline; in a few cases twins are observed. The outline is distinct and consistent with published lattice parameters, but at low temperature the {010} faces are very rough as judged from interference colors seen in the polarizing microscope. Lateral faces belonging to the {110} form are visible on crystals grown at 45 and 56 °C, and the widths of their projections on {010} as measured with a micrometer eyepiece served for estimating crystal thickness, making use of the face angle from lattice parameters. Optical parameters are determined by a combination of three methods: 1) measurement of birefringence with an Ehringhaus 6λ compensator, 2) Kamb's method for the optic axis angle determined by the angle‐of‐flight method in conoscopic illumination, and 3) visual interferometry using a polarizing microscope incorporating a Mach–Zehnder interference device. Reasonably precise values of principal refractive indices in the expected range are found.

U2 - 10.1002/crat.v55.6

DO - 10.1002/crat.v55.6

M3 - Journal article

VL - 55

JO - Journal of Crystal Growth

JF - Journal of Crystal Growth

SN - 0022-0248

IS - 6

M1 - 1900226

ER -

ID: 243428194