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hopeite

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Journal Article
Published: 01 October 2013
American Mineralogist (2013) 98 (10): 1893–1898.
...); 3.424(52)(240,221); 2.873(100)(241); 2.644(36)(400,331); 2.540(33)(420,161,002); and 1.953(36)(281). Nizamoffite is isostructural with hopeite. The structure ( R 1 = 1.7% for 1014 F o > 4σ F ) contains corner-sharing zigzag chains of ZnO 4 tetrahedra along [001]. The chains are connected by corner...
FIGURES | View All (4)
Journal Article
Published: 01 July 2007
American Mineralogist (2007) 92 (7): 1038–1047.
...Paul F. Schofield; Kevin S. Knight; Mark E. Hodson; Anna M. Lanfranco Abstract The lattice parameters extracted from Lebail analysis of neutron powder diffraction data collected between 2 and 300 K have been used to calculate the temperature evolution of the thermal expansion tensor for hopeite, Zn...
FIGURES | View All (8)
Journal Article
Published: 01 June 1991
The Canadian Mineralogist (1991) 29 (2): 337–345.
Journal Article
Published: 01 October 1976
American Mineralogist (1976) 61 (9-10): 987–995.
Image
The crystal structures of hopeite and parahopeite: (a) hopeite projected onto (010); (b) hopeite projected onto (001); hydrogen bonds are omitted for clarity; (c) parahopeite projected onto (010); (d) parahopeite projected onto (001). (Znϕ4) tetrahedra and (Znϕ6) octahedra are shadow-shaded.
Published: 01 January 2002
Figure 11. The crystal structures of hopeite and parahopeite: (a) hopeite projected onto (010); (b) hopeite projected onto (001); hydrogen bonds are omitted for clarity; (c) parahopeite projected onto (010); (d) parahopeite projected onto (001). (Znϕ 4 ) tetrahedra and (Znϕ 6 ) octahedra
Image
Hydrogen bonding in nizamoffite, α-hopeite, and β-hopeite. Hydrogen bonds are shown as thin black lines. The gray spheres are the octahedrally coordinated cations and the bonds to the O atoms surrounding them are shown as sticks. Oxygen atoms in the nizamoffite structure are labeled with numbers and H atoms with letters as appropriate.
Published: 01 October 2013
Figure 4 Hydrogen bonding in nizamoffite, α-hopeite, and β-hopeite. Hydrogen bonds are shown as thin black lines. The gray spheres are the octahedrally coordinated cations and the bonds to the O atoms surrounding them are shown as sticks. Oxygen atoms in the nizamoffite structure are labeled
Image
SEM image of a spray of bright blue-green zincolibethenite crystals on colourless platy hopeite crystals, Kabwe, Zambia. Z = zincolibethenite, H = hopeite.
Published: 01 April 2005
F ig . 1. SEM image of a spray of bright blue-green zincolibethenite crystals on colourless platy hopeite crystals, Kabwe, Zambia. Z = zincolibethenite, H = hopeite.
Journal Article
Published: 01 June 2012
Mineralogical Magazine (2012) 76 (3): 603–612.
...F. Neuhold; U. Kolitsch; H.-J. Bernhardt; C. L. Lengauer Abstract Arsenohopeite, ideally Zn 3 (AsO 4 ) 2 ·4H 2 O, is the arsenate analogue of hopeite, Zn 3 (PO 4 ) 2 ·4H 2 O (it is isostructural with α-hopeite). It was found as a single colourless to blue crystalline grain from the Tsumeb mine...
FIGURES
Image
Diffraction data (crosses) from the 90° detector bank of HRPD, their calculated fits (solid lines) difference curve and calculated reflection positions (vertical tick marks) for hopeite at 2 K collected for 400 μAh (top), hopeite at 50 K collected for 10 μAh (middle) and zinc phosphate dihydrate at 380 K collected for 20 μAh (bottom).
Published: 01 July 2007
F igure 3. Diffraction data (crosses) from the 90° detector bank of HRPD, their calculated fits (solid lines) difference curve and calculated reflection positions (vertical tick marks) for hopeite at 2 K collected for 400 μAh (top), hopeite at 50 K collected for 10 μAh (middle) and zinc
Journal Article
Published: 01 April 2005
Mineralogical Magazine (2005) 69 (2): 145–153.
...F ig . 1. SEM image of a spray of bright blue-green zincolibethenite crystals on colourless platy hopeite crystals, Kabwe, Zambia. Z = zincolibethenite, H = hopeite. ...
FIGURES
Journal Article
Published: 01 December 1940
American Mineralogist (1940) 25 (12): 787–809.
...C. W. Wolfe Abstract This family is composed of the triclinic group—parahopeite and anapaite; the monoclinic member—phosphophyllite; and the orthorhombic member—hopeite. The relations between the unit cells of phosphophyllite and hopeite are simple and are given in the description of the former...
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DTA and TG profile of deuterated α-hopeite with a heating rate of 10 K/min.
Published: 01 July 2007
F igure 1. DTA and TG profile of deuterated α-hopeite with a heating rate of 10 K/min.
Image
Zn K-edge XANES from (top) hopeite and (middle) bonemeal reacted with Zn in solution, and (bottom) a bonemeal particle from within the treated Parys Mountain soil.
Published: 01 February 2008
F ig . 2. Zn K-edge XANES from (top) hopeite and (middle) bonemeal reacted with Zn in solution, and (bottom) a bonemeal particle from within the treated Parys Mountain soil.
Image
Infrared absorption spectra for deuterated and protonated α-hopeite in the region 4000 to 1300 cm−1 (top) showing the internal modes of the H2O/D2O molecules and in the region 1200 to 400 cm−1 (bottom) showing the internal modes of the phosphate molecules and librational modes (R) of the H2O/D2O molecules.
Published: 01 July 2007
F igure 2. Infrared absorption spectra for deuterated and protonated α-hopeite in the region 4000 to 1300 cm −1 (top) showing the internal modes of the H 2 O/D 2 O molecules and in the region 1200 to 400 cm −1 (bottom) showing the internal modes of the phosphate molecules and librational
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Variation of the lattice parameters of hopeite within the temperature range 2 ≤ T ≤ 300 K. The calculated fits (solid lines) are represented by Einstein functions for a, c, and V, and by an empirical logistic function for b.
Published: 01 July 2007
F igure 4. Variation of the lattice parameters of hopeite within the temperature range 2 ≤ T ≤ 300 K. The calculated fits (solid lines) are represented by Einstein functions for a , c , and V , and by an empirical logistic function for b .
Image
Representation of the crystal structure of hopeite after Whitaker (1975). (a) The tetrahedral sheet comprising layers of PO4 tetrahedra and 1 layer of ZnO4 tetrahedra. The filled tetrahedra are PO4, tetrahedral Zn are small shaded circles, the O atoms of the water molecules are larger, darker filled circles and the protons are white. (b) The layer of ZnO6 octahedra between the tetrahedral sheets with PO4 represented by filled tetrahedra, the Zn atoms are small shaded circles, the O atoms of the water molecules are larger, darker filled circles and the protons are white.
Published: 01 July 2007
F igure 6. Representation of the crystal structure of hopeite after Whitaker (1975) . ( a ) The tetrahedral sheet comprising layers of PO 4 tetrahedra and 1 layer of ZnO 4 tetrahedra. The filled tetrahedra are PO 4 , tetrahedral Zn are small shaded circles, the O atoms of the water molecules
Image
Variation of the lattice parameters of the hopeite subhydrate Zn3(PO4)2·2H2O within the temperature range 335 ≤ T ≤ 480 K. The calculated fits are empirically represented by a quadratic of the form X = X0 + dT + fT2 where X0 represents the 0 K cell parameter value and d and f are constants.
Published: 01 July 2007
F igure 7. Variation of the lattice parameters of the hopeite subhydrate Zn 3 (PO 4 ) 2 ·2H 2 O within the temperature range 335 ≤ T ≤ 480 K. The calculated fits are empirically represented by a quadratic of the form X = X 0 + dT + fT 2 where X 0 represents the 0 K cell parameter
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Reflectance spectra of Pb and Zn ‘phosphate’ minerals: 1, hopeite;2, scholzite; 3, tarbuttite;4, pyromorphite; 5, parahopeite;6, veszelyite.
Published: 01 May 2007
Fig. 4 Reflectance spectra of Pb and Zn ‘phosphate’ minerals: 1, hopeite;2, scholzite; 3, tarbuttite;4, pyromorphite; 5, parahopeite;6, veszelyite.
Journal Article
Published: 20 May 2024
Mineralogical Magazine (2024) 88 (5): 576–584.
... of the paulkerrite group, from the Hagendorf-Süd pegmatite, Oberpfalz, Bavaria, Germany. It was found in corrosion pits of altered zwieselite, in association with columbite, hopeite, leucophosphite, mitridatite, scholzite, orange–brown zincoberaunite sprays and tiny green crystals of zincolibethenite. Sperlingite...
FIGURES | View All (7)
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Temperature dependence of the thermal expansion tensor coefficients, α11, α22, and α33, of hopeite as calculated from the mathematical fits of the lattice parameters.
Published: 01 July 2007
F igure 5. Temperature dependence of the thermal expansion tensor coefficients, α 11 , α 22 , and α 33 , of hopeite as calculated from the mathematical fits of the lattice parameters.