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paranatrolite

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Journal Article
Published: 01 January 2005
American Mineralogist (2005) 90 (1): 252–257.
...Yongjae Lee; Joseph A. Hriljac; John B. Parise; Thomas Vogt Abstract The origin and stability of paranatrolite (approximate formula Na 16– x Ca x Al 16+ x Si 24– x O 80 ·24H 2 O), a naturally occurring zeolite with the natrolite topology, has long been debated, with its detailed structure unknown...
FIGURES
Journal Article
Published: 01 May 2004
European Journal of Mineralogy (2004) 16 (3): 545–550.
...Yurii V. SERYOTKIN; Vladimir V. BAKAKIN; Igor A. BELITSKY Abstract Paranatrolite from the Khibiny massif, Kola Peninsula, Russia, Na 1.88 K 0.22 Ca 0.06 [Al 2.24 Si 2.76 O 10 ].3.1H 2 O, is monoclinic (space group Cc, Z = 4). For better comparison of this mineral with the related structure...
FIGURES
Journal Article
Published: 01 November 2000
American Mineralogist (2000) 85 (11-12): 1808–1815.
... sites and x varies from approximately 0.3 to 3.2. Tetranatrolite is a dehydration product of paranatrolite and probably does not have a true stability field. Further understanding of the paragenesis of tetranatrolite was given by Chao (1980) . He found that the overgrowths on some of the Mont Saint...
FIGURES
Journal Article
Published: 01 February 1980
The Canadian Mineralogist (1980) 18 (1): 85–88.
Journal Article
Published: 01 July 2007
European Journal of Mineralogy (2007) 19 (4): 593–598.
...Yurii V. Seryotkin; Vladimir V. Bakakin Abstract The problem of the reversibility of paranatrolite-tetranatrolite transformation is a key problem in understanding the paragenesis of the natrolite group zeolites. Two paranatrolite samples of different chemical composition were studied by X-ray...
FIGURES | View All (6)
Journal Article
Published: 01 February 2006
American Mineralogist (2006) 91 (2-3): 247–251.
...Yongjae Lee; Joseph A. Hriljac; John B. Parise; Thomas Vogt Abstract The tetranatrolite-paranatrolite transformation has remained a key problem in understanding the paragenesis of zeolites in the natrolite family. It is accepted that when paranatrolite, approximate formula Na 16− x Ca x Al 16+ x Si...
FIGURES
Journal Article
Published: 01 August 1992
American Mineralogist (1992) 77 (7-8): 685–703.
...Malcolm Ross; Marta J. K. Flohr; Daphne R. Ross Abstract The zeolite minerals of the natrolite group (natrolite, tetranatrolite, paranatrolite, mesolite, scolecite, thomsonite, gonnardite, edingtonite, and tetraedingtonite) have the general formula (Na,Ca,Ba) 8–16 (Al,Si) 40 O 80 · n H 2 O...
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Evolution of diffraction pattern for the sample Iversus temperature (bottom-up: heating from room temperature to 38 °C and subsequent cooling). Heating: monoclinic paranatrolite (a); monoclinic and tetragonal phases (b–d); tetragonal phase (e). Cooling: tetragonal phase (f); tetragonal and monoclinic phases (g–j); monoclinic paranatrolite after 24 hours in ambient conditions (k).
Published: 01 July 2007
Fig. 2. Evolution of diffraction pattern for the sample I versus temperature (bottom-up: heating from room temperature to 38 °C and subsequent cooling). Heating: monoclinic paranatrolite ( a ); monoclinic and tetragonal phases ( b–d ); tetragonal phase ( e ). Cooling: tetragonal phase ( f
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Published: 01 May 2004
Table 1. Crystal and experimental data of the paranatrolite structure.
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Published: 01 May 2004
Table 4. Na-O(Ow) and K-O(Ow) distances (Å) in paranatrolite.
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Published: 01 May 2004
Table 3. T-O bond lengths (Å) and T–O–T angles (°) in paranatrolite.
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A projection of the paranatrolite structure along [001]. A part of the alternative Ow60, Ow7, and K positions are shown by broken circles. The Ψ angle of the chain rotation is shown to the right.
Published: 01 May 2004
Fig. 1. A projection of the paranatrolite structure along [001]. A part of the alternative Ow60, Ow7, and K positions are shown by broken circles. The Ψ angle of the chain rotation is shown to the right.
Image
Coordination polyhedra of Na cations in the paranatrolite structure. (a) Trigonal O4(H2O)2 prisms typical for natrolite with the extra Na-Ow70 contacts; Na-O(Ow) distances are < 3.1 Å. (b) Octahedra O3(H2O)3, Ow7 positions are vacant; Na-O(Ow) distances are < 2.8 Å. (c) Octahedra O3(H2O)3, the alternative possibility - Ow60 positions are vacant.
Published: 01 May 2004
Fig. 2. Coordination polyhedra of Na cations in the paranatrolite structure. (a) Trigonal O 4 (H 2 O) 2 prisms typical for natrolite with the extra Na-Ow70 contacts; Na-O(Ow) distances are < 3.1 Å. (b) Octahedra O 3 (H 2 O) 3 , Ow7 positions are vacant; Na-O(Ow) distances are < 2.8 Å. (c
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Published: 01 May 2004
Table 5. Selected surroundings of H 2 O molecules and determined H bond lengths (Å) and angles (°) in paranatrolite.
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Published: 01 May 2004
Table 2. Atomic coordinates, equivalent isotropic displacement parameters U eq = 1/3 ∑ I (∑ j (U ij a i * a j * a i a j )) (Å 2 ) and occupancies for paranatrolite.
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Experimental (points) and calculated (line) diffraction profiles of the wetted sample II. The tick marks indicate the positions of allowed Bragg peaks for the paranatrolite structure, space group F1d1.
Published: 01 July 2007
Fig. 6. Experimental (points) and calculated (line) diffraction profiles of the wetted sample II . The tick marks indicate the positions of allowed Bragg peaks for the paranatrolite structure, space group F 1 d 1.
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Experimental (points) and calculated (line) diffraction profiles of the sample I in ambient conditions. The tick marks indicate the positions of allowed Bragg peaks for the paranatrolite structure, space group F1d1.
Published: 01 July 2007
Fig. 1. Experimental (points) and calculated (line) diffraction profiles of the sample I in ambient conditions. The tick marks indicate the positions of allowed Bragg peaks for the paranatrolite structure, space group F 1 d 1.
Journal Article
Published: 01 January 2005
American Mineralogist (2005) 90 (1): 247–251.
... at the framework T-sites. Paranatrolite is another natrolite analog with a high water content, Na 16– x Ca x Al 16+ x Si 24– x O 80 · n H 2 O or ideally Na 16 Al 16 Si 24 O 80 · n H 2 O, n ~ 24 ( Chao 1980 ; Ross et al. 1992 ). It is claimed to transform irreversibly to tetranatrolite upon exposure...
FIGURES | View All (5)
Journal Article
Published: 01 March 2005
European Journal of Mineralogy (2005) 17 (2): 305–313.
... such as natrolite Na 2 (H 2 O) 2 [Al 2 Si 3 O 10 ], mesolite Na 2 Ca 2 (H 2 O) 8 [Al 6 Si 9 O 30 ], scolecite Ca(H 2 O) 3 [Al 2 Si 3 O 10 ], and paranatrolite Na 2 K 0.25 (H 2 O) 3 [(Al,Si) 5 O 10 ], are characterized by a very flexible framework. This is clearly by the fact that “collapsed” dehydrated natrolite...
FIGURES | View All (5)
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Heat capacity of molecular H2O in various micro/nanoporous hydrous silicates and ice, liquid, and gaseous H2O: filled circles = cordierite, filled squares = analcime, filled triangles = mordenite, open circles = paranatrolite, plus signs = ice and liquid water, and open squares = gaseous H2O.
Published: 01 February 2007
F igure 8. Heat capacity of molecular H 2 O in various micro/nanoporous hydrous silicates and ice, liquid, and gaseous H 2 O: filled circles = cordierite, filled squares = analcime, filled triangles = mordenite, open circles = paranatrolite, plus signs = ice and liquid water, and open squares