4.7 Article

Structural transition of Friedel's salt 3CaO•Al2O3•CaCl2•10H2O studied by synchrotron powder diffraction

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CEMENT AND CONCRETE RESEARCH
卷 32, 期 4, 页码 513-519

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PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/S0008-8846(01)00716-5

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crystal structure; X-ray diffraction; synchrotron radiation; chloride; Friedel's salt; structural transition

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The structural phase transition occurring in Friedel's salt, the chlorinated compound 3CaO.Al2O3.CaCl2.10H(2)O (AFm phase), was studied by synchrotron and standard X-ray powder diffraction. The compound transforms at 35 degreesC from a rhombohedral (rh) high-temperature (HT) phase [R-3c; a=5.744(2) Angstrom, c=46.890(3) Angstrom] to a monoclinic (m) low-temperature (LT) phase [C2/c; a=9.960(4) Angstrom, b=5.7320(2) Angstrom, c =16.268(7) Angstrom, beta =104.471(2)degrees]. The LT and HT phases were refined with the Rietveld method from synchrotron data recorded at 20 and 40 degreesC. Variations of the lattice parameters as a function of temperature are reported between 8 and 48 degreesC. The rh --> m transition is characterized by a unit cell volume expansion of 1% and a movement of the interlayer species: a shift of 0.45 Angstrom of the Cl- anions along [010](h) and a shift of 0.25 Angstrom of the water molecules along [210](h) of the hexagonal cell. The m phase distortion is due to an ordering of the hydrogen bonds between chloride anions and H-atoms of the water molecules. (C) 2002 Elsevier Science Ltd. All rights reserved.

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