z-logo
Premium
A New Calcium Oxalate Monohydrate Produced by Thermal Dehydration of Weddellite
Author(s) -
Schubert G.,
Ziemer B.
Publication year - 1981
Publication title -
kristall und technik
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.377
H-Index - 64
eISSN - 1521-4079
pISSN - 0023-4753
DOI - 10.1002/crat.19810160913
Subject(s) - orthorhombic crystal system , crystallography , chemistry , phase (matter) , materials science , crystal structure , organic chemistry
A high temperature‐Guinier photograph of weddellite power showed at 118 °C a transition to a so far unknown phase which transformed to β‐Ca(COO) 2 at 135 °C and during cooling down to whewellite at 103 °C. X‐ray diffraction studies on single crystals revealed the new phase to have an orthorhombic symmetry with the lattice constant a = 12.088 Å, b = 10.112 Å, c = 14.634 Å, α = β = γ = 90°. There are very simple orientation relations to weddellite: a 1 (wed) ∥ a (new phase), a 2 (wed) ∥ b (new phase), c (wed) ∥ c (new phase). DTA/TG studies showed that the new phase is a calcium oxalate monohydrate.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom