Calcium
oxalate minerals are broadly present in nature. They form
through biogenic, geogenic, and pathogenic processes that lead to
different pseudopolymorphs.
Being the most common solid phase in human nephrolithiasis, calcium
oxalate monohydrate (COM) in particular has been the focus of much
investigation. It exists in several crystalline forms, two of which
appear to be of biological and medical relevance: the low- and high-temperature
forms (COM-LT and COM-HT, respectively). While there is broad consensus
on the ordered structure of COM-LT, which possesses the P21/n space group symmetry, for COM-HT
controversy remains. Experimental results suggest that there is a
certain degree of structural disorder in the high-temperature form.
However, the exact character of disorder in COM-HT is yet an open
question. Here, we examine the effect of the disorder of water molecules
on the structure of COM using first-principles calculations based
on dispersion-augmented density functional theory. Such calculations
allow for controlled examination of specific disorder features and
their effect on crystal structure and stability. On the basis of our
first-principles analysis, we suggest that in COM-HT each water dimer
site is randomly occupied by any of four water dimer arrangements
present in COM-LT, leading to statistical 2/m point
symmetry at each site and a statistical I2/m space group symmetry