Samples of pure aragonite are synthesized by precipitation from aqueous sol
ution and used to determine the heat capacity and temperature dependence of
the unit cell parameters in the temperature range 291-700 K. The X-ray dif
fraction powder diagram at room temperature is refined in space group Pnma
and resulted in the cell parameters a = 5.7444(8) Angstrom, b = 4.9620(4) A
ngstrom, c = 7.9700(6) Angstrom, and V = 227.17(3) Angstrom(3). TRXD allows
the study of the thermal expansion of the lattice up to the phase transiti
on to the stable calcite which occurs at 723 K. anisotropic expansion coeff
icients are computed in the temperature ranges 291-700 K and 800-900 K for
aragonite and calcite, respectively. From heat capacity measurements and hi
gh pressure compressibility data from the literature, some elastic coeffici
ents of aragonite and calcite, particularly those of the Gruneisen type, ar
e reexamined. (C) 1999 Academic Press.