Simulated annealing structure solution of a new phase of dicalcium silicate Ca(2)SiO(4) and the mechanism of structural changes from alpha-dicalcium silicate hydrate to alpha(L)'-dicalcium silicate via the new phase.

A new phase of dicalcium silicate (Ca(2)SiO(4)) was formed by heating alpha-dicalcium silicate hydrate [alpha-Ca(2)(SiO(4)H)OH = alpha-C(2)SH] at temperatures of approximately 663-763 K, and it was transformed into alpha(L)'-Ca(2)SiO(4) (= alpha(L)'-C(2)S) above approximately 1193 K. The crystal structure of the new phase (hereafter called x-C(2)S) has been determined by simulated annealing and refined by the Rietveld method using synchrotron radiation powder diffraction data. The structure consists of isolated SiO(4) tetrahedra and a three-dimensional CaO(n) polyhedral network, forming a new structural type of dicalcium silicate. A structural change from alpha-C(2)SH to x-C(2)S is compelled by large displacements of SiO(4) tetrahedra, accompanied by dehydration, in the direction perpendicular to the two-dimensional Ca(O,OH)(n) polyhedral network in alpha-C(2)SH. With increasing temperature, sizes of CaO(n) polyhedra in x-C(2)S become too large to confine Ca atoms at the sixfold to eightfold coordination sites. Then the structure of x-C(2)S is transformed into alpha(L)'-C(2)S, having eightfold to tenfold coordination sites for the Ca atoms.

Ab initio structure determination of monoclinic 2,2-dihydroxymethylbutanoic acid from synchrotron radiation powder diffraction data: combined use of direct methods and the Monte Carlo method.

The crystal structure of 2,2-dihydroxymethylbutanoic acid (C(6)H(12)O(4)) in monoclinic form has been determined ab initio from synchrotron radiation powder diffraction data. Two O and five C atoms were first derived by direct methods. Two missing O atoms and one C atom were found by the Monte Carlo method without applying constraint to their relative positions. Positional and isotropic displacement parameters of these non-H atoms were refined by the Rietveld method. Molecules are linked by hydrogen bonds and they make sheet-like networks running parallel to the (010) plane. The Monte Carlo method is demonstrated to be a powerful tool for finding missing atoms in partially solved structure.

First results from the crystal structure analysis beamline at SPring-8.

Results from the first measurements at the crystal structure analysis beamline (BL02B1) at SPring-8 are presented. The capabilities of this beamline are also discussed.

A new powder diffractometer for synchrotron radiation with a multiple-detector system.

A new powder diffractometer for synchrotron radiation with six detector arms has been constructed. Five detector arms are attached radially at intervals of 25 degrees to the 2theta axis and form a multiple-detector system. Five scintillation counters coupled with flat Ge(111) crystal analyzers on the respective arms can simultaneously record the whole powder pattern divided into five segments, each with an equal 2theta span. The optics design is based on flat-specimen reflection geometry using a parallel beam. The intensity data are collected using a 2theta step-scan technique in asymmetric diffraction at a fixed incident angle. A sixth multi-purpose detector arm can be used in the conventional single-arm scan mode. It can be equipped with various kinds of analyzers such as long horizontal parallel slits, a fiat or channel-cut crystal analyzer, a receiving slit and a solid-state detector. Test operations of the multiple-detector system, conducted at the Photon Factory in Tsukuba, recorded a full width at half maximum of 0.022 degrees and a peak maximum intensity of more than 40000 counts s(-1) for the (111) reflection from Si powder. The whole powder pattern of Mg(2)SiO(4) over a 2theta range of 130 degrees could be step-scanned at a step interval of 0.004 degrees (2theta) in just 4 h. Results of whole-powder-pattern decomposition and Rietveld refinement of the Mg(2)SiO(4) pattern are given.

Long Horizontal Parallel Slits with 0.03 degrees Angular Resolution for Powder Diffraction Using Synchrotron Radiation.

Long horizontal parallel slits with angular apertures of 0.032 and 0.065 degrees were constructed for powder diffraction experiments with synchrotron radiation. They have been tested at the BL-4B experimental station at the Photon Factory by using a monochromated beam with a wavelength of 1.528 A. The horizontal parallel slits with the smaller aperture gave a full-width at half-maximum of 0.030 (1) degrees for the (200) reflection from CeO(2) and an intensity about one order of magnitude higher than that obtained with a receiving slit in the same angular resolution, demonstrating the finest horizontal parallel slits developed so far. The misalignment of the horizontal parallel slits does not affect the intensity whilst it shifts the Bragg-peak positions systematically.

Precision Lattice-Parameter Determination of (Mg,Fe)SiO3 Tetragonal Garnets.

The tetragonal garnet (Mg,Fe)SiO(3) is a high-pressure phase of pyroxene that is thought to be a major constituent of the earth's upper mantle. Its crystal structure is similar to that of cubic garnet, but it is slightly distorted to tetragonal symmetry so that its x-ray powder diffraction pattern shows a very small line splitting. A suite of tetragonal garnets with different compositions in the MgSiO(3)-rich portion of the MgSiO(3)-FeSiO(3) system was synthesized at about 20 gigapascals and 2000 degrees C. The lattice parameters a and c of quenched samples were determined by whole-powder-pattern decomposition analysis of Fe Kalpha x-ray powder diffraction data, which has the capacity to resolve to a high degree heavily overlapping reflections. It was found that the lattice parameters can be obtained from the following equations; a (in angstroms) = 11.516 + 0.088x and c (in angstroms) = 11.428 + 0.157x, where x, teh mole fraction of FeSiO(3), is 0.0