Structures of the monohydrate and dihydrate of (bidentate pyrophosphato) trans-diammine cis-diaqua chromium (III)

(OC-6-32)-Diamminediaqua [pyrophosphato(3-)]chromium(III) monohydrate, [Cr(NH3)2-(H2O)2(HP2O7)]. H2O, Mr = 315.1, triclinic, P1, a = 7.127 (2), b = 8.390 (2), c = 9.619 (2) A, alpha = 72.14 (2), beta = 98.86 (2), gamma = 76.98 (3) degrees, V = 517.7 (3) A3, Z = 2, Dx = 2.02 g cm-3, lambda(Cu K alpha) = 1.5418 A, mu = 129 cm-1, F(000) = 322, T = 293 K. (OC-6-32)-Diamminediaqua[pyrophosphato(3-)]-chromium(III) dihydrate, 0.5( [Cr(NH3)2(H2O)2-(HP2O7)].2H2O), Mr = 0.5(333.1), monoclinic, C2/m, a = 13.118 (3), b = 12.101 (3), c = 7.436 (2) A, beta = 105.09 (2) degrees, V = 1139.7 (3) A3, Z = 8, Dx = 1.94 g cm-3, lambda(Cu K alpha) = 1.5418 A, mu = 118 cm-1, F(000) = 684, T = 293 K. The structures were solved by the multi-solution technique and refined by the method of least squares to yield a final R index of 0.057 for 986 reflections in the monohydrate and a final R index of 0.043 for 1030 reflections in the dihydrate. The six-membered chromium pyrophosphate chelate ring is in a boat conformation for the monohydrate with an intramolecular hydrogen bond between an ammonia proton and a pyrophosphate O atom. In the dihydrate, the chelate ring is bisected by the mirror plane resulting in an unusual planar chelate ring conformation which does not permit intramolecular hydrogen bonding.

Biotransformation of intracellular minerals by zinc ions in vivo and in vitro

Inorganic granules of the general type CaMgP2O7 are found within cells of a wide range of species. The granules are amorphous to X-rays and occur in membrane-bound compartments. They accumulate a variety of cations from the body fluids of these animals. The interaction of zinc ions with pyrophosphate granules from cells of the snail Helix aspersa have been studied in vivo and in vitro by X-ray absorption spectroscopy and X-ray diffraction. The in vivo deposits incorporate zinc and remain amorphous although the pyrophosphate is hydrolysed to orthophosphate. In this in vitro reaction the mineral becomes crystalline but there is little change in the form of the The results clearly indicate a role for the cellular system in maintaining the amorphous state and in the hydrolysis of pyrophosphate to orthophosphate. As such they provide a model system for some of the changes observed in precursors of bone mineral and in pathological changes in the calcification of cartilage.

[High-molecular polyphosphates and pyrophosphate in cyclosporin- producing Tolypocladium sp. and their role in the processes of growth and antibiotic synthesis]

The contents of high-energy phosphorous compounds, i.e. three fractions of polyphosphates, pyrophosphate, and ATP were determined in isogenic strains of Tolypocladium sp. differing in cyclosporine production levels. The content of polyphosphates was 1 to 2 orders of magnitude greater than that of pyrophosphate or ATP and did not depend on the strain productivity. During the period of the mycelial intensive growth and at the beginning of antibiotic synthesis, the level of polyphosphates lowered 2-3-fold and the content of pyrophosphate markedly decreased as well. The activities of polyphosphatase and pyrophosphatase during the culture growth and cyclosporine biosynthesis was higher in the highly productive strain.

Effects of inorganic orthophosphate and pyrophosphate on dissolution of calcium fluoride in water

Calcium and fluoride release from excess solid calcium fluoride was monitored for 15-30 min in aqueous solutions containing various concentrations of inorganic orthophosphate and pyrophosphate. Low concentrations of these ions (1-10 mumol/L) considerably inhibited the rate of dissolution of calcium fluoride. This inhibition was pH-dependent, being reduced at pH values below 5. It is suggested that a reduced calcium fluoride dissolution rate, in the presence of phosphate, can account for the relatively slow loss of calcium fluoride from dental enamel observed in recent clinical studies. It also appears that calcium fluoride coated with phosphate may provide a pH-controlled slow release of fluoride that may be of clinical significance and a major component of the cariostatic mechanism of topically applied fluoride.

Imidodiphosphate and Pyrophosphate: Possible Biological Significance of Similar Structures

The structure of sodium imidodiphosphate has been determined by single crystal x-ray diffraction. The P-N-P bond angle (127.2 degrees) and P-N bond distance (1.68 angstroms) are remarkably similar to newly refined values for the P-O-P bond angle (128.6 degrees) and the bridging P-O bond distance (1.63 angstroms) of sodium pyrophosphate. This close similarity may explain why P-N-P linkages in algal "polyphosphates" escaped detection until recently and why adenosine triphosphate analogs with this linkage mimic adenosine triphosphate so closely.