Radical-based dephosphorylation and organophosphonate biodegradation
作者:J. W. Frost、S. Loo、M. L. Cordeiro、D. Li
DOI:10.1021/ja00241a039
日期:1987.4
Products resulting from the degradation of organophosphonates by Escherichia coli are identified and used as a basis for evaluating mechanisms which may be the chemical basis of the biodegradation. One mechanistic hypothesis which is consistent with the biodegradation products involves radical-based dephosphorylation. Chemical modeling of this process is achieved by the reaction of alkylphosphonic
Catalytic recruitment by phosphonyl derivatives as inactivators of acetylcholinesterase and substrates for imidazole-catalyzed hydrolysis: .beta.-deuterium isotope effects
作者:Andrew J. Bennet、Ildiko M. Kovach、Jeffrey A. Bibbs
DOI:10.1021/ja00198a067
日期:1989.8
Neutron powder diffraction study of the layer organic–inorganic hybrid iron(II) methylphosphonate-hydrate, Fe[(CD3PO3)(D2O)]
作者:Philippe Léone、Carlo Bellitto、Elvira M. Bauer、Guido Righini、Gilles André、Françoise Bourée
DOI:10.1016/j.jssc.2008.07.032
日期:2008.11
The crystal and magnetic structures of the hybrid organic-inorganic layer compound Fe[(CD3PO3)(D2O)] have been studied by neutron powder diffraction as a function of temperature down to 1.5 K. The neutron diffraction pattern recorded at 200 K shows that the fully deuterated compound crystallizes in one of the two known forms of the undeuterated Fe[(CH3PO3)(H2O)]. The crystal structure is orthorhombic, space group Pmn2(1), with the following unit-cell parameters: a = 5.7095(1) angstrom, b = 8.8053(3) angstrom and c = 4.7987(1) angstrom; Z = 2. The crystal structure remains unchanged on cooling from 200 to 1.5K Moreover, at low temperature, Fe[(CD3PO3)(D2O)] shows a commensurate magnetic structure (k = (0,0,0)). As revealed by bulk susceptibility measurements oil Fe[(CH3PO3)(H2O)] the magnetic structure corresponds to a canted antiferromagnet with a critical temperature T-N = 25 K. Neutron powder diffraction reveals that below T-N = 23.5 K the iron magnetic moments in Fe[(CD3PO3D2O)] are antiferromagnetically coupled and oriented along the b-axis, perpendicular to the inorganic layers. No ferromagnetic component is observable in the neutron powder diffraction experiment, due to its too small value (<0.1 mu(B)). (C) 2008 Elsevier Inc. All rights reserved.
FROST J. W.; LOO S.; CORDEIRO M. L.; LI D., J. AMER. CHEM. SOC., 109,(1987) N 7, 2166-2171