A Carbone-Stabilized Two-Coordinate Phosphorus(III)-Centered Dication
作者:Madelyn Qin Yi Tay、Yunpeng Lu、Rakesh Ganguly、Dragoslav Vidović
DOI:10.1002/anie.201209223
日期:2013.3.11
coordinatively unsaturated dicationic phosphorus compound has been synthesized and characterized (see structure; P pink, N blue, C gray). DFT calculations revealed that the polycation should show superior Lewis acid and σ‐donor properties to the corresponding bis(dimethylamino)phosphenium cations. Preliminary investigations with PMe3 confirmed unusual reactivity patterns for the dication.
Hoffmann, G. G., Zeitschrift fur Anorganische und Allgemeine Chemie
作者:Hoffmann, G. G.
DOI:——
日期:——
A solid-state NMR study of aluminum Lewis acid adducts with trimethylphosphine in zeolite Y: magic angle spinning sideband analysis of dipolar and J-coupled multiplet system
作者:Po Jen Chu、A. De Mallmann、Jack H. Lunsford
DOI:10.1021/j100172a047
日期:1991.9
The adsorption of trimethylphosphine (TMP) on a mixture consisting of a H-Y zeolite and aluminum chloride results in AlCl3-P(CH3)3 coordination complexes which exists as a family of structures with different stoichiometries. These complexes have been characterized by Al-27 and P-31 solid-state NMR. Two significant phases are formed with AlCl3:(CH3)3P ratios of 1:1 and 1:2. In the 1:1 adduct the aluminum is tetrahedrally coordinated and is directly bonded to phosphorus. The 1:2 adduct involves P-Al-P type bonding as suggested by the P-31 NMR sideband line shape and multiplet structure. Here aluminum is likely to be fivefold coordinated with trigonal-bipyramidal geometry (D3h). The two trimethylphosphine molecules are believed to be trans axial. From an analysis of the sample spinning sidebands multiplet, the Al-P distances were found to be 2.58 +/- 0.02 angstrom for the 1:1 complex and 2.96 +/- 0.02 angstrom for the 1:2 complex. These values are in good agreement with values obtained from crystal structure studies of the individual phases. From a comparison of samples with different TMP loadings, it is concluded that an equilibrium can be established between these two major phases in the presence of a H-Y zeolite, in a manner similar to that which occurs in the solution phase or in the solid state.