scholarly journals Charge flipping of spontaneous polarization in vapour-deposited films of small polar organic molecules

Author(s):  
Georgios M. Tourlakis ◽  
Sotirios Alexandros T. Adamopoulos ◽  
Irini K. Gavra ◽  
Alexandros A. Milpanis ◽  
Liveria F. Tsagri ◽  
...  

Films of polar molecules vapour-deposited on sufficiently cold substrates are not only amorphous, but also exhibit charge polarization across their thickness. This is an effect known for 50 years, but...

2019 ◽  
Vol 116 (9) ◽  
pp. 3419-3424
Author(s):  
Tian Zhou ◽  
Santanu Malakar ◽  
Steven L. Webb ◽  
Karsten Krogh-Jespersen ◽  
Alan S. Goldman

The insertion of CO into metal-alkyl bonds is the key C-C bond-forming step in many of the most important organic reactions catalyzed by transition metal complexes. Polar organic molecules (e.g., tetrahydrofuran) have long been known to promote CO insertion reactions, but the mechanism of their action has been the subject of unresolved speculation for over five decades. Comprehensive computational studies [density functional theory (DFT)] on the prototypical system Mn(CO)5(arylmethyl) reveal that the polar molecules do not promote the actual alkyl migration step. Instead, CO insertion (i.e. alkyl migration) occurs rapidly and reversibly to give an acyl complex with a sigma-bound (agostic) C-H bond that is not easily displaced by typical ligands (e.g. phosphines or CO). The agostic C-H bond is displaced much more readily, however, by the polar promoter molecules, even though such species bind only weakly to the metal center and are themselves then easily displaced; the facile kinetics of this process are attributable to a hydrogen bonding-like interaction between the agostic C-H bond and the polar promoter. The role of the promoter is to thereby catalyze isomerization of the agostic product of CO insertion to give an η2-C,O-bound acyl product that is more easily trapped than the agostic species. This ability of such promoters to displace a strongly sigma-bound C-H bond and to subsequently undergo facile displacement themselves is without reported precedent, and could have implications for catalytic reactions beyond carbonylation.


2019 ◽  
Vol 123 (40) ◽  
pp. 8505-8511 ◽  
Author(s):  
Alexandra N. Pilidi ◽  
Irini K. Gavra ◽  
Athanassios A. Tsekouras

1981 ◽  
Vol 59 (16) ◽  
pp. 2518-2529 ◽  
Author(s):  
Claude Treiner

The salting effect of polar molecules in aqueous electrolyte solutions has been examined in the case of 22 solute molecules. It is observed that the salting constants of polar and nonpolar molecules of the same size in a given salt solution are close to each other and are generally greater than a critical diameter of the solute molecules. Using the available data from the literature, the salting constants ks of neutral polar molecules by univalent cation electrolytes has been classified in three groups: (1) Organic molecules and inorganic salts: for a given electrolyte ks is a monotonous function of the solute size and the nonelectrolyte dipole moment plays no role. (2) Organic molecules and organic salts: again a smooth variation of ks with size is observed whatever the polar mono-functional molecule. (3) Inorganic molecules and inorganic salts: a correlation is exhibited between ks and the solute dipole moment. These observations may be interpreted by assuming that both ends of a dipole are to be available to solute + solvent interactions for a dipole effect to be observed.Furthermore it is shown that in case 1, the scaled-particle theory with incorporation of a preferential solvation phenomenon may be useful for predicting salting out effects of polar molecules in inorganic salt solutions. In case 2 an approach based on microscopic surface tension and molecular surface area is also considered.


Author(s):  
W. W. Barker ◽  
W. E. Rigsby ◽  
V. J. Hurst ◽  
W. J. Humphreys

Experimental clay mineral-organic molecule complexes long have been known and some of them have been extensively studied by X-ray diffraction methods. The organic molecules are adsorbed onto the surfaces of the clay minerals, or intercalated between the silicate layers. Natural organo-clays also are widely recognized but generally have not been well characterized. Widely used techniques for clay mineral identification involve treatment of the sample with H2 O2 or other oxidant to destroy any associated organics. This generally simplifies and intensifies the XRD pattern of the clay residue, but helps little with the characterization of the original organoclay. Adequate techniques for the direct observation of synthetic and naturally occurring organoclays are yet to be developed.


Author(s):  
S. Herd ◽  
S. M. Mader

Single crystal films in (001) orientation, about 1500 Å thick, were produced by R-F sputtering of Al + 4 wt % Cu onto cleaved KCl at 150°C substrate temperature. The as-deposited films contained numerous θ-CuAl2 particles (C16 structure) about 0.1μ in size. They were transferred onto Mo screens, solution treated and rapidly cooled (within about ½ min) so as to retain a homogeneous solid solution. Subsequently, the films were aged in vacuum at various temperatures in order to induce precipitation and to compare structures and morphologies of precipitate particles in Al-Cu films with those found in age hardened bulk material.Aging for 3 weeks at 60°C or 48 hrs at 100°C did not produce any detectable change in high resolution micrographs or diffraction patterns. In this range Guinier-Preston zones (GP) form in quenched bulk material. The absence of GP in the present experiments in this aging range is perhaps due to the cooling rate employed, which might be more equivalent to an aged and reverted bulk material than to a quenched one.


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