114 research outputs found

    Fast Track Communication

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    Abstract Photoionization of Mg 3s is studied near the Cooper minimum in dipole channels using the relativistic-random-phase approximation. While the importance of first-order nondipole effects on photoelectron angular distributions at low energies is well known, it is reported here for the first time that in the energy region near the dipole Cooper minimum, quadrupole transitions are not just important, but actually dominate the total photoionization cross section. Studies of dipole-dipole, dipole-quadrupole and quadrupole-quadrupole interference terms in the photoelectron angular distribution show that in the region of dipole Cooper minimum even the calculation of the dipole angular distribution parameter, β, requires the inclusion of quadrupole channels. The significance of second-order [O(k 2 r 2 )] nondipole terms, primarily due to the contributions from electric quadrupole-quadrupole interference terms at photon energy as low as ∼11 eV, are shown to induce dramatic changes in the photoelectron angular distribution over a small energy range

    A theoretical study on the formation of iodine oxide aggregates and monohydrates

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    Biotic and abiotic emissions of molecular iodine and iodocarbons from the sea or the ice surface and the intertidal zone to the coastal/polar marine boundary layer lead to the formation of iodine oxides, which subsequently nucleate forming iodine oxide particles (IOPs). Although the link between coastal iodine emissions and ultrafine aerosol bursts is well established, the details of the nucleation mechanism have not yet been elucidated. In this paper, results of a theoretical study of a range of potentially relevant aggregation reactions of different iodine oxides, as well as complexation with water molecules, are reported. Thermochemical properties of these reactions are obtained from high level ab initio correlated calculations including spin-orbit corrections. The results show that the nucleation path most likely proceeds through dimerisation of I2O4. It is also shown that water can hinder gas-to-particle conversion to some extent, although complexation with key iodine oxides does not remove enough of these to stop IOP formation. A consistent picture of this process emerges from the theoretical study presented here and the findings of a new laboratory study reported in the accompanying paper (Gomez Martin et al., 2013)

    Stereoelectronic effects and the kinetic acidities of diastereotopic hydrogens

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    A general qualitative treatment is proposed which accounts for the relative reactivities of diastereotopic hydrogens adjacent to a heteroatom in proton transfer, hydride transfer, and hydrogen atom transfer reactions. This treatment focuses on the structures of the reactive intermediates formed in such reactions, which can be predicted or understood in terms of qualitative molecular orbital arguments, and on the manner in which these intermediates will undergo readdition of H+, H\uaf, or H\ub7. The procedure has been tested, for the specific case of proton transfer reactions, by a direct computational approach to the energy differences between diastereomeric transition states of reactions HO\uaf + CH3X \u2192 H2O + \uafCH2X (X = sulfide, sulfoxide, sulfone, sulfonium). The computations support the qualitative treatment, and are in all cases in near quantitative agreement with the extensive experimental data concerning the diastereotopic selectivities exhibited in these systems.On propose une m\ue9thode qualitative g\ue9n\ue9rale qui tient compte des r\ue9activit\ue9s relatives des hydrog\ue8nes diast\ue9r\ue9otopiques adjacents \ue0 un h\ue9t\ue9roatome lors de r\ue9actions de transfert de protons, d'hydrures ou d'atomes d'hydrog\ue8ne. Cette m\ue9thode met l'accent \ue0 la fois sur la structure des interm\ue9diaires r\ue9actifs form\ue9s au cours de telles r\ue9actions, qui peuvent \ueatre pr\ue9vus ou compris en termes d'arguments qualitatifs d'orbitales mol\ue9culaires, et sur la fa\ue7on dont ces interm\ue9diaires peuvent subir une nouvelle addition de H+, H\uaf ou H\ub7. On a v\ue9rifi\ue9 cette m\ue9thode, dans le cas sp\ue9cifique de r\ue9actions de transfert de proton, par une technique de calculs directs des diff\ue9rences d'\ue9nergie entre les \ue9tats de transition diast\ue9r\ue9oisom\ue8res des r\ue9actions: HO\uaf + CH3X \u2192 H2O + \uafCH2X (X = sulfure, sulfoxyde, sulfone, sulfonium). Les calculs sont en accord avec l'approche qualitative et, dans tous les cas, ils sont aussi en accord quasi-quantitatif avec les donn\ue9es exp\ue9rimentales extensives relatives aux s\ue9lectivit\ue9s diast\ue9r\ue9otopiques observ\ue9es dans ces syst\ue8mes.NRC publication: Ye
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