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Theoretical investigation of the water/corundum (0001) interface

机译:水/刚玉(0001)界面的理论研究

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For the reliable long-term modeling of the actinide migration in geological formations, theadsorption/desorption properties and the reactivity of mineral surfaces must be understood at themolecular level. The adsorption of radioisotopes at mineral surfaces of the aquifer is an importantprocess that leads to the retention of contaminants such as radionuclides. Their transport by theground water is either retarded or even completely inhibited by the presence of such a surface.Accordingly, this subject is of main importance for the safety assessment of nuclear wasterepositories. As part' of a joint theoretical/experimental effort, the interaction of water with thecorundum (0001) surface is studied using several theoretical methods (Moller–Plesset perturbationtheory, coupled cluster singles doubles with triplet corrections, as well as density functional theory).We focus in this study on the determination of the bond lengths and tilt angles of the surface OHspecies and their respective vibrational frequencies. The theoretical results are confirmed bysubsequent simulation of the interface selective nonlinear sum frequency spectra. The excellentagreement of the simulated with the experimental spectra allows an assignment of the observedpeaks in the sum frequency spectra of the water/corundum (0001) interface on the basis of ourtheoretical data. In this theoretical study we are able to give a unique interpretation of the observedsum frequency spectra of the water/corundum (0001) interface
机译:为了对act系元素在地质构造中的迁移进行可靠的长期建模,必须在分子水平上理解矿物表面的吸附/解吸特性和反应性。放射性同位素在含水层矿物表面的吸附是一个重要的过程,可导致污染物如放射性核素的保留。这种表面的存在阻碍了它们在地下水中的运输,甚至被完全抑制。因此,这个问题对于核废料库的安全评估至关重要。作为联合理论/实验工作的一部分,使用几种理论方法(Moller-Plesset摄动理论,耦合三重态校正的偶合簇单重体以及密度泛函理论)研究了水与刚玉(0001)表面的相互作用。本研究的重点是确定表面OH物种的键长和倾斜角以及它们各自的振动频率。随后对界面选择性非线性和频谱的仿真结果证实了理论结果。模拟物与实验光谱的优异一致性允许根据我们的理论数据在水/刚玉(0001)界面的总光谱中分配观察到的峰。在这项理论研究中,我们能够对水/刚玉(0001)界面的观测和频谱做出独特的解释

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