首页> 外文会议>IUTAM(International Union of Theoretical and Applied Mechanics) Symposium on Physicochemical and Electromechanical Interactions in Porous Media; ; >NUMERICAL AND EXPERIMENTAL STUDIES OF THE WATER AND IONIC MOBILITIES WITHIN SUSPENSIONS OF CHARGED ANISOTROPIC COLLOIDS
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NUMERICAL AND EXPERIMENTAL STUDIES OF THE WATER AND IONIC MOBILITIES WITHIN SUSPENSIONS OF CHARGED ANISOTROPIC COLLOIDS

机译:悬浮带电各向异性胶体中水和离子迁移率的数值和实验研究

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摘要

We use Nuclear Magnetic Resonance relaxometry (i.e. the frequency variation of the NMR relaxation rates) of quadrupolar nucleus (~(23)Na) and ~1H Pulsed Gradient Spin Echo NMR to determine the mobility of the counterions and the water molecules within aqueous dispersions of clays. The local ordering of iso-tropic dilute clay dispersions is investigated by NMR relaxometry. In contrast, the NMR spectra of the quadrupolar nucleus and the anisotropy of the water self-diffusion tensor clearly exhibit the occurrence of nematic ordering in dense aqueous dispersions. Multi-scale numerical models exploiting molecular orbital quantum calculations, Grand Canonical Monte Carlo simulations, Molecular and Brownian Dynamics are used to interpret the measured water mobility and the ionic quadrupolar relaxation measurements.
机译:我们使用四极核(〜(23)Na)和〜1H脉冲梯度自旋回波NMR的核磁共振弛豫法(即NMR弛豫率的频率变化)来确定抗衡离子和水分子在水分散液中的迁移率黏土。通过NMR弛豫法研究各向同性稀粘土分散体的局部有序性。相反,四极核的NMR光谱和水自扩散张量的各向异性清楚地显示出在浓水分散体中向列有序的发生。利用分子轨道量子计算,大经典蒙特卡洛模拟,分子动力学和布朗动力学的多尺度数值模型来解释测得的水迁移率和离子四极弛豫测量值。

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