首页> 外文会议>Clay Minerals Society Annual Meeting >LARGE-SCALE MOLECULAR DYNAMICS SIMULATIONS OF METAL SORPTION ONTO BASAL SURFACES OF CLAY MINERALS
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LARGE-SCALE MOLECULAR DYNAMICS SIMULATIONS OF METAL SORPTION ONTO BASAL SURFACES OF CLAY MINERALS

机译:粘土矿物基部表面的大规模分子动力学模拟金属吸附

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摘要

Large-scale molecular dynamics computer simulations have been completed to evaluatethe sorption of cesium, strontium, and other related ions onto the basal surfaces of kaolinite andmontmorillonite. Simulations were undertaken as a function of metal ion concentration toevaluate sorption mechanisms and to determine distribution coefficients; K_d values are oftenincorporated in reactive transport models to predict contaminant transport. The molecularsimulations demonstrate that cesium ions bind to both kaolinite and montmorillonite surfaces,while strontium ions tend to remain in solution. At high solution concentrations (greater than 0.5M), cesium sorption occurs on both the tetrahedral and octahedral sheets of kaolinite.
机译:已经完成了大规模的分子动力学计算机模拟,以评估铯,锶和其他相关离子的吸附到高岭石和莫尔氏石的基础表面上。仿真作为金属离子浓度的函数进行,以进行吸附机制并确定分布系数; K_D值在无功运输模型中是通常的,以预测污染物运输。分子筛证明铯离子与高岭石和蒙脱石表面结合,而锶离子倾向于保留在溶液中。在高溶液浓度下(大于0.5米),在高岭石的四面体和八面体片上发生铯吸附。

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