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首页> 外文期刊>Clays and clay minerals >INTERACTION OF MAGNESIUM CATIONS WITH DIOCTAHEDRAL SMECTITES UNDER HLRW REPOSITORY CONDITIONS
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INTERACTION OF MAGNESIUM CATIONS WITH DIOCTAHEDRAL SMECTITES UNDER HLRW REPOSITORY CONDITIONS

机译:HLRW沉积条件下镁阳离子与二面体蒙脱石的相互作用

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In some real and up-scale tests using high-level radioactive waste (HLRW), Mg accumulation was observed in smectites at the contact of heated Fe or Cu metal tubes. It is important to understand why Mg accumulated in order to model the long term performance of bentonites in HLRW systems. In some of these tests, an increased number of trioctahedral domains was measured in the smectites using X-ray diffraction (XRD) and infrared spectroscopy (IR). The trioctahedral domains either formed by the dissolution/precipitation of smectites or by the addition of Mg through a solid-state reaction similar to the Hofmann-Klemen effect. The Hofmann-Klemen effect is used in the Greene-Kelly test to distinguish montmorillonites from beidellites. Many studies have been carried out about Li-uptake by smectites, but Mg was rarely taken into account. The present study was, therefore, undertaken to compare the interactions of different bentonites with Li and Mg under various conditions. A significant CEC decrease was found for Li- and Mg-saturated bentonite samples after heating at 250 degrees C under dry conditions. The extent of this CEC reduction depended on the octahedral to tetrahedral charge ratio and was smaller for Mg-saturated samples than Li-saturated samples. This finding proved that it is much more difficult for Mg to enter octahedral vacancies than Li, which probably can be explained by the larger hydration energy and/or slightly larger radius of Mg. The relationship between CEC reduction and the octahedral/tetrahedral charge ratio of both Li- and Mg-saturated samples, however, suggests a similar process. The Mg that can reside at the bottom of the pseudohexagonal holes would not explain this relationship. The important result with respect to understanding HLRW bentonite performance, on the other hand, is that Mg fixation only occurs under dry conditions and that Mg fixation acts as a sink for Mg and, hence, leads Mg to diffuse towards the heated metal surface.
机译:在一些使用高放废物(HLRW)的真实且大规模的测试中,在加热的Fe或Cu金属管的接触处,绿土中观察到Mg积累。重要的是要理解为什么镁会积聚,以模拟膨润土在HLRW系统中的长期性能。在其中一些测试中,使用X射线衍射(XRD)和红外光谱(IR)在绿土中测量到数量增加的三八面体域。通过与绿土的溶解/沉淀或通过类似于霍夫曼-克莱门效应的固态反应添加镁来形成三八面体域。霍夫曼-克莱门效应在格林-凯利检验中用于区分蒙脱石与贝得石。关于蒙脱石对锂的吸收已经进行了许多研究,但是很少考虑到镁。因此,本研究旨在比较不同条件下膨润土与Li和Mg的相互作用。在干燥条件下于250摄氏度加热后,发现锂和镁饱和膨润土样品的CEC显着降低。这种CEC降低的程度取决于八面体与四面体的电荷比,并且Mg饱和的样品比Li饱和的样品小。这一发现证明,Mg进入八面体空位要比Li困难得多,这可能可以用更大的水合能和/或稍大的Mg半径来解释。然而,Li和Mg饱和样品的CEC降低与八面体/四面体电荷比之间的关系表明了类似的过程。可以位于拟六角孔底部的Mg不能解释这种关系。另一方面,关于了解HLRW膨润土性能的重要结果是,Mg固定仅在干燥条件下发生,并且Mg固定充当Mg的吸收剂,因此导致Mg向加热的金属表面扩散。

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