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首页> 外文期刊>Russian journal of physical chemistry, B. >Kinetics and mechanism of the leaching of sodium from A-terskite and its influence on ion-exchange properties
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Kinetics and mechanism of the leaching of sodium from A-terskite and its influence on ion-exchange properties

机译:从钠钙钛矿中浸出钠的动力学,机理及其对离子交换性能的影响

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摘要

NMR (23)Na spectroscopy, conductometry, calorimetry, and EDs electron microprobe are used to study the ion mobility, the kinetics of the leaching of sodium and the influence of the leaching on the ion-exchange properties of A-terskite (H (x) Na(4 - x) ZrSi(6)O(15)(OH)(2) center dot H(2)O), a natural microporous material with a high selectivity with respect to Cs(+). The leaching of Na(+) ions by water is preceded by their transition into a mobile state in the zeolite channels of the sorbent. Over the temperature range of 20 to 90A degrees C, the kinetics of leaching at the initial stage is limited by diffusion in the liquid phase, becoming of dispersion character at late stages. The activity of A-terskite in the process of ion exchange with Cs(+) increases with the degree of leaching.
机译:使用NMR(23)Na光谱,电导法,量热法和EDs电子微探针研究离子迁移率,钠浸出的动力学以及浸出对A-三水铝矾石(H(x )Na(4-x)ZrSi(6)O(15)(OH)(2)中心点H(2)O),是一种天然微孔材料,对Cs(+)具有高选择性。 Na(+)离子被水浸出之前,会先在吸附剂的沸石通道中将其转变为可移动状态。在20到90A摄氏度的温度范围内,初始阶段的浸出动力学受到液相扩散的限制,后期则变为分散特性。 A-白钨矿在与Cs(+)离子交换过程中的活性随浸出程度的增加而增加。

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