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Influence of Hydronium Ions in Zeolites on Sorption

机译:盐酸盐脉对沸石对吸附的影响

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摘要

In the presence of sufficient concentrations of water, stable, hydrated hydronium ions are formed in the pores and at the surface of solid acids such as zeolites. For a medium-pore zeolite, such as zeolite MFI, hydrated hydronium ions consist of eight water molecules and have an effective volume of 0.24 nm(3). In their presence, larger organic molecules can only adsorb in the portions of the pore that are not occupied by hydronium ions. As a consequence, the available pore volume decreases proportionally to the concentration of the hydronium ions. The higher charge density (the increasing ionic strength) that accompanies an increasing concentration of hydronium ions leads to an increase in the activity coefficients of the adsorbed substrates, thus, weakening the interactions between the organic part of the molecules and the zeolite and favoring the interactions with polar groups. The quantitative understanding of these interactions makes it possible to link a collective property such as hydrophilicity and hydrophobicity of zeolites to specific interactions on molecular level.
机译:在存在足够的水浓度的水中,在孔中形成稳定的水合氢离子,并且在沸石如沸石的固体酸表面上形成。对于中孔沸石,例如沸石MFI,水合的氢化氢离子由八个水分子组成,具有0.24nm(3)的有效体积。在它们存在下,较大的有机分子只能吸收不被纳温离子占据的孔的部分。结果,可用的孔体积与纳温离子的浓度成比例地降低。伴随着含有氢化氢离子浓度的较高的电荷密度(不断增加的离子强度)导致吸附的基材的活性系数的增加,从而削弱了分子的有机部分与沸石之间的相互作用并有利于相互作用与极性群体。对这些相互作用的定量理解使得可以将沸石的亲水性和疏水性的集体性质联系起来与分子水平的特异性相互作用。

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