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用于沸石孔隙率分析的NLDFT吸附模型,特别关注使用氧和氢的超微孔沸石。

NLDFT adsorption models for zeolite porosity analysis with particular focus on ultra-microporous zeolites using O and H.

作者信息

Jagiello Jacek, Kenvin Jeffrey

机构信息

Micromeritics Instrument Corporation, Norcross, GA 30093, USA.

Micromeritics Instrument Corporation, Norcross, GA 30093, USA.

出版信息

J Colloid Interface Sci. 2022 Nov;625:178-186. doi: 10.1016/j.jcis.2022.06.044. Epub 2022 Jun 11.

Abstract

The most often used gases for the PSD characterization of zeolites are N and Ar. According to the IUPAC Technical Report (2015), Ar is recommended as more reliable than N, which molecules possess a significant quadrupole moment that may influence the adsorption isotherms on polar surfaces. In practice, however, using Ar as a cryogen for Ar adsorption measurements is not preferred due to its higher cost than liquid N. We propose using O which has a much lower quadrupole moment than N, and its adsorption can be measured using standard liquid N as a coolant. To support using O, we demonstrate good agreement between the PSDs calculated from O and Ar adsorption. In the present work, we develop several semiempirical models based on nonlocald density functional theory (NLDFT) for the PSD characterization of several types of zeolites. We discuss the underlying difficulties in modeling gas adsorption on zeolites which adsorption potential field depends on both the pore width and the chemical structure of the zeolite. For the analysis of ultra microporous zeolites such as Chabazite and molecular sieve 5A, we apply H in combination with O at 77 K. H molecule has a smaller diameter than O and diffuses faster into ultra micropores, reducing the time of isotherm measurement. Moreover, we show that the dual gas analysis method can be used with O isotherms measurements omitting low-pressure points, making the analysis faster.

摘要

用于沸石颗粒大小分布(PSD)表征的最常用气体是氮气和氩气。根据国际纯粹与应用化学联合会(IUPAC)技术报告(2015年),推荐使用氩气,因为它比氮气更可靠,氮气分子具有显著的四极矩,可能会影响极性表面上的吸附等温线。然而,在实际应用中,由于氩气的成本高于液氮,因此不建议将其用作氩吸附测量的制冷剂。我们建议使用氧气,其四极矩比氮气低得多,并且可以使用标准液氮作为冷却剂来测量其吸附情况。为了支持使用氧气,我们证明了通过氧气和氩气吸附计算得到的颗粒大小分布之间具有良好的一致性。在本工作中,我们基于非局部密度泛函理论(NLDFT)开发了几个半经验模型,用于几种类型沸石的颗粒大小分布表征。我们讨论了在模拟沸石上气体吸附时的潜在困难,其吸附势场取决于沸石的孔径和化学结构。对于菱沸石和5A分子筛等超微孔沸石的分析,我们在77K下将氢气与氧气结合使用。氢分子的直径比氧分子小,扩散到超微孔中的速度更快,从而减少了等温线测量的时间。此外,我们表明双气体分析方法可用于氧气等温线测量,省略低压点,从而使分析更快。

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