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介孔二氧化硅中深度冷冻水的重新取向:孔径依赖性的核磁共振研究

Reorientation of Deeply Cooled Water in Mesoporous Silica: NMR Studies of the Pore-Size Dependence.

作者信息

Weigler M, Brodrecht M, Buntkowsky G, Vogel M

机构信息

Institut für Festkörperphysik , Technische Universität Darmstadt , Hochschulstr. 6 , 64289 Darmstadt , Germany.

Eduard-Zintl-Institut für Anorganische und Physikalische Chemie , Technische Universität Darmstadt , Alarich-Weiss-Str. 8 , 64287 Darmstadt , Germany.

出版信息

J Phys Chem B. 2019 Mar 7;123(9):2123-2134. doi: 10.1021/acs.jpcb.8b12204. Epub 2019 Feb 25.

Abstract

We apply H NMR to investigate water reorientation in mesoporous silica. Using synthesized MCM-41 and purchased SBA-15 materials, we systematically study the dependence on the pore diameter. For a characterization of the properties of the silica matrices, scanning electron microscopy and nitrogen gas adsorption are employed. To ascertain the thermodynamic behavior of the confined water, we utilize differential scanning calorimetry. The dynamical properties are analyzed in a broad temperature range from the weakly to the deeply cooled regime using a combination of H spin-lattice relaxation and stimulated-echo experiments. We find that the reorientation of confined water is governed by prominent heterogeneity. The peak correlation time τ of the distribution is independent of the pore diameter in a range of ca. 2-6 nm. It shows a dynamical crossover at ∼220 K in all studied confinements, including wide silica pores where the effect occurs below T and, hence, in the two-phase region with coexisting liquid and solid water fractions. Above and below the no-man's land of water, the pore-size-independent correlation times τ of confined water are consistent with those of the bulk liquid, suggesting that we probe a dynamical process that is a characteristic feature of water. We argue that none of the proposed origins of the dynamical crossover is fully consistent with all observations and discuss possible new directions.

摘要

我们应用氢核磁共振((^1H\ NMR))来研究介孔二氧化硅中的水重取向。使用合成的MCM - 41和购买的SBA - 15材料,我们系统地研究了其对孔径的依赖性。为了表征二氧化硅基质的性质,采用了扫描电子显微镜和氮气吸附法。为了确定受限水的热力学行为,我们使用了差示扫描量热法。利用(^1H)自旋 - 晶格弛豫和受激回波实验的组合,在从弱冷却到深度冷却的宽温度范围内分析动力学性质。我们发现受限水的重取向受显著的非均质性支配。分布的峰值相关时间(\tau)在约2 - 6纳米的范围内与孔径无关。在所有研究的受限体系中,包括宽二氧化硅孔(在该体系中,这种效应在低于(T)时出现,即在液态水和固态水共存的两相区域),它在约220 K处表现出动力学转变。在水的“无人区”之上和之下,受限水的与孔径无关的相关时间(\tau)与本体液体的一致,这表明我们探测到了一个作为水的特征的动力学过程。我们认为,所提出的动力学转变的起源均不能完全与所有观测结果一致,并讨论了可能的新方向。

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