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质子交换同成分铌酸锂晶体中示踪剂扩散与氢含量的关系

Tracer diffusion in proton-exchanged congruent LiNbO crystals as a function of hydrogen content.

作者信息

Dörrer Lars, Heller René, Schmidt Harald

机构信息

Clausthaler Zentrum für Materialtechnik, Technische Universität Clausthal, Leibnizstraße 9, 38678 Clausthal-Zellerfeld, Germany.

Institut für Metallurgie, AG Mikrokinetik, Technische Universität Clausthal, Robert-Koch-Straße 42, 38678 Clausthal-Zellerfeld, Germany.

出版信息

Phys Chem Chem Phys. 2022 Jul 6;24(26):16139-16147. doi: 10.1039/d2cp01818g.

Abstract

The proton-exchange process is an effective method of fabricating low-loss waveguides based on LiNbO crystals. During proton-exchange, lithium is replaced by hydrogen and LiHNbO is formed. Currently, mechanisms and kinetics of the proton-exchange process are unclear, primarily due to a lack in reliable tracer diffusion data. We studied lithium and hydrogen tracer diffusion in proton-exchanged congruent LiNbO single crystals in the temperature range between 130-230 °C. Proton-exchange was done in benzoic acid with 0, 1, 2, or 3.6 mol% lithium benzoate added, resulting in micrometre thick surface layers where Li is substituted by H with relative fractions between = 0.45 and 0.85 as determined by Nuclear Reaction Analysis. For the diffusion experiments, ion-beam sputtered isotope enriched LiNbO was used as a Li tracer source and deuterated benzoic acid as a H tracer source. Isotope depth profile analysis was carried out by secondary ion mass spectrometry. From the experimental results, effective diffusivities governing the lithium/hydrogen exchange as well as individual hydrogen and lithium tracer diffusivities are extracted. All three types of diffusivities can be described by the Arrhenius law with an activation enthalpy of about 1.0-1.2 eV and increase as a function of hydrogen content nearly independent of temperature. The effective diffusivities and the lithium tracer diffusivities are identical within a factor of two to five, while the hydrogen diffusivities are higher by three orders of magnitude. The results show that the diffusion of Li is the rate determining step governing the proton-exchange process. Exponential dependencies between diffusivities and hydrogen concentrations are determined. The observed increase of Li tracer diffusivities and effective diffusivities as a function of hydrogen concentration is attributed to a continuous reduction of the migration enthalpy of diffusion by a maximum factor of about 0.2 eV. Simulations based on the determined diffusivities can reproduce the step-like profile of hydrogen penetration during proton-exchange.

摘要

质子交换过程是一种基于铌酸锂晶体制造低损耗波导的有效方法。在质子交换过程中,锂被氢取代并形成LiHNbO。目前,质子交换过程的机理和动力学尚不清楚,主要原因是缺乏可靠的示踪扩散数据。我们研究了在130 - 230°C温度范围内质子交换的同成分铌酸锂单晶中锂和氢的示踪扩散。质子交换在添加了0、1、2或3.6 mol%苯甲酸锂的苯甲酸中进行,形成了微米厚的表面层,通过核反应分析确定其中锂被氢取代的相对分数在 = 0.45至0.85之间。对于扩散实验,离子束溅射的同位素富集铌酸锂用作锂示踪剂源,氘代苯甲酸用作氢示踪剂源。通过二次离子质谱进行同位素深度剖析分析。从实验结果中,提取了控制锂/氢交换的有效扩散率以及单个氢和锂示踪剂扩散率。所有三种类型的扩散率都可以用阿伦尼乌斯定律描述,活化焓约为1.0 - 1.2 eV,并且几乎与温度无关地随氢含量增加。有效扩散率和锂示踪剂扩散率在二到五倍的范围内相同,而氢扩散率高三个数量级。结果表明,锂的扩散是控制质子交换过程的速率决定步骤。确定了扩散率与氢浓度之间的指数依赖关系。观察到的锂示踪剂扩散率和有效扩散率随氢浓度的增加归因于扩散迁移焓最大约0.2 eV的持续降低。基于确定的扩散率进行的模拟可以重现质子交换过程中氢渗透的阶梯状分布。

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