Suppr超能文献

氟化铵掺杂对冰III至冰IX相变的影响。

Effect of ammonium fluoride doping on the ice III to ice IX phase transition.

作者信息

Sharif Zainab, Shephard Jacob J, Slater Ben, Bull Craig L, Hart Martin, Salzmann Christoph G

机构信息

Department of Chemistry, University College London, 20 Gordon Street, London WC1H 0AJ, United Kingdom.

ISIS Pulsed Neutron and Muon Source, Rutherford Appleton Laboratory, Harwell Oxford, Didcot OX11 0QX, United Kingdom.

出版信息

J Chem Phys. 2021 Mar 21;154(11):114502. doi: 10.1063/5.0032485.

Abstract

Ice III is a hydrogen-disordered phase of ice that is stable between about 0.2 and 0.35 GPa. Upon cooling, it transforms to its hydrogen-ordered counterpart ice IX within the stability region of ice II. Here, the effect of ammonium fluoride doping on this phase transition is investigated, which is followed for the first time with in situ neutron diffraction. The a and c lattice constants are found to expand and contract, respectively, upon hydrogen ordering, yielding an overall negative volume change. Interestingly, the anisotropy in the lattice constants persists when ice IX is fully formed, and negative thermal expansion is observed. Analogous to the isostructural keatite and β-spodumenes, the negative thermal expansion can be explained through the buildup of torsional strain within the a-b plane as the helical "springs" within the structure expand upon heating. The reversibility of the phase transition was demonstrated upon heating. As seen in diffraction and Raman spectroscopy, the ammonium fluoride doping induces additional residual hydrogen disorder in ice IX and is suggested to be a chemical way for the "excitation" of the configurational ice-rules manifold. Compared to ice VIII, the dopant-induced hydrogen disorder in ice IX is smaller, which suggests a higher density of accessible configurational states close to the ground state in ice IX. This study highlights the importance of dopants for exploring the water's phase diagram and underpins the highly complex solid-state chemistry of ice.

摘要

冰III是冰的一种氢无序相,在约0.2至0.35吉帕斯卡之间稳定。冷却时,它在冰II的稳定区域内转变为其氢有序对应物冰IX。在此,研究了氟化铵掺杂对这种相变的影响,首次采用原位中子衍射进行跟踪。发现氢有序时,a和c晶格常数分别膨胀和收缩,导致总体体积负变化。有趣的是,当冰IX完全形成时,晶格常数的各向异性仍然存在,并观察到负热膨胀。与同结构的透锂长石和β-锂辉石类似,负热膨胀可以通过结构中的螺旋“弹簧”在加热时膨胀,从而在a-b平面内产生扭转应变来解释。加热时证明了相变的可逆性。如在衍射和拉曼光谱中所见,氟化铵掺杂在冰IX中诱导了额外的残余氢无序,被认为是“激发”构型冰规则流形的一种化学方式。与冰VIII相比,掺杂剂在冰IX中诱导的氢无序较小,这表明冰IX中接近基态的可及构型态密度更高。这项研究突出了掺杂剂在探索水的相图方面的重要性,并支撑了冰的高度复杂的固态化学。

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验