NIST Center for Neutron Research, National Institute of Standards and Technology, Gaithersburg, MD 20899, USA.
J Phys Condens Matter. 2012 Feb 15;24(6):064106. doi: 10.1088/0953-8984/24/6/064106. Epub 2012 Jan 25.
Using neutron diffraction, we have tracked the temperature dependence of structural properties for heavy water confined in the nanoporous silica matrix MCM-41-S. By observing the correlation peak corresponding to the pore-pore distance, which is determined by the scattering contrast between the silica and the water, we monitored the density of the confined water. Concurrently, we studied the prominent first diffraction peak of D(2)O at ≈ 1.8 Å(-1), which furnishes information on the microscopic arrangement of the water molecules. The data show the presence of a density maximum at ≈ 275 K (± 10 K), a property similar to bulk water, and the occurrence of a density minimum at ≈ 180 K (± 10 K). The prominent diffraction peak of D(2)O is found to shift and sharpen over a wide T range from 200 to 270 K, reflecting structural changes that are strongly correlated with the changes in density. We also observe the continuous formation of external ice, arising from water expelled from the pores while expansion takes place within the pores. An efficient method for monitoring the density of the confined D(2)O using a triple-axis spectrometer is demonstrated.
利用中子衍射,我们跟踪了重水在介孔硅质 MCM-41-S 基质中结构性质随温度的变化。通过观察对应于孔-孔距离的相关峰(由硅质和水之间的散射对比决定),我们监测了受限水的密度。同时,我们研究了 D(2)O 的显著第一衍射峰在 ≈ 1.8 Å(-1)处,该峰提供了水分子微观排列的信息。数据表明在 ≈ 275 K(± 10 K)处存在密度最大值,类似于体相水,并且在 ≈ 180 K(± 10 K)处存在密度最小值。发现 D(2)O 的显著衍射峰在从 200 到 270 K 的宽 T 范围内发生位移和变锐,反映了与密度变化强烈相关的结构变化。我们还观察到外部冰的连续形成,这是由于水从孔中排出,而孔内发生膨胀。展示了一种使用三轴光谱仪监测受限 D(2)O 密度的有效方法。