低温红外光谱研究无机碳酸盐和硝酸盐的晶格频率和旋转势垒

R. Schroeder, C. Weir, E. Lippincott
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引用次数: 61

摘要

在室温、液氮和液氦制冷条件下,获得了无机硝酸盐和碳酸盐在单晶上的红外吸收光谱。在1400 ~ 700 cm/sup -1/之间的室温光谱中观察到的漫反射吸收,在液氦制冷下被分解成大量的波段,这些波段不能归因于阴离子的基频或基频的组合。几乎所有这些频带都可以很容易地解释为振荡振荡器连续电平的基频的和频带。这种振动被认为是阴离子绕三角轴的平面扭振。振动频率部分取决于晶体结构和离子。在给定的材料中,由连续波段确定的振动频率是相当恒定的。在所研究的物质中,振动频率约为15至30 cm/sup -1/。光谱中观察到的带限被解释为代表旋转能垒。这些势垒高度约为200 cm/sup -1/,与晶体结构和所涉及的离子有一定的关系。余弦势函数计算的势垒高度与立方结构和方解石结构中所观察到的势垒高度相当吻合。由于分配可疑或结构细节未知,没有对其他结构进行类似的计算。特别是文石结构的光谱非常详细和复杂,没有进行分析。然而,这些细节和所有其他研究光谱似乎涉及类似的现象。(身份验证)«更少
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LATTICE FREQUENCIES AND ROTATIONAL BARRIERS FOR INORGANIC CARBONATES AND NITRATES FROM LOW TEMPERATURE INFRARED SPECTROSCOPY
Infrared absorption spectra of inorganic nitrates and carbonates were obtained on single crystals at room temperature, under liquid nitrogen and liquid helium refrigeration. Diffuse absorption observed in the room temperature spectra between about 1400 and 700 cm/sup -1/ is solved under liquid helium refrigeration into a large number of bands not attributable to fundamentals or combinations of fundamental frequencies of the anions. Almost all of these bands are readily interpreted as summation bands of fundamental frequencies with successive levels of a librating oscillator. The libration is considered to represent a planar torsional oscillation of the anion about the trigonal axis. The librational frequency depends in part on the crystal structure and on the ions. In a given material the librational frequency as determined from successive bands is reasonably constant. In the substances studied the librational frequency varied from about 15 to 30 cm/sup -1/. Band limits observed in the spectra are interpreted as representing rotational energy barriers. These barrier heights are approximately 200 cm/sup -1/ with some dependence on the crystal structure and the ions involved. Barrier heights calculated from a cosine potential function agree reasonably well with the observed barriers for the cubic and calcite structures. Similar calculations weremore » not made for other structures studied because of doubtful assignments or unknown structural details. In particular, spectra of the aragonite structures are remarkable in detail and complexity, and were not analyzed. However, the details of these and all other spectra studied appear to involve similar phenomena. (auth)« less
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