Small angle X-ray scattering study on Lingula unguis shell.

M Iijima, Y Moriwaki, T Gyotoku, K Hayashi, S Imura
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引用次数: 4

Abstract

Lingula unguis shell yields a diffuse small angle X-ray scattering which is caused mainly by the scattering from particles of apatite. In this study, the distribution of particles smaller than 500A was analyzed using the small angle X-ray scattering technique. The non-linear Guinier plot indicates that the shell contains various sizes of apatite particles ranging about 20-460A. The small granules with size about 20-160A in diameter are located in the marginal part of the shell and progressively larger granules are observed internally towards the central part. The scattering is anisotropic in the lateral and central part, where the apatite crystals highly ordered. The combined analysis of wide and small angle diffraction indicates that the particles are elongated in the c-axis direction and, furthermore, their long axes are arranged almost parallel to the direction of growth in these parts. This suggests that small and isotropic particles are formed in the early stage of mineralization and larger ellipsoidal shaped particles are formed in the later stage of mineralization.

狭舌龟壳的小角x射线散射研究。
甲壳产生一种漫射小角x射线散射,这种散射主要是由磷灰石颗粒散射引起的。在本研究中,使用小角x射线散射技术分析了小于500A的颗粒的分布。非线性Guinier图表明,壳中含有不同尺寸的磷灰石颗粒,大小在20 ~ 460a之间。直径约为20-160A的小颗粒位于壳的边缘部分,向内向中心部分观察到逐渐增大的颗粒。在磷灰石晶体高度有序的侧面和中心部分,散射是各向异性的。宽角和小角衍射的结合分析表明,颗粒在c轴方向上被拉长,并且它们的长轴在这些部分几乎与生长方向平行。这表明成矿作用早期形成小而各向同性的颗粒,成矿作用后期形成较大的椭球状颗粒。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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