中子解剖学。

G E Bacon
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引用次数: 0

摘要

我们所熟悉的晶体材料的极端是单晶和无序粉末。介于这两个极端之间的是多晶聚集体,它们不是随机排列的,而是具有某种偏好的方向,这是建筑材料采取的形式,无论是钢梁还是人类或动物骨骼。优选方向的细节决定了材料在任何方向上承受应力的能力。在骨骼的例子中,关键因素是矿物成分(六方羟基磷灰石晶体)的c轴方向,这可以很容易地通过中子衍射确定。特别是,它可以测量一块骨头的体积,利用距离从1毫米到10毫米不等。主要的实际问题是避免胶原蛋白中氢的强烈非相干散射;这可以最好地通过热处理来实现,并且证明这不会影响下面的磷灰石。这些对骨头的研究为人类和动物的生活和活动提供了重要的解剖学信息——例如,包括人类股骨的生活史、羊的运动、赛马腿的骨折和新石器时代部落的生活方式。我们的结论是,这种材料被经济地放置在骨骼中,以承受预期的生活和环境压力。实验结果以0002磷灰石反射的幅度表示。碰巧的是,对于一种随机粉末,0002和1121的反射,它们是粉末图案中相邻的线,在强度上大致相等。后一种反射是多重的,几乎不受首选方向的影响,因此0002/1121比率的数值可以相当准确地作为骨样本c轴在任何选择方向上的方向程度的定量测量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Neutron anatomy.

The familiar extremes of crystalline material are single-crystals and random powders. In between these two extremes are polycrystalline aggregates, not randomly arranged but possessing some preferred orientation and this is the form taken by constructional materials, be they steel girders or the bones of a human or animal skeleton. The details of the preferred orientation determine the ability of the material to withstand stress in any direction. In the case of bone the crucial factor is the orientation of the c-axes of the mineral content-the crystals of the hexagonal hydroxyapatite- and this can readily be determined by neutron diffraction. In particular it can be measured over the volume of a piece of bone, utilising distances ranging from 1 mm to 10 mm. The major practical problem is to avoid the intense incoherent scattering from the hydrogen in the accompanying collagen; this can best be achieved by heat-treatment and it is demonstrated that this does not affect the underlying apatite. These studies of bone give leading anatomical information on the life and activities of humans and animals-including, for example, the life history of the human femur, the locomotion of sheep, the fracture of the legs of racehorses and the life-styles of Neolithic tribes. We conclude that the material is placed economically in the bone to withstand the expected stresses of life and the environment. The experimental results are presented in terms of the magnitude of the 0002 apatite reflection. It so happens that for a random powder the 0002, 1121 reflections, which are neighbouring lines in the powder pattern, are approximately equal in intensity. The latter reflection, being of manifold multiplicity, is scarcely affected by preferred orientation so that the numerical value of the 0002/1121 ratio serves quite accurately as a quantitative measure of the degree of orientation of the c-axes in any chosen direction, for a sample of bone.

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