Stock Stuart R, Morse Paul E, Stock Michala K, James Kelsey C, Natanson Lisa J, Chen Haiyan, Shevchenko Pavel D, Maxey Evan R, Antipova Olga A, Park Jun-Sang
Northwestern University, Simpson Querrey Institute, Feinberg School of Medicine, Chicago Department of Cell and Developmental Biology, Illinois, United States.
Duke University, Department of Evolutionary Anthropology, Durham, North Carolina, United States.
J Med Imaging (Bellingham). 2022 May;9(3):031504. doi: 10.1117/1.JMI.9.3.031504. Epub 2022 Feb 2.
Tomography using diffracted x-rays produces reconstructions mapping quantities such as crystal lattice parameter(s), crystallite size, and crystallographic texture, information quite different from that obtained with absorption or phase contrast. Diffraction tomography is used to map an entire blue shark centrum with its double cone structure (corpora calcerea) and intermedialia (four wedges). Energy dispersive diffraction (EDD) and polychromatic synchrotron x-radiation at 6-BM-B, the Advanced Photon Source, were used. Different, properly oriented Bragg planes diffract different x-ray energies; these intensities are measured by one of ten energy-sensitive detectors. A pencil beam defines the irradiated volume, and a collimator before each energy-sensitive detector selects which portion of the irradiated column is sampled at any one time. Translating the specimen along , and axes produces a 3D map. We report 3D maps of the integrated intensity of several bioapatite reflections from the mineralized cartilage centrum of a blue shark. The axis reflection's integrated intensities and those of a reflection with no axis component reveal that the cone wall's bioapatite is oriented with its axes lateral, i.e., perpendicular to the backbone's axis, and that the wedges' bioapatite is oriented with its axes axial. Absorption microcomputed tomography (laboratory and synchrotron) and x-ray excited x-ray fluorescence maps provide higher resolution views. The bioapatite in the cone walls and wedges is oriented to resist lateral and axial deflections, respectively. Mineralized tissue samples can be mapped in 3D with EDD tomography and subsequently studied by destructive methods.
使用衍射X射线的断层扫描技术可生成重建图像,用以描绘诸如晶格参数、微晶尺寸和晶体取向等物理量,这些信息与通过吸收或相衬获得的信息截然不同。衍射断层扫描技术被用于绘制一条蓝鲨椎体的完整图像,该椎体具有双锥体结构(钙化体)和中间部分(四个楔形物)。研究使用了位于先进光子源6-BM-B处的能量色散衍射(EDD)和多色同步加速器X射线辐射。不同且取向合适的布拉格平面衍射不同的X射线能量;这些强度由十个能量敏感探测器之一进行测量。一支铅笔状光束确定被照射体积,并且在每个能量敏感探测器之前的准直器选择在任何时刻对被照射柱的哪一部分进行采样。沿x、y和z轴平移样本可生成三维地图。我们报告了来自蓝鲨矿化软骨椎体的几种生物磷灰石反射的积分强度的三维地图。z轴反射的积分强度以及一个没有z轴分量的反射的积分强度表明,锥体壁的生物磷灰石其z轴呈横向取向,即垂直于脊柱轴,并且楔形物的生物磷灰石其z轴呈轴向取向。吸收式微型计算机断层扫描(实验室和同步加速器)以及X射线激发的X射线荧光地图提供了更高分辨率的视图。锥体壁和楔形物中的生物磷灰石分别以抵抗横向和轴向偏转的方式取向。矿化组织样本可以通过EDD断层扫描进行三维映射,随后用破坏性方法进行研究。