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Histological and electron microprobe studies of mineralisation in aluminium-related osteomalacia.

机译:铝相关骨软化症中矿化的组织学和电子微探针研究。

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摘要

AIMS: To determine a possible mechanism to explain the presence of aluminium lines within fully calcified bone in aluminium-related osteomalacia. METHODS: Fifty five bone cases shown by bone biopsy to be aluminium-related osteomalacia were studied. In 38 specimens aluminium lines were identified within calcified bone by means of the Aluminon stain and a characteristic form of patchy mineralisation was seen within thickened osteoid seams. Five representative examples were analysed quantitatively by histomorphometry and electronprobe X-ray microanalysis and compared with five cases of vitamin D deficiency-related osteomalacia which also had patchy mineralisation. RESULTS: The patchy calcification occupied 40 +/- 8% (mean +/- SEM) of the osteoid and consisted of small focal deposits (less than 40 microns diameter), often (52%) around osteoid osteocytes (probably an underestimate of the association), and larger areas that extended to the aluminium lines at the underlying mineralisation front. Small and large mineralisation nuclei were seen ultrastructurally in the patchy calcification. Quantitative electronprobe X-ray microanalysis showed that calcium concentrations and calcium:phosphorus ratios in the mineralisation nuclei and in the superficial layer of the fully calcified bone of the aluminium-related osteomalacia cases were significantly less than values measured at similar sites in the vitamin D deficiency-related osteomalacia cases. Furthermore, aluminium could not be detected by means of this technique at the mineralisation front or along cement lines in these specimens. CONCLUSIONS: Calcification can occur in thickened osteoid seams in osteomalacia. It can begin around osteoid osteocytes as small deposits that enlarge within the osteoid and extend to the underlying mineralisation front or cement line where aluminium lines may become trapped. Complete calcification of osteoid could account for the presence of aluminium lines within fully calcified bone. The Aluminon stain appears to be a more sensitive method for the detection of aluminium in bone than electronprobe X-ray microanalysis.
机译:目的:确定解释铝相关骨软化症中完全钙化骨中铝线存在的可能机制。方法:对55例经骨活检证实为铝相关性骨软化症的骨病例进行了研究。在38个标本中,通过Aluminon染色在钙化的骨中发现了铝线,并且在增厚的类骨质接缝中发现了斑块状矿化的特征形式。通过组织形态计量学和电子探针X射线显微分析对5个代表性实例进行了定量分析,并与5例维生素D缺乏症相关的骨软化症(也有片状矿化)进行了比较。结果:斑块状钙化占类骨质的40 +/- 8%(平均+/- SEM),由小的病灶性沉积物(直径小于40微米)组成,通常(52%)位于类骨质骨细胞周围(可能是骨钙素的低估了)关联)和更大的区域,这些区域扩展到了潜在矿化前沿的铝线。在斑片状钙化中超微结构可见大小矿化核。定量电子探针X射线显微分析表明,与铝有关的骨软化症病例的矿化核和完全钙化的骨的表层中的钙浓度和钙:磷比明显低于在维生素D缺乏症的相似部位测得的值相关的骨软化症病例。此外,通过这种技术无法在这些样品的矿化前沿或沿水泥线检测到铝。结论:骨软化症中增厚的类骨质接缝可发生钙化。它可以在类骨质骨细胞周围开始,是在类骨质内扩大并延伸到下面的矿化带或水泥线的小沉积物,铝线可能会被困住。类固醇的完全钙化可以解释完全钙化的骨中铝线的存在。与电子探针X射线显微分析相比,Aluminon染色似乎是一种更灵敏的检测骨骼中铝的方法。

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