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绘制骨间质液流动图谱:组织学处理过程中铁蛋白示踪剂的位移

Mapping bone interstitial fluid movement: displacement of ferritin tracer during histological processing.

作者信息

Ciani Cesare, Doty Stephen B, Fritton Susannah P

机构信息

Department of Biomedical Engineering, City College of New York/CUNY, Convent Avenue at 138th Street, New York, NY 10031, USA.

出版信息

Bone. 2005 Sep;37(3):379-87. doi: 10.1016/j.bone.2005.04.004.

Abstract

Bone interstitial fluid flow is thought to play a fundamental role in the mechanical stimulation of bone cells, either via shear stresses or cytoskeletal deformations. Recent evidence indicates that osteocytes are surrounded by a fiber matrix that may be involved in the mechanotransduction of external stimuli as well as in nutrient exchange. In our previous tracer studies designed to map how different-sized molecules travel through the bone porosities, we found that injected ferritin was confined to blood vessels and did not pass into the mineralized matrix. However, other investigators have shown that ferritin forms halo-shaped labeling that enters the mineralized matrix around blood vessels. This labeling is widely used to explain normal interstitial fluid movement in bone; in particular, it is said to demonstrate bulk centrifugal interstitial fluid movement away from a highly pressurized vascular porosity. In addition, appositional ferritin fronts are said to demonstrate centrifugal interstitial fluid movement from the medullary canal to the periosteal surface. The purpose of this study was to investigate the conflicting ferritin labeling results by evaluating the role of different histological processes in the formation of ferritin "halos." Ferritin was injected into the rat vasculature and allowed to circulate for 5 min. Samples obtained from tibiae were reacted for different times with Perl's reagent and then were either paraffin-embedded or sectioned with a cryostat. Halo-like labeling surrounding vascular pores was found in all groups, ranging from 1.2-3.9% for the samples treated with the shortest histological processes (unembedded, frozen sections) to 5.6-15% for the samples treated with the longest histological processes (paraffin-embedded sections). These results indicate that different histological processing methods are able to create ferritin "halos," with some processing methods allowing more redistribution of the ferritin tracer than others. Based on these results and the fact that "halo" labeling has not been found with any other tracer, as we seek to further delineate the movement of interstitial fluid and the role it plays in bone mechanotransduction, we believe that ferritin "halo" labeling should not be used to demonstrate physiological bone interstitial fluid flow.

摘要

骨间质液流动被认为在对骨细胞的机械刺激中发挥着基础性作用,其作用途径可以是剪切应力或细胞骨架变形。最近的证据表明,骨细胞被一种纤维基质所包围,这种纤维基质可能参与外部刺激的机械转导以及营养物质交换。在我们之前旨在绘制不同大小分子如何穿过骨孔隙的示踪剂研究中,我们发现注入的铁蛋白局限于血管内,并未进入矿化基质。然而,其他研究人员表明,铁蛋白形成晕状标记并进入血管周围的矿化基质。这种标记被广泛用于解释骨中正常的间质液流动;特别是,据说它证明了大量离心性间质液从高压血管孔隙中流出。此外,并列的铁蛋白前沿据说证明了间质液从髓腔到骨膜表面的离心性流动。本研究的目的是通过评估不同组织学过程在铁蛋白“晕”形成中的作用来研究相互矛盾的铁蛋白标记结果。将铁蛋白注入大鼠血管系统并使其循环5分钟。从胫骨获取的样本与佩尔试剂反应不同时间,然后进行石蜡包埋或用低温恒温器切片。在所有组中均发现血管孔周围有晕状标记,对于采用最短组织学处理过程(未包埋、冷冻切片)的样本,该标记范围为1.2 - 3.9%,而对于采用最长组织学处理过程(石蜡包埋切片)的样本,该标记范围为5.6 - 15%。这些结果表明,不同的组织学处理方法能够产生铁蛋白“晕”,一些处理方法比其他方法允许铁蛋白示踪剂有更多的重新分布。基于这些结果以及尚未用任何其他示踪剂发现“晕”标记这一事实,当我们试图进一步描绘间质液的流动及其在骨机械转导中所起的作用时,我们认为铁蛋白“晕”标记不应被用于证明生理性骨间质液流动。

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