Chesnick Ingrid E, Avallone Francis A, Leapman Richard D, Landis William J, Eidelman Naomi, Potter Kimberlee
Magnetic Resonance Microscopy Facility, Department of Biophysics, Armed Forces Institute of Pathology Annex, 1413 Research Blvd, Rockville, MD 20850, USA.
Bone. 2007 Apr;40(4):904-12. doi: 10.1016/j.bone.2006.10.020. Epub 2006 Dec 15.
We present a three-dimensional mineralizing model based on a hollow fiber bioreactor (HFBR) inoculated with primary osteoblasts isolated from embryonic chick calvaria. Using non-invasive magnetic resonance microscopy (MRM), the growth and development of the mineralized tissue around the individual fibers were monitored over a period of 9 weeks. Spatial maps of the water proton MRM properties of the intact tissue, with 78 microm resolution, were used to determine changes in tissue composition with development. Unique changes in the mineral and collagen content of the tissue were detected with high specificity by proton density (PD) and magnetization transfer ratio (MTR) maps, respectively. At the end of the growth period, the presence of a bone-like tissue was verified by histology and the formation of poorly crystalline apatite was verified by selected area electron diffraction and electron probe X-ray microanalysis. FTIR microspectroscopy confirmed the heterogeneous nature of the bone-like tissue formed. FTIR-derived phosphate maps confirmed that those locations with the lowest PD values contained the most mineral, and FTIR-derived collagen maps confirmed that bright pixels on MTR maps corresponded to regions of high collagen content. In conclusion, the spatial mapping of tissue constituents by FTIR microspectroscopy corroborated the findings of non-invasive MRM measurements and supported the role of MRM in monitoring the bone formation process in vitro.
我们展示了一种基于中空纤维生物反应器(HFBR)的三维矿化模型,该反应器接种了从胚胎鸡颅骨分离的原代成骨细胞。使用非侵入性磁共振显微镜(MRM),在9周的时间内监测了单个纤维周围矿化组织的生长和发育。利用分辨率为78微米的完整组织的水质子MRM特性空间图来确定组织组成随发育的变化。分别通过质子密度(PD)图和磁化传递率(MTR)图以高特异性检测到组织中矿物质和胶原蛋白含量的独特变化。在生长周期结束时,通过组织学证实了类骨组织的存在,并通过选区电子衍射和电子探针X射线微分析证实了 poorly 结晶磷灰石的形成。傅里叶变换红外光谱显微镜(FTIR)证实了所形成的类骨组织的异质性。FTIR衍生的磷酸盐图证实,PD值最低的位置含有最多的矿物质,FTIR衍生的胶原蛋白图证实,MTR图上的亮像素对应于高胶原蛋白含量的区域。总之,FTIR显微镜对组织成分的空间映射证实了非侵入性MRM测量的结果,并支持了MRM在体外监测骨形成过程中的作用。