首页> 外文会议>ASME summer bioengineering conference;SBC2009 >THE CHARACTERIZATION AND COMPARISON OF HUMAN CORTICAL BONE AND TEETH STRUCTURAL CHANGES BY LOW FIELD NMR
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THE CHARACTERIZATION AND COMPARISON OF HUMAN CORTICAL BONE AND TEETH STRUCTURAL CHANGES BY LOW FIELD NMR

机译:低场核磁共振对人骨皮质和牙齿结构变化的表征与比较

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It is known that NMR proton spin-spin (T_2) or spin-lattice (T_1) relaxation time measurements and analytical processing techniques have been used to determine microstructural characteristics of various types of fluid filled porous materials with characteristic pore sizes ranging from sub-micron to sub-millimeter. Currently this method has been developed and applied to quantify the porosity, pore size distribution and microdamage in human cortical bone [1-3]. The observed proton NMR relaxation signals are a convolution of the relaxation of fluid in the pores throughout the observed system with the longer relaxation time corresponding to larger pore sizes. Thus, regions within the bone matrix in which fluid may accumulate can effectively be treated as a "pore" and will be manifest as a change in the relaxation signal. Deconvolution of the relaxation signal can provide quantitative information about the relaxation distributions of fluid inside bone, i.e., the distribution of water within bone tissue.
机译:众所周知,已使用NMR质子自旋(T_2)或自旋晶格(T_1)弛豫时间测量和分析处理技术来确定各种类型的流体填充多孔材料的微结构特征,其特征孔径为亚微米到亚毫米。目前,已经开发出该方法并将其用于定量人类皮质骨中的孔隙率,孔径分布和微损伤[1-3]。观察到的质子NMR弛豫信号是整个观察系统中孔隙中流体弛豫的卷积,弛豫时间越长,对应的孔径越大。因此,骨基质内可能积聚流体的区域可以有效地视为“孔”,并将表现为松弛信号的变化。松弛信号的去卷积可以提供关于骨内流体的松弛分布,即,骨组织内的水的分布的定量信息。

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