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通过2H双量子滤波MRI研究静息和受压状态下关节软骨中的纤维取向映射。

Mapping the fiber orientation in articular cartilage at rest and under pressure studied by 2H double quantum filtered MRI.

作者信息

Shinar Hadassah, Seo Yoshiteru, Ikoma Kazuya, Kusaka Yoshiaki, Eliav Uzi, Navon Gil

机构信息

School of Chemistry, Tel Aviv University, Israel.

出版信息

Magn Reson Med. 2002 Aug;48(2):322-30. doi: 10.1002/mrm.10195.

Abstract

The one-dimensional (2)H double quantum filtered (DQF) spectroscopic imaging technique was used to study the orientation of collagen fibers in articular cartilage. The method detects only water molecules in anisotropic environments, which in cartilage is caused by their interaction with the collagen fibers. A large quadrupolar splitting was observed in the calcified zone and a smaller splitting in the radial zone. In the transitional zone the splitting was not resolved and a small splitting was again detected in the superficial zone. From measurements performed at two orientations of the plug relative to the magnetic field it was deduced that in the calcified and radial zones the fibers are oriented perpendicular to the bone, bending at the transitional zone and flattening at the superficial zone. The effect of load applied to the cartilage-bone plug was monitored by the same technique. At low loads there is a small decrease in the quadrupolar splitting in the calcified zone, a marked decrease in the radial zone, and an increase of the splitting accompanied by a thickening of the superficial zone. Under high loads, while the thickening and the splitting of the superficial zone further increase, the splitting in the radial and calcified zones completely collapse. Pressure-induced changes in the thickness of the surface zone indicate flattening of the collagen fibers near the surface. The marked collapse of the splitting near the bone at high pressures may result from crimping of the collagen fibers.

摘要

采用一维氘双量子滤波(DQF)光谱成像技术研究关节软骨中胶原纤维的取向。该方法仅检测各向异性环境中的水分子,在软骨中,这是由水分子与胶原纤维的相互作用引起的。在钙化区观察到较大的四极分裂,在放射状区分裂较小。在过渡区,分裂未分辨出来,而在表层区再次检测到较小的分裂。通过对软骨-骨栓相对于磁场的两个取向进行测量,推断出在钙化区和放射状区,纤维垂直于骨定向,在过渡区弯曲,在表层区变平。用相同技术监测施加于软骨-骨栓的负荷的影响。在低负荷下,钙化区的四极分裂略有下降,放射状区明显下降,分裂增加并伴有表层区增厚。在高负荷下,虽然表层区的增厚和分裂进一步增加,但放射状区和钙化区的分裂完全消失。压力引起的表面区厚度变化表明表面附近的胶原纤维变平。高压下骨附近分裂的明显消失可能是由于胶原纤维的卷曲。

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