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正常椎间盘1H-NMR弛豫时间(T1、T2)的局部差异及其与水分含量的关系。

Topographic differences of 1H-NMR relaxation times (T1, T2) in the normal intervertebral disc and its relationship to water content.

作者信息

Chatani K, Kusaka Y, Mifune T, Nishikawa H

机构信息

Department of Orthopaedic Surgery, Kyoto Prefectural University of Medicine, Japan.

出版信息

Spine (Phila Pa 1976). 1993 Nov;18(15):2271-5. doi: 10.1097/00007632-199311000-00022.

Abstract

1H-nuclear magnetic resonance studies, in vitro, on normal intervertebral discs dissected from adult bovine (3- or 4-year-old) coccygeal vertebrae were performed to clarify topographic differences in relaxation times (T1, T2) and relationships between the relaxation times and water content. Immediately after death, intervertebral discs were dissected from 1st/2nd and 2nd/3rd coccygeal vertebrae and divided into three specimens: the nucleus pulposus, inner anulus fibrosus, and outer anulus fibrosus. T1, T2, and water content were measured for the specimens collected from 15 intervertebral discs (untreated group). Secondly, specimens were similarly collected from 12 intervertebral discs and were treated to changed water contents (dehydrated group and hydrated group). For each treated specimen, T1, T2, and water content were measured. The results showed highly significant differences (P < 0.01) in T1 values among the nucleus pulposus, inner anulus fibrosus, and outer anulus fibrosus, and also in T2 values between the nucleus pulposus and anulus fibrosus. In each of the nucleus pulposus and anulus fibrosus, a positive linear relationship (r = 0.97, P < 0.01) was found between T1 and water content. The respective regression lines for the nucleus pulposus and anulus fibrosus had different slopes, and the slope of the nucleus pulposus was significantly greater than that of the anulus fibrosus. Thus, the decrease in water content shortens the T1 in intervertebral discs, and changes in water content have a greater influence on T1 in the nucleus pulposus than in the anulus fibrosus.(ABSTRACT TRUNCATED AT 250 WORDS)

摘要

对从成年牛(3或4岁)尾椎骨上解剖下来的正常椎间盘进行了体外1H核磁共振研究,以阐明弛豫时间(T1、T2)的地形差异以及弛豫时间与含水量之间的关系。牛死后立即从第1/2和第2/3尾椎骨上解剖出椎间盘,并将其分为三个样本:髓核、纤维环内层和纤维环外层。对从15个椎间盘收集的样本(未处理组)测量了T1、T2和含水量。其次,从12个椎间盘同样收集样本并进行处理以改变含水量(脱水组和水化组)。对每个处理后的样本测量了T1、T2和含水量。结果显示,髓核、纤维环内层和纤维环外层之间的T1值存在高度显著差异(P < 0.01),髓核与纤维环之间的T2值也存在显著差异。在髓核和纤维环中,T1与含水量之间均发现呈正线性关系(r = 0.97,P < 0.01)。髓核和纤维环各自的回归线斜率不同,髓核的斜率显著大于纤维环的斜率。因此,含水量的降低会缩短椎间盘的T1,且含水量的变化对髓核T1的影响大于对纤维环T1的影响。(摘要截短至250字)

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