Harder S L, Hopp K M, Ward H, Neglio H, Gitlin J, Kido D
Department of Medical Imaging, Royal University Hospital, Saskatoon, Saskatchewan, Canada.
AJNR Am J Neuroradiol. 2008 Jan;29(1):176-83. doi: 10.3174/ajnr.A0770. Epub 2007 Nov 7.
Susceptibility-weighted imaging (SWI) is an advanced MR imaging sequence that can be implemented at high resolution. This sequence can be performed on conventional MR imaging scanners and is very sensitive to mineralization. The purpose of this study was to establish the course of mineralization in the deep gray matter with age by using SWI.
We retrospectively reviewed susceptibility-weighted images of 134 patients (age range, 1 to 88 years). Inclusion criteria comprised a normal conventional MR imaging (T1, T2, and fluid-attenuated inversion recovery sequences). We statistically analyzed the relative signal intensities of the globus pallidus, putamen, substantia nigra, caudate nucleus, red nucleus, and thalamus for correlation with age. The putamen was graded according to a modified scale, based on previous work that described a systematic pattern of mineralization with age. Bands of hypointensity in the globus pallidus, dubbed "waves," were also evaluated.
We documented decreasing intensity (ie, increasing mineralization) with age in all deep gray matter areas analyzed. We confirmed the age-related posterolateral to anteromedial progression of mineralization in the putamen. Characteristic medial and lateral bands of mineralization were exhibited in the globus pallidus in all children and young adults older than 3 years. Finally, an increase in the number of "waves" present in the globus pallidus was associated with increased age by category.
This study documents the course and pattern of mineralization in the deep gray matter with age, as determined by SWI. These findings may play a role in evaluating diseased brains in the future.
磁敏感加权成像(SWI)是一种先进的磁共振成像序列,可实现高分辨率成像。该序列可在传统磁共振成像扫描仪上进行,对矿化非常敏感。本研究的目的是利用SWI确定深部灰质矿化随年龄增长的过程。
我们回顾性分析了134例患者(年龄范围为1至88岁)的磁敏感加权图像。纳入标准包括常规磁共振成像(T1、T2和液体衰减反转恢复序列)正常。我们对苍白球、壳核、黑质、尾状核、红核和丘脑的相对信号强度进行了统计学分析,以确定其与年龄的相关性。根据之前描述矿化随年龄变化的系统模式的研究,壳核按改良量表进行分级。还对苍白球中被称为“波”的低信号带进行了评估。
我们记录了在所分析的所有深部灰质区域中,信号强度随年龄降低(即矿化增加)的情况。我们证实了壳核中矿化从后外侧向前内侧的年龄相关进展。在所有3岁以上的儿童和年轻人中,苍白球均呈现出特征性的内侧和外侧矿化带。最后,苍白球中“波”的数量增加与年龄类别增加相关。
本研究记录了利用SWI确定的深部灰质矿化随年龄增长的过程和模式。这些发现可能在未来评估患病大脑中发挥作用。