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正常压力脑积水背景下的脑脊液在脑内的流动

CSF Flow in the Brain in the Context of Normal Pressure Hydrocephalus.

作者信息

Bradley W G

机构信息

From the Department of Radiology, University of California, San Diego, San Diego, California.

出版信息

AJNR Am J Neuroradiol. 2015 May;36(5):831-8. doi: 10.3174/ajnr.A4124. Epub 2014 Oct 29.

Abstract

CSF normally flows back and forth through the aqueduct during the cardiac cycle. During systole, the brain and intracranial vasculature expand and compress the lateral and third ventricles, forcing CSF craniocaudad. During diastole, they contract and flow through the aqueduct reverses. Hyperdynamic CSF flow through the aqueduct is seen when there is ventricular enlargement without cerebral atrophy. Therefore, patients presenting with clinical normal pressure hydrocephalus who have hyperdynamic CSF flow have been found to respond better to ventriculoperitoneal shunting than those with normal or decreased CSF flow. Patients with normal pressure hydrocephalus have also been found to have larger intracranial volumes than sex-matched controls, suggesting that they may have had benign external hydrocephalus as infants. While their arachnoidal granulations clearly have decreased CSF resorptive capacity, it now appears that this is fixed and that the arachnoidal granulations are not merely immature. Such patients appear to develop a parallel pathway for CSF to exit the ventricles through the extracellular space of the brain and the venous side of the glymphatic system. This pathway remains functional until late adulthood when the patient develops deep white matter ischemia, which is characterized histologically by myelin pallor (ie, loss of lipid). The attraction between the bare myelin protein and the CSF increases resistance to the extracellular outflow of CSF, causing it to back up, resulting in hydrocephalus. Thus idiopathic normal pressure hydrocephalus appears to be a "2 hit" disease: benign external hydrocephalus in infancy followed by deep white matter ischemia in late adulthood.

摘要

在心动周期中,脑脊液通常在中脑导水管中来回流动。在收缩期,脑和颅内血管系统扩张并压迫侧脑室和第三脑室,迫使脑脊液作头尾方向流动。在舒张期,它们收缩,脑脊液通过中脑导水管的流动方向逆转。当存在脑室扩大而无脑萎缩时,可观察到脑脊液通过中脑导水管的高动力性流动。因此,已发现临床诊断为正常压力脑积水且脑脊液流动呈高动力性的患者,比起脑脊液流动正常或降低的患者,对脑室腹腔分流术的反应更好。还发现正常压力脑积水患者的颅内体积比性别匹配的对照组更大,这表明他们在婴儿期可能患过良性外部脑积水。虽然他们的蛛网膜颗粒明显降低了脑脊液的吸收能力,但现在看来这是固定不变的,而且蛛网膜颗粒不仅仅是不成熟。这类患者似乎形成了一条平行的脑脊液流出途径,即通过脑的细胞外间隙和类淋巴系统的静脉侧离开脑室。这条途径在成年后期之前一直发挥作用,直到患者发生深部白质缺血,其组织学特征为髓鞘苍白(即脂质丧失)。裸露的髓鞘蛋白与脑脊液之间的吸引力增加了脑脊液向细胞外流出的阻力,导致脑脊液回流,从而引起脑积水。因此,特发性正常压力脑积水似乎是一种“双重打击”疾病:婴儿期的良性外部脑积水,随后是成年后期的深部白质缺血。

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