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结合锰增强弛豫成像,通过动态二维相关实验分析心肌组织各区间的平衡水交换。

Analyzing equilibrium water exchange between myocardial tissue compartments using dynamical two-dimensional correlation experiments combined with manganese-enhanced relaxography.

作者信息

Seland John Georg, Bruvold Morten, Brurok Heidi, Jynge Per, Krane Jostein

机构信息

Department of Circulation and Medical Imaging, Norwegian University of Science and Technology, Trondheim, Norway.

出版信息

Magn Reson Med. 2007 Oct;58(4):674-86. doi: 10.1002/mrm.21323.

Abstract

Water compartments were identified and equilibrium water exchange was studied in excised rat myocardium enriched with intracellular manganese (Mn(2+)). Standard relaxographic measurements were supplemented with diffusion-T(2) and T(1)-T(2) correlation measurements. In nonenriched myocardium, one T(1) component (800 ms) and three T(2) components (32, 120, and 350 ms) were identified. The correlation measurements revealed fast- and slow-diffusing water fractions with mean diffusion coefficients of 1.2 x 10(-5) and 3.0 x 10(-5) cm(2) s(-1). The two shortest T(2) components, which had different diffusivities, both originated from water in intracellular compartments. A component with longer relaxation time (T(1) approximately equal 2200 ms; T(2) approximately equal 1200 ms), originating from extra-tissue water, was also observed. The presence of this component may lead to erroneous estimations of water exchange rates from multiexponential relaxographic analyses of excised tissues. The tissue T(1) value is strongly reduced with increasing enrichment of Mn(2+), and eventually a second tissue T(1) component emerges, indicating a shift in the equilibrium water exchange between intra- and extracellular compartments from the fast-exchange limit to the slow-exchange regime. Using a two-site water exchange analysis, the lifetime of intracellular water, T(ic), was found to be 475 ms, with a fraction, p(ic), of 0.71.

摘要

在富含细胞内锰(Mn(2+))的离体大鼠心肌中识别水室并研究平衡水交换。标准弛豫成像测量辅以扩散-T(2)和T(1)-T(2)相关性测量。在未富集的心肌中,识别出一个T(1)成分(800毫秒)和三个T(2)成分(32、120和350毫秒)。相关性测量揭示了快速和慢速扩散的水分数,其平均扩散系数分别为1.2×10(-5)和3.0×10(-5)平方厘米每秒。两个最短的T(2)成分具有不同的扩散率,均源自细胞内室中的水。还观察到一个具有较长弛豫时间的成分(T(1)约等于2200毫秒;T(2)约等于1200毫秒),源自组织外水。该成分的存在可能导致从离体组织的多指数弛豫成像分析中错误估计水交换率。随着Mn(2+)富集增加,组织T(1)值显著降低,最终出现第二个组织T(1)成分,表明细胞内和细胞外室之间的平衡水交换从快速交换极限转变为慢速交换状态。使用两点水交换分析,发现细胞内水的寿命T(ic)为475毫秒,分数p(ic)为0.71。

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