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磁共振成像弛豫对比剂的外球层研究。以具有第二球层水的环十肽钆配合物为例。

Outer-sphere investigation of MRI relaxation contrast agents. Example of a cyclodecapeptide gadolinium complex with second-sphere water.

机构信息

CEA, INAC, Service de Chimie Inorganique et Biologique (UMR_E 3 CEA UJF, FRE 3200 CNRS), 38054 Grenoble, France.

出版信息

J Phys Chem B. 2010 Jul 8;114(26):8770-81. doi: 10.1021/jp101443v.

Abstract

We show how the purely outer-sphere (OS) relaxivity of a probe solute due to a Gd(3+) complex can help characterize the outer (O), inner (I), and second (2) sphere (S) contributions to the water proton relaxivity. Because of the difficulties of accurate theoretical predictions, we propose an experimental determination of the OS dipolar time correlation function (OS-DTCF) of the relative position of Gd(3+) with respect to any of the equivalent protons of the purely OS probe p-dioxane, which moves around the complex without binding to it. The method is illustrated by the GdPA complex with PA = c(AspArgGluProGlyGluTrpAspProGly). The experimental DTCF for dioxane is obtained by a model-free analysis of the high-field relaxivity of its protons. The time-modulation of the dioxane DTCF by the Gd(3+) electronic spin relaxation yields a measurable quenching of the longitudinal relaxivity at low-to-medium field, which serves us to deduce the fluctuating zero-field splitting (ZFS) Hamiltonian causing this electronic relaxation. The DTCF for water is derived from that for dioxane by appropriate scaling of the geometry of collision and relative diffusion coefficients of these molecules with respect to GdPA. The information obtained on the OS motion for water and the ZFS Hamiltonian together with an independent characterization of the IS contribution allows us to disentangle the OS, IS, and 2S mechanisms and interpret the relaxivity profile of the water protons from 2.35 mT to 18.8 T. The presence of a large 2S contribution is confirmed.

摘要

我们展示了由于 Gd(3+) 配合物,探针溶质的纯外球(OS)弛豫率如何帮助表征水质子弛豫率的外(O)、内(I)和第二(2)球(S)贡献。由于准确的理论预测存在困难,我们提出了一种实验确定 Gd(3+) 相对于纯 OS 探针 p-二氧六环的任何等效质子的相对位置的 OS 偶极子相关函数(OS-DTCF)的方法,该方法是通过模型自由分析其质子的高场弛豫率来说明的。该方法用于 GdPA 配合物,其中 PA = c(AspArgGluProGlyGluTrpAspProGly)。通过电子自旋弛豫,二氧六烷的 DTCF 随时间的变化导致在低至中等场时纵向弛豫率可测量地猝灭,这使我们能够推断出引起这种电子弛豫的波动零场分裂(ZFS)哈密顿量。水的 DTCF 是通过适当缩放这些分子的碰撞几何形状和相对扩散系数相对于 GdPA 从二氧六烷推导出来的。获得的关于水的 OS 运动和 ZFS 哈密顿量的信息以及 IS 贡献的独立特征化,使我们能够分离 OS、IS 和 2S 机制,并解释从 2.35 mT 到 18.8 T 的水质子的弛豫率谱。证实了存在较大的 2S 贡献。

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