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NMR relaxation induced by iron oxide particles: testing theoretical models

机译:氧化铁颗粒引起的NMR弛豫:测试理论模型

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Superparamagnetic iron oxide particles find their main application as contrast agents for cellular and molecular magnetic resonance imaging. The contrast they bring is due to the shortening of the transverse relaxation time T-2 of water protons. In order to understand their influence on proton relaxation, different theoretical relaxation models have been developed, each of them presenting a certain validity domain, which depends on the particle characteristics and proton dynamics. The validation of these models is crucial since they allow for predicting the ideal particle characteristics for obtaining the best contrast but also because the fitting of T-1 experimental data by the theory constitutes an interesting tool for the characterization of the nanoparticles. In this work, T-2 of suspensions of iron oxide particles in different solvents and at different temperatures, corresponding to different proton diffusion properties, were measured and were compared to the three main theoretical models (the motional averaging regime, the static dephasing regime, and the partial refocusing model) with good qualitative agreement. However, a real quantitative agreement was not observed, probably because of the complexity of these nanoparticulate systems. The Roch theory, developed in the motional averaging regime (MAR), was also successfully used to fit T-1 nuclear magnetic relaxation dispersion (NMRD) profiles, even outside the MAR validity range, and provided a good estimate of the particle size. On the other hand, the simultaneous fitting of T-1 and T-2 NMRD profiles by the theory was impossible, and this occurrence constitutes a clear limitation of the Roch model. Finally, the theory was shown to satisfactorily fit the deuterium T-1 NMRD profile of superparamagnetic particle suspensions in heavy water.
机译:超顺磁性氧化铁颗粒主要用作细胞和分子磁共振成像的造影剂。它们带来的对比度是由于水质子的横向弛豫时间T-2缩短。为了了解它们对质子弛豫的影响,已经开发了不同的理论弛豫模型,每个模型都表现出一定的有效性域,这取决于粒子的特性和质子动力学。这些模型的验证至关重要,因为它们可以预测理想的颗粒特征以获得最佳对比度,而且因为该理论对T-1实验数据的拟合构成了表征纳米颗粒的有趣工具。在这项工作中,测量了氧化铁颗粒在不同溶剂和不同温度下的悬浮液的T-2(对应于不同的质子扩散特性),并将其与三个主要理论模型(运动平均模型,静态移相模型,以及部分重定焦模型)但是,由于这些纳米微粒系统的复杂性,未观察到真正的定量协议。在运动平均方式(MAR)中发展起来的Roch理论也被成功地用于拟合T-1核磁弛豫色散(NMRD)曲线,甚至超出了MAR的有效范围,并提供了对粒径的良好估计。另一方面,理论上不可能同时拟合T-1和T-2 NMRD曲线,这种情况构成了Roch模型的明显局限性。最终,该理论显示出令人满意的拟合了重水中超顺磁性颗粒悬浮液的氘T-1 NMRD曲线。

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