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具有极高弛豫率的沸石GdNaY纳米颗粒,用作磁共振成像中的造影剂。

Zeolite GdNaY nanoparticles with very high relaxivity for application as contrast agents in magnetic resonance imaging.

作者信息

Platas-Iglesias Carlos, Vander Elst Luce, Zhou Wuzong, Muller Robert N, Geraldes Carlos F G C, Maschmeyer Thomas, Peters Joop A

机构信息

Laboratory of Applied Organic Chemistry and Catalysis, Delft University of Technology, Julianalaan 136, 2628 BL Delft, The Netherlands.

出版信息

Chemistry. 2002 Nov 15;8(22):5121-31. doi: 10.1002/1521-3765(20021115)8:22<5121::AID-CHEM5121>3.0.CO;2-W.

Abstract

In this paper we explore Gd(3+)-doped zeolite NaY nanoparticles for their potential application as a contrast agent in magnetic resonance imaging (MRI). The nanoparticles have an average size of 80-100 nm, as determined by TEM and XRD. A powdered sample loaded with La3+ was characterised by means of multinuclear solid-state NMR spectroscopy. The NMR dispersion (NMRD) profiles obtained from aqueous suspensions of samples with Gd3+ doping ratios of 1.3-5.4 wt% were obtaining at different temperatures. The relaxivity increases drastically as the Gd3+ loading decreases, with values ranging between 11.4 and 37.7 s-1 mM-1 at 60 MHz and 37 degrees C. EPR spectra of aqueous suspensions of the samples suggest that an interaction between neighbouring Gd3+ ions within the same particle produces a significant increase in the transversal electronic relaxation rates in samples with a high Gd3+ content. The experimental NMRD and EPR data are explained with the use of a model that considers the system as a concentrated aqueous solution of Gd3+ in the interior of the zeolite that is in exchange with the bulk water outside the zeolite. The results obtained indicate that the Gd3+ ion is immobilised in the interior of the zeolite and that the relaxivity is mainly limited by the relatively slow diffusion of water protons from the pores of the zeolite channels into the bulk water.

摘要

在本文中,我们探索了掺杂钆(Gd(3+))的沸石NaY纳米颗粒作为磁共振成像(MRI)造影剂的潜在应用。通过透射电子显微镜(TEM)和X射线衍射(XRD)测定,这些纳米颗粒的平均尺寸为80 - 100纳米。用多核固态核磁共振光谱对负载La3+的粉末样品进行了表征。从钆(Gd3+)掺杂比例为1.3 - 5.4 wt%的样品的水悬浮液中获得的核磁共振分散(NMRD)曲线是在不同温度下得到的。随着Gd3+负载量的降低,弛豫率急剧增加,在60 MHz和37摄氏度下,其值在11.4至37.7 s-1 mM-1之间。样品水悬浮液的电子顺磁共振(EPR)光谱表明,在同一颗粒内相邻Gd3+离子之间的相互作用会使Gd3+含量高的样品中的横向电子弛豫率显著增加。利用一个模型对实验得到的NMRD和EPR数据进行了解释,该模型将系统视为沸石内部Gd3+的浓水溶液,它与沸石外部的大量水进行交换。所得结果表明,Gd3+离子固定在沸石内部,弛豫率主要受水质子从沸石通道孔隙向大量水的相对缓慢扩散的限制。

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