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

被引:0
|
作者
Platas-Iglesias, C
Vander Elst, L
Zhou, WZ
Muller, RN
Geraldes, CFGC
Maschmeyer, T
Peters, JA
机构
[1] Delft Univ Technol, Lab Appl Organ Chem, NL-2628 BL Delft, Netherlands
[2] Univ A Coruna, Fac Ciencias, Dept Quim Fundamental, La Coruna, Spain
[3] Univ Mons, Dept Organ Chem, NMR Lab, B-7000 Mons, Belgium
[4] Univ St Andrews, Sch Chem, St Andrews KY16 9ST, Fife, Scotland
[5] Univ Coimbra, Dept Bioquim, Fac Ciencias & Tecnol, P-3049 Coimbra, Portugal
[6] Univ Coimbra, Ctr Neurociencias, P-3049 Coimbra, Portugal
关键词
contrast agents; gadolinium; lanthanides; magnetic resonance imaging; zeolites;
D O I
10.1002/1521-3765(20021115)8:22<5121::AID-CHEM5121>3.0.CO;2-W
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
In this paper we explore Gd3+-doped zeolite NaY nanoparticles for their potential application as a contrast agent in magnetic resonance imaging (MRI). The nanoparticles have an average size of 80-100nm, 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 obtained 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 degreesC. 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.
引用
收藏
页码:5121 / 5131
页数:11
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