Hifumi Hiroki, Tanimoto Akihiro, Citterio Daniel, Komatsu Hirokazu, Suzuki Koji
Department of Applied Chemistry, Faculty of Science and Technology, Keio University, 3-14-1 Hiyoshi, Kohoku-ku, Yokohama, Kanagawa 223-8522, Japan.
Analyst. 2007 Nov;132(11):1153-60. doi: 10.1039/b707225b. Epub 2007 Aug 17.
Novel gadolinium complexes (KMR-series: KMR-K and KMR-Mg), which have a bis-15-crown-5 ether or a charged beta-diketone structure as a recognition site, have been designed, synthesized and applied for the detection of K(+) or of Mg(2+) and Ca(2+) using MRI or NMR techniques. The measurements are based on the modulation of the longitudinal relaxation time (T(1)) of water protons in proximity of the gadolinium complexes. Relaxivity measurements of KMR-K1 in aqueous solution showed that the initial longitudinal relaxivity value (r(1)) of 5.05 mM(-1) s(-1) is monotonously decreasing with increasing K(+) concentrations, reaching a final value of 4.78 mM(-1) s(-1). This decrease is attributed to a change in the second sphere of hydration of the gadolinium (Gd(3+)) complex (KMR-K), resulting in a K(+) concentration-dependent contrast in MR images. From stoichiometric analysis using mass spectrometry and UV/VIS spectrometry, a 1 : 1 complex formation between KMR-K1 and K(+) in a sandwich-type manner with a log K of 3.20 was confirmed. In the case of KMR-Mg, the initial r(1) value of 4.98 mM(-1) s(-1) is monotonously decreasing with increasing Mg(2+) or Ca(2+) concentrations, reaching a final value of 3.95 or 4.16 mM(-1) s(-1), respectively, resulting in Mg(2+) and Ca(2+) concentration-dependent contrast in MR images. The formation of a 1:1 complex with a log K of 2.33 for Mg(2+) and 1.91 for Ca(2+) was confirmed. KMR-K1 and KMR-Mg are the first ion-selective or ion-sensitive gadolinium complexes for K(+) or Mg(2+) and Ca(2+), respectively.
设计、合成了具有双-15-冠-5醚或带电荷的β-二酮结构作为识别位点的新型钆配合物(KMR系列:KMR-K和KMR-Mg),并将其应用于利用磁共振成像(MRI)或核磁共振(NMR)技术检测K⁺或Mg²⁺和Ca²⁺。这些测量基于钆配合物附近水质子纵向弛豫时间(T₁)的调制。KMR-K1在水溶液中的弛豫率测量表明,5.05 mM⁻¹ s⁻¹的初始纵向弛豫率值(r₁)随着K⁺浓度的增加而单调下降,最终值达到4.78 mM⁻¹ s⁻¹。这种下降归因于钆(Gd³⁺)配合物(KMR-K)第二水合层的变化,从而在磁共振图像中产生了依赖于K⁺浓度的对比度。通过质谱和紫外/可见光谱的化学计量分析,证实了KMR-K1与K⁺以夹心型方式形成1:1配合物,log K为3.20。对于KMR-Mg,4.98 mM⁻¹ s⁻¹的初始r₁值随着Mg²⁺或Ca²⁺浓度的增加而单调下降,最终值分别达到3.95或4.16 mM⁻¹ s⁻¹,从而在磁共振图像中产生了依赖于Mg²⁺和Ca²⁺浓度的对比度。已证实与Mg²⁺形成log K为2.33、与Ca²⁺形成log K为1.91的1:1配合物。KMR-K1和KMR-Mg分别是第一种对K⁺或Mg²⁺和Ca²⁺具有离子选择性或离子敏感性的钆配合物。