TRG Diagnostic Imaging, Bayer Pharma AG, Berlin, Germany.
Invest Radiol. 2011 Dec;46(12):796-800. doi: 10.1097/RLI.0b013e31822b1272.
X-ray contrast agents (CA) possess specific physicochemical properties and are excreted renally by glomerular filtration. Thereby, they may affect the diffusion of water molecules within the kidney. The aim of our preclinical study was to investigate potential changes in the apparent diffusion coefficient (ADC) of the kidney after administration of monomeric, low-osmolar, and dimeric, iso-osmolar CA by using diffusion-weighted magnetic resonance imaging (DWI).
First, the relationship between CA viscosity and the ADC of water was assessed by phantom measurements. Subsequently, Han Wistar rats (8 per group) received an intravenous injection of iso-osmolar CA (iodixanol) or low-osmolar CA (iopromide) at a dosage of 4 gI/kg body weight. The control group received saline (0.9% NaCl) at the same volume. The renal ADC was dynamically monitored up to 40 minutes postinjection (p.i.) by DWI using a 1.5-T clinical MR unit. After DWI, the animals were killed and the kidneys were removed for iodine measurements by x-ray fluorescence analysis.
The in vitro measurements yielded an inverse relationship between increasing viscosity and decreasing water diffusion. In vivo, a slight increase in ADC was observed immediately after administration of the low-osmolar iopromide (ΔADC=80±78 μm²/s) and saline (ΔADC=89±53 μm²/s), which normalized to the baseline level at 40 minutes p.i. In contrast, a strong decrease in ADC was observed after administration of the iso-osmolar iodixanol. This was most prominent 12 minutes p.i. (ΔADC=-555±194 μm²/s) and persisted throughout the investigation. Concomitantly, the kidney iodine concentration 50 minutes p.i. was significantly higher after iodixanol (58.6±5.3 mgI/g kidney) compared with iopromide injection (18.4±4.5 mgI/g kidney).
A significant difference in the renal ADC was observed between the low-osmolar CA/saline and the iso-osmolar CA. The in vitro measurements suggest that the substantial decrease in ADC observed after administration of the iso-osmolar CA is based on the high viscosity of the agent during renal passage. This, in turn, may explain the delayed iodine retention after administration of iso-osmolar CA and demonstrates the importance of the physicochemical properties of CA during their renal elimination.
X 射线对比剂(CA)具有特定的物理化学特性,通过肾小球滤过从肾脏排泄。因此,它们可能会影响肾脏内水分子的扩散。本临床前研究的目的是通过扩散加权磁共振成像(DWI)研究单体低渗和二聚体等渗 CA 给药后肾脏表观扩散系数(ADC)的潜在变化。
首先,通过体模测量评估 CA 粘度与水 ADC 之间的关系。随后,每组 8 只汉-威斯塔大鼠分别静脉注射等渗 CA(碘克沙醇)或低渗 CA(碘普罗胺),剂量为 4 gI/kg 体重。对照组给予相同体积的生理盐水(0.9%NaCl)。使用 1.5T 临床磁共振仪通过 DWI 动态监测注射后 40 分钟内的肾脏 ADC。DWI 后,处死动物,通过 X 射线荧光分析从肾脏中取出碘测量。
体外测量结果表明,随着粘度的增加,水扩散逐渐减少。体内,低渗碘普罗胺(ΔADC=80±78μm²/s)和生理盐水(ΔADC=89±53μm²/s)给药后立即观察到 ADC 略有增加,在 40 分钟时恢复到基线水平。相比之下,等渗碘克沙醇给药后观察到 ADC 明显下降。这在 12 分钟时最为明显(ΔADC=-555±194μm²/s),并持续整个研究过程。同时,碘克沙醇给药后 50 分钟时肾脏碘浓度(58.6±5.3mgI/g 肾脏)明显高于碘普罗胺(18.4±4.5mgI/g 肾脏)。
低渗 CA/生理盐水和等渗 CA 之间观察到肾脏 ADC 有显著差异。体外测量结果表明,等渗 CA 给药后 ADC 显著下降,是由于 CA 在肾脏通过时的高粘度所致。这反过来又可以解释等渗 CA 给药后碘的滞留延迟,并证明了 CA 在肾脏排泄过程中的物理化学特性的重要性。