Moll H, Stumpf Th, Merroun M, Rossberg A, Selenska-Pobell S, Bernhard G
Institut für Radiochemie, Forschungszentrum Rossendorf e.V., P.O. Box 510119, D-01314 Dresden, Germany.
Environ Sci Technol. 2004 Mar 1;38(5):1455-9. doi: 10.1021/es0301166.
The influence of microorganisms on migration processes of actinides has to be taken into account for the risk assessment of potential high-level nuclear waste disposal sites. Therefore it is necessary to characterize the actinide-bacteria species formed and to elucidate the reaction mechanisms involved. This work is focused on the sulfate-reducing bacterial (SRB) strain Desulfovibrio äspöensis (D. äspöensis) DSM 10631T which frequently occurs in the deep granitic rock aquifers at the Aspö Hard Rock Laboratory (Aspö HRL), Sweden. We chose Cm(III) due to its high fluorescence spectroscopic sensitivity as a model system for exploring the interactions of trivalent actinides with D. äspöensis in the trace concentration range of 3 x 10(-7) mol/L. A time-resolved laser fluorescence spectroscopy (TRLFS) study has been carried out in the pH range from 3.00 to 7.55 in 0.154 mol/L NaCl. We interpret the pH dependence of the emission spectra with a biosorption forming an inner-sphere surface complex of Cm(III) onto the D. äspöensis cell envelope. This Cm(III)-D. äspöensis-surface complex is characterized by its emission spectrum (peak maximum at 600.1 nm) and its fluorescence lifetime (162 +/- 5 micros). No evidence was found for incorporation of Cm(III) into the bacterial cells under the chosen experimental conditions.
在对潜在的高放核废料处置场地进行风险评估时,必须考虑微生物对锕系元素迁移过程的影响。因此,有必要对形成的锕系元素 - 细菌物种进行表征,并阐明其中涉及的反应机制。这项工作聚焦于经常出现在瑞典阿斯波硬岩实验室(Aspö HRL)深层花岗岩含水层中的硫酸盐还原菌(SRB)菌株阿斯波脱硫弧菌(D. äspöensis)DSM 10631T。由于其高荧光光谱灵敏度,我们选择了Cm(III)作为模型系统,以探索三价锕系元素在3×10(-7) mol/L痕量浓度范围内与阿斯波脱硫弧菌的相互作用。在0.154 mol/L NaCl中,于pH值3.00至7.55范围内进行了时间分辨激光荧光光谱(TRLFS)研究。我们通过生物吸附来解释发射光谱的pH依赖性,即Cm(III)在阿斯波脱硫弧菌细胞包膜上形成内球表面络合物。这种Cm(III) - 阿斯波脱硫弧菌 - 表面络合物通过其发射光谱(峰值最大值在600.1 nm)及其荧光寿命(162±5微秒)来表征。在所选择的实验条件下,未发现有证据表明Cm(III)被纳入细菌细胞。