Wildung R E, Gorby Y A, Krupka K M, Hess N J, Li S W, Plymale A E, McKinley J P, Fredrickson J K
Pacific Northwest National Laboratory, Richland, Washington 99352, USA.
Appl Environ Microbiol. 2000 Jun;66(6):2451-60. doi: 10.1128/AEM.66.6.2451-2460.2000.
To help provide a fundamental basis for use of microbial dissimilatory reduction processes in separating or immobilizing (99)Tc in waste or groundwaters, the effects of electron donor and the presence of the bicarbonate ion on the rate and extent of pertechnetate ion [Tc(VII)O(4)(-)] enzymatic reduction by the subsurface metal-reducing bacterium Shewanella putrefaciens CN32 were determined, and the forms of aqueous and solid-phase reduction products were evaluated through a combination of high-resolution transmission electron microscopy, X-ray absorption spectroscopy, and thermodynamic calculations. When H(2) served as the electron donor, dissolved Tc(VII) was rapidly reduced to amorphous Tc(IV) hydrous oxide, which was largely associated with the cell in unbuffered 0. 85% NaCl and with extracellular particulates (0.2 to 0.001 microm) in bicarbonate buffer. Cell-associated Tc was present principally in the periplasm and outside the outer membrane. The reduction rate was much lower when lactate was the electron donor, with extracellular Tc(IV) hydrous oxide the dominant solid-phase reduction product, but in bicarbonate systems much less Tc(IV) was associated directly with the cell and solid-phase Tc(IV) carbonate may have been present. In the presence of carbonate, soluble (<0.001 microm) electronegative, Tc(IV) carbonate complexes were also formed that exceeded Tc(VII)O(4)(-) in electrophoretic mobility. Thermodynamic calculations indicate that the dominant reduced Tc species identified in the experiments would be stable over a range of E(h) and pH conditions typical of natural waters. Thus, carbonate complexes may represent an important pathway for Tc transport in anaerobic subsurface environments, where it has generally been assumed that Tc mobility is controlled by low-solubility Tc(IV) hydrous oxide and adsorptive, aqueous Tc(IV) hydrolysis products.
为了帮助为利用微生物异化还原过程在废物或地下水中分离或固定(99)Tc提供基本依据,测定了电子供体和碳酸氢根离子的存在对地下金属还原细菌腐败希瓦氏菌CN32对高锝酸根离子[Tc(VII)O(4)(-)]的酶促还原速率和程度的影响,并通过高分辨率透射电子显微镜、X射线吸收光谱和热力学计算相结合的方法评估了水相和固相还原产物的形态。当H(2)作为电子供体时,溶解的Tc(VII)迅速还原为无定形的Tc(IV)水合氧化物,在未缓冲的0.85% NaCl中,它主要与细胞结合,而在碳酸氢盐缓冲液中,则与细胞外颗粒(0.2至0.001微米)结合。与细胞相关的Tc主要存在于周质和外膜之外。当乳酸作为电子供体时,还原速率要低得多,细胞外的Tc(IV)水合氧化物是主要的固相还原产物,但在碳酸氢盐体系中,直接与细胞结合的Tc(IV)要少得多,可能存在固相的Tc(IV)碳酸盐。在有碳酸盐存在的情况下,还形成了可溶性(<0.001微米)的带负电的Tc(IV)碳酸盐络合物,其电泳迁移率超过了Tc(VII)O(4)(-)。热力学计算表明,实验中鉴定出的主要还原态Tc物种在天然水典型的一系列E(h)和pH条件下是稳定的。因此,碳酸盐络合物可能代表了厌氧地下环境中Tc迁移的一条重要途径,而在这种环境中,一般认为Tc的迁移受低溶解度的Tc(IV)水合氧化物和吸附性的水相Tc(IV)水解产物控制。