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特高硒环境中硒氧离子的细菌还原及其矿化机制
袁永强
导师朱建明 ; 刘丛强
2013
学位授予单位中国科学院研究生院
学位授予地点北京
学位名称博士
学位专业地球化学
关键词特高硒 碳质泥岩 亚硒酸盐 细菌还原 生物矿化机制
摘要湖北恩施渔塘坝是中国典型的高硒地区之一,硒在该地的富集引起了许多环境问题。本文以渔塘坝高硒碳质泥岩样品为研究对象,采用从其中筛选出的3株具有还原亚硒酸盐能力的细菌,包括地衣芽孢杆菌(Bacillus licheniformis SeRB-1)、芽孢杆菌(Bacillus sp. SeRB-2)和节杆菌(Arthrobacter sp. SeRB-3)作为研究工具,展开了细菌高耐受性、细菌还原亚硒酸盐动力学以及离子胁迫下的生物矿化的初步研究。通过以上研究,得到以下几点认识和结论。 (1) 碳质泥岩样品极度富集元素硒,其含量平均约3000 mg/kg,最高可达21830 mg/kg,属于特高硒样品。V、Mo、Cr、Zn、Cu、Ni等生物活性元素也表现出一定程度的富集,说明该泥岩样品的形成有生物活动参与。而泥岩样品中丰富的有机质和氮素的组成,以及疏松的结构为细菌生存创造条件。(2)耐受性实验表明,随Se(IV)浓度(1~10 mM)升高,细菌的倍增时间延长、生长速率变缓、生长抑制指数变大。实验得出细菌SeRB-1、SeRB-2和SeRB-3对亚硒酸盐的还原耐受浓度高达800 mM,其中细菌致死半数有效浓度高达100~150 mM,说明这3种菌属于高还原耐受亚硒酸盐菌。在耐受性实验中,细菌SeRB-1的延滞期较短、生长较快、适应性更强。 (3)还原实验表明,细菌对亚硒酸盐的还原主要集中在对数生长期和稳定期前期。还原一般分为两个阶段,阶段一是从开始接种到对数生长前期,该阶段细菌生长较慢,还原速率较小;阶段二是从对数前期末到取样结束,该阶段前期,细胞生长快、还原速率大,细菌达到稳定期后,还原速率又变小。通过不同浓度下细菌对亚硒酸盐还原的平均效率计算,结合米氏方程,推导出了3种细菌在Se(IV)浓度为1~10mM的平均还原动力学方程。细菌SeRB-1的为:Ci/V=76.14+13.72Ci;细菌SeRB-2的为Ci/V=61.49+13.21Ci和细菌SeRB-3的为Ci/V=58.96+13.51Ci。通过动力学方程,计算出了细菌SeRB-1、SeRB-2和SeRB-3的酶的特征常数分别为5.55 mM、4.65 mM和4.22 mM,最大反应速率分别为0.073μM/(L?h)、0.076 μM/(L?h)和0.074 μM/(L?h)。其中细菌SeRB-2对亚硒酸盐的最大还原速率更大,还原时间更长。 (4) 3种细菌对亚硒酸盐的还原效率随Se(IV)浓度(1~10 mM)升高而降低,在Se(IV)浓度为1mM时达到最大,其中细菌SeRB-2在该浓度下还原效率最高可达90%、SeRB-1和SeRB-3也分别达到70%~60%,说明这3种菌具有在硒污染场地修复的应用潜力,其中细菌SeRB-2更有优势,Se(IV)浓度不超过1mM时,能达到比较理想的处理效果。 (5) Fe+2和Cu+2胁迫下细菌SeRB-1对亚硒酸盐的还原矿化表明,离子胁迫下也有生物矿物生成,但其生成速度比单纯的细菌还原亚硒酸盐的速度要小。透射电镜观察揭示了不同时期,生物矿物生成过程。矿化初期,小颗粒矿物(10~20 nm)开始主要在细胞膜、少量在细胞质生成,颗粒沿细胞轮廓规则排列。矿化中期,细胞开始凋亡,部分细胞壁已完全分解,粘附在细胞膜上的矿物颗粒暴露在外;细胞质出现空泡, 并被矿物颗粒补充。此阶段矿物颗粒增大(100~200 nm),仍较有规律的沿细胞轮廓或胞内空洞周边分布,也有部分颗粒从细胞表面脱落或通过胞吐作用进入培养基,而呈游离状。矿化后期,细胞几乎溶解完毕,少量颗粒粘附在细胞残体,大量的颗粒聚集成团,此阶段矿物粒径更大(300~500 nm)。成分分析表明,矿物是元素硒与某种或多种铜硒或铁硒化物的混合物,这为生物成矿作用提供佐证,也说明细菌可以通过还原、矿化来固定污染物。 总之,通过特高硒环境中细菌还原亚硒酸盐的研究,得到了动力学方程,量化表达了细菌对亚硒酸盐的还原过程,为高硒地区的污染修复提供了参考;通过离子胁迫下的生物矿化研究,揭示了生物矿化过程,为矿物的生物成因提供了新的认识,也为生物矿化机制的进一步研究提供了研究路径。
其他摘要Yutangba, in Enshi City, Hubei Province, is one of the typical high-Se areas in China,and it has given rise to lots of environmental problems, due to selenium enrichment in local biotope. Using Se-laden carbonaceous mudstones as studying subjects, and three Se(IV)-reducing strains, Bacillus licheniformis SeRB-1, Bacillus sp. SeRB-2, and Arthrobacter sp. SeRB-3, screened form the mudstones, as researching tools, we preliminary studied the high Se(IV)-resistant cabalicity of strains, kinetics of selenite bioreduction and biomineralization under ion stress. Based on the above studies, major conclusions are drawn as follows. (1) The carbonaceous mudstones are super high-Se samples, within selenium highly enriched, and the average concentration is as high as 3000 mg/kg, with the highest value to 21830 mg/kg. The enrichment of bioactive elements, V, Mo, Cr, Zn, Cu and so on, tells that there are biological activity enrolling in the formation of the mudstones. While, the rich organic matter and nitrogen composition, and the unconsolidated structures create survival conditions for bacteria. (2) It shows that the doubling time got longer, growth rate turned smaller, and percentages of growth inhibition became larger, with the increasing of Se(IV) concentration, from the Se(IV)-resistant experiments. It also tells that the Se(IV)-reducing tolerance concentration is as high as 800 mM, and the median lethal concentration is high to 100~ 150 mM, indicating the strains belonging to high Se(IV)-reducing tolerance bacteria. Of which, strain SeRB-1 is better, with faster growing rate and short lag phase. (3) It illustrates that selenite reduction is mainly concentrated in exponential phase and earlier stationary phase. The reduction is generally divided into two stages. Stage I: From inoculation to earlier logarithmic growth phase, in this phase, cells grew slowly and the reducing ratio was small. Stage II: From the end of earlier logarithmic growth phase to time over, in later logarithmic phase, cells grew most quickly and the reducing ratio was largest,especially from 12~24 h. After that, in the stationary phase, reducing ratio turned smaller again. Finally, the average Se(IV)-reducing kinetics of the three strains at the concentrations from 1~10 mM were obtained, through average reducing efficiency calculating at each concentration and combining Michaelis-Menten equation. The kinetic equations of strains SeRB-1, SeRB-2 and SeRB-3 are Ci/V=76.14+13.72Ci, Ci/V=61.49+13.21Ci, and Ci/V=58.96+13.51Ci, respectively. According to which, Michaelis constants Km of enzyme reaction and maximum growth rate Vmax were calculated. The Km values are 5.55 mM, 4.22 mM and 4.65 mM and Vmax values are 0.073 μM/(L?h), 0.076 μ M/(L?h) and 0.074 μ M/(L?h), for SeRB-1, SeRB-2 and SeRB-3, respectively. Of which, strain SeRB-2 has a larger Vmax and longer reducing time. (4) The Se(IV)-reducing efficiency is dreasing with selenite concentrations increasing from 1 mM to 10 mM, and the maxnium reducing efficiency (or RE) was reached at Se(IV)=1 mM. Of which, the RE value of strain SeRB-2 is high to 90%, with 70% and 60% followed for SeRB-1 and SeRB-3, respectively. It indicates these bacteria have the application potential in bioremediation of selenium-contaminated sites, and strain SeRB-2 is more advantage. More Satisfied results would be obtained when selenite concentration is no more than 1mM. (5) There are also biominerals formation, during selenite bioreduction under Cu+2 and Fe+2 stress, but the rate is much slower than selenite bioreduction. Transmission electron microscopy revealed the process of biomineral formation at different periods. In earlier period, small granules(10~20 nm) were present mainly on the membranes, a few in the cytoplasm, and they are regular arranged around the cell envelopes. In the middle period, cells lysis appeared, and partial cell walls were completely decomposed, only leaving larger mineral particles exposed outside. Cytoplasm appeared vacuoles, and larger particles filled the vacancies. These particles, about 100~20 
学科领域环境地球化学
语种中文
文献类型学位论文
条目标识符http://ir.gyig.ac.cn/handle/352002/5815
专题研究生_研究生_学位论文
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袁永强. 特高硒环境中硒氧离子的细菌还原及其矿化机制[D]. 北京. 中国科学院研究生院,2013.
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