...
首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Insights into the formation mechanism of vaterite mediated by a deep-sea bacterium Shewanella piezotolerans WP3
【24h】

Insights into the formation mechanism of vaterite mediated by a deep-sea bacterium Shewanella piezotolerans WP3

机译:深海细菌雪兰乳蛋白皮唑烷介导的Vaterite的形成机制见解WP3

获取原文
获取原文并翻译 | 示例
           

摘要

Microbially mediated carbonate mineralization plays a crucial role in biogeochemical cycling of carbon, as microbes can efficiently transform atmospheric CO2 and organic carbon into carbonate cements which represent a significant sink in the global carbon cycle. It is well established that diverse bacteria from various natural habitats can induce the precipitation of calcium carbonate, and an increasing number of bacteria were found to be able to mediate the mineralization of vaterite. However, the precise mechanisms for the formation of bacterial vaterite are not fully understood. To better understand the effect of bacterial activity on vaterite formation, Shewanella piezotolerans WP3 was selected as a model microbe to induce calcium carbonate mineralization. A combination of bacterial and biomimetic mineralization experiments was adopted. Different bacterial components including native cells, EPS-free cells, cell-bound EPS, soluble EPS, and small molecule organics were isolated from the cultures and used to influence calcium carbonate crystallization and growth. The identification and characterization of the mineralized products were done using field emission scanning electron microscopy (FESEM), X-ray powder diffraction (XRD), Raman spectroscopy, Fourier transform infrared spectroscopy (FT-IR), thermogravimetry and differential thermal analysis (TG-DTA), X-ray photoelectron spectroscopy (XPS), transmission electron microscopy (TEM) and selected area electron diffraction (SAED). Bacterial in situ mineralization experiments demonstrate that S. piezotolerans WP3 can not only promote the mineralization of calcium carbonate, but also mediate polymorph selection of vaterite. Biomimetic mineralization experiments involving individual bacterial components reveal that different bacterial components have different effects on calcium carbonate polymorphism, and low molecular-weight amino acids secreted by the bacteria play a dominant role on vaterite formation and stabiliza
机译:微生物介导的碳酸盐矿化在碳的生物地质化学循环中起着至关重要的作用,因为微生物可以将大气CO 2和有机碳有效地转化为在全球碳循环中表示显着汇率的碳酸盐水泥。很明显,各种天然栖息地的各种细菌可以诱导碳酸钙的沉淀,发现越来越多的细菌能够介导Vaterite的矿化。然而,不完全理解形成细菌Vaterite的精确机制。为了更好地了解细菌活性对Vaterite形成的影响,选择雪兰菜压电溶剂WP3作为模型微生物以诱导碳酸钙矿化。采用细菌和仿生矿化实验的组合。从培养物中分离出不同的细胞组分,包括天然细胞,无eps,细胞结合的EPS,可溶性EP和小分子有机物,并用于影响碳酸钙结晶和生长。使用现场发射扫描电子显微镜(FeSEM),X射线粉末衍射(XRD),拉曼光谱,傅里叶变换红外光谱(FT-IR),热重量和差分热分析(TG- DTA),X射线光电子能谱(XPS),透射电子显微镜(TEM)和选择的区域电子衍射(SAED)。原位矿化实验的细菌表明,S.压电溶剂素WP3不仅可以促进碳酸钙的矿化,还可以介导Vaterite的多晶型选择。涉及各种细菌组分的仿生矿化实验表明,不同的细菌成分对碳酸钙多态性不同,细菌分泌的低分子量氨基酸在Vaterite地层和稳定性上发挥着显性作用

著录项

相似文献

  • 外文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号