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Estimating the corrosion of compacted bentonite by a conceptual model based on microbial growth dynamics

机译:通过基于微生物生长动力学的概念模型估算压实膨润土的腐蚀

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摘要

The microbial corrosion of compacted bentonite by the dissolution of smectite is biophysically, chemically, and mathematically estimated using an energy conservation law established between Gibbs free energy of formation △G_f~0 from the elements of smectite and the energy required for the growth and living maintenance requirement of microorganisms. The growth and decay dynamics of microorganisms are described with a universal Monod-type equation in which the specific growth rate and decay coefficient are given as a function of time considering the rapid development of a population of microorganisms at an initial stage and, in addition, by introducing the change of a density of colonies and the development of bio-films with time. The solution revealed that the corrosion depth of compacted bentonite depended primarily on the population density of microorganisms that had initially adhered onto the surface, the maximum thickness of bio-films, and a population of microorganisms at a stable living stage, although they depended on the specific growth and the specific decay rate, the ratio of energy required for maintenance to that required for the growth and the microbial consumption efficiency of energy to Gibbs free energy of smectite. In conclusion, a mean population of microorganisms came to the maximum value of an order of 10~6 to 10~7 cells/cm~3 on the bentonite surface; the thickness of bio-films was 5-10 μm; and the microbial corrosion depth was estimated to be in the range of less than 0.2 to 2.0 mm per 10~5 years in nature, provided the density of smectite was kept to be 1.6 Mg/m~3 on the compacted bentonite.
机译:利用蒙脱石元素的吉布斯自由形成能△G_f〜0与生长和维持生命所需的能量之间建立的能量守恒定律,通过生物物理,化学和数学估算致密蒙脱石对膨润土的微生物腐蚀。微生物的需求。考虑到微生物种群在初始阶段的快速发展,用通用的Monod型方程式描述了微生物的生长和衰减动力学,在该方程式中,特定的生长速率和衰减系数是时间的函数。通过引入菌落密度的变化和生物膜随着时间的发展。该解决方案表明,压实膨润土的腐蚀深度主要取决于最初粘附在表面上的微生物的种群密度,生物膜的最大厚度以及处于稳定生活阶段的微生物种群,尽管它们取决于比生长和比衰变速率,维持所需能量与生长所需能量之比,以及微生物与蒙脱石的吉布斯自由能的微生物消耗效率。综上所述,膨润土表面微生物的平均数量达到最大值,约为10〜6〜10〜7细胞/ cm〜3。生物膜的厚度为5-10μm。假设蒙脱石在致密膨润土上的密度保持在1.6 Mg / m〜3,则每10〜5年微生物的腐蚀深度估计在每10〜5年小于0.2至2.0 mm的范围内。

著录项

  • 来源
    《Applied clay science》 |2010年第2期|43-50|共8页
  • 作者单位

    The University of Tokyo, School of Agriculture and Life Science, 1-1-7 Yayoi, Bunkyo-ku, Tokyo, Japan;

    Tokyo Institute of Technology, Division of Earth and Planetary Science, Tokyo, Japan;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    clay; corrosion; microorganism; bio-film; growth dynamics;

    机译:粘土;腐蚀;微生物;生物膜增长动力;
  • 入库时间 2022-08-17 13:55:26

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