...
首页> 外文期刊>Advances in Water Resources >Modelling coupled microbial processes in the subsurface: Model development, verification, evaluation and application
【24h】

Modelling coupled microbial processes in the subsurface: Model development, verification, evaluation and application

机译:在地下耦合微生物过程的建模:模型开发,验证,评估和应用

获取原文
获取原文并翻译 | 示例
           

摘要

To study subsurface microbial processes, a coupled model which has been developed within a Thermal-Hydraulic-Chemical-Mechanical (THCM) framework is presented. The work presented here, focuses on microbial transport, growth and decay mechanisms under the influence of multiphase flow and bio-geochemical reactions. In this paper, theoretical formulations and numerical implementations of the microbial model are presented. The model has been verified and also evaluated against relevant experimental results. Simulated results show that the microbial processes have been accurately implemented and their impacts on porous media properties can be predicted either qualitatively or quantitatively or both. The model has been applied to investigate biofilm growth in a sandstone core that is subjected to a two-phase flow and variable pH conditions. The results indicate that biofilm growth (if not limited by substrates) in a multiphase system largely depends on the hydraulic properties of the medium. When the change in porewater pH which occurred due to dissolution of carbon dioxide gas is considered, growth processes are affected. For the given parameter regime, it has been shown that the net biofilm growth is favoured by higher pH; whilst the processes are considerably retarded at lower pH values. The capabilities of the model to predict microbial respiration in a fully coupled multiphase flow condition and microbial fermentation leading to production of a gas phase are also demonstrated.
机译:为了研究地下微生物的过程,提出了一种在热-液压-化学-机械(THCM)框架内开发的耦合模型。本文介绍的工作重点是在多相流和生物地球化学反应的影响下微生物的运输,生长和衰变机理。本文介绍了微生物模型的理论公式和数值实现。该模型已经过验证,并已根据相关实验结果进行了评估。模拟结果表明,微生物过程已得到精确实施,并且可以定性或定量地或同时预测它们对多孔介质性能的影响。该模型已被用于研究砂岩岩心中生物膜的生长,该砂岩岩心受到两相流和可变pH条件的影响。结果表明,多相系统中生物膜的生长(如果不受底物限制)在很大程度上取决于介质的水力特性。当考虑到由于二氧化碳气体溶解而导致的孔隙水pH值变化时,会影响生长过程。对于给定的参数范围,已表明较高的pH值有利于净生物膜的生长;而在较低的pH值下,该过程明显受阻。还展示了该模型在完全耦合的多相流条件下预测微生物呼吸的能力以及导致气相产生的微生物发酵的能力。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 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