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Pore-scale network modeling of microbially induced calcium carbonate precipitation: Insight into scale dependence of biogeochemical reaction rates

机译:微生物引起的碳酸钙沉淀的孔尺度网络建模:对生物地球化学反应速率的尺度依赖性的认识

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摘要

The engineering of microbially induced calcium carbonate precipitation (MICP) has attracted much attention in a number of applications, such as sealing of CO2 leakage pathways, soil stabilization, and subsurface remediation of radionuclides and toxic metals. The goal of this work is to gain insight into pore-scale processes of MICP and scale dependence of biogeochemical reaction rates. This will help us develop efficient field-scale MICP models. In this work, we have developed a comprehensive pore-network model for MICP, with geochemical speciation calculated by the open-source PHREEQC module. A numerical pseudo-3-D micromodel as the computational domain was generated by a novel pore-network generation method. We modeled a three-stage process in the engineering of MICP including the growth of biofilm, the injection of calcium-rich medium, and the precipitation of calcium carbonate. A number of test cases were conducted to illustrate how calcite precipitation was influenced by different operating conditions. In addition, we studied the possibility of reducing the computational effort by simplifying geochemical calculations. Finally, the effect of mass transfer limitation of possible carbonate ions in a pore element on calcite precipitation was explored.
机译:微生物引起的碳酸钙沉淀(MICP)的工程在许多应用中引起了很多关注,例如密封CO2泄漏途径,土壤稳定以及放射性核素和有毒金属的地下修复。这项工作的目的是深入了解MICP的孔隙尺度过程以及生物地球化学反应速率的尺度依赖性。这将帮助我们开发有效的现场规模MICP模型。在这项工作中,我们开发了MICP的综合孔隙网络模型,并通过开源PHREEQC模块计算了地球化学形态。通过一种新型的孔网生成方法,生成了数值伪-3-D微观模型作为计算域。我们在MICP的工程设计中模拟了一个三个阶段的过程,包括生物膜的生长,富含钙的培养基的注入以及碳酸钙的沉淀。进行了许多测试案例,以说明方解石沉淀如何受到不同操作条件的影响。此外,我们研究了通过简化地球化学计算来减少计算量的可能性。最后,探讨了孔隙元素中可能存在的碳酸根离子的传质限制对方解石沉淀的影响。

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  • 来源
    《Water resources research》 |2016年第11期|8794-8810|共17页
  • 作者单位

    Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands;

    Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands;

    Imperial Coll, Dept Earth Sci & Engn, London, England|ETH, Dept Earth Sci, Inst Geophys, Geothermal Energy & Geofluids Grp, Zurich, Switzerland;

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