Coupling simulation of microbial growth and MICP phenomena based on reaction-diffusion system

Ibuki Nishimura, H. Matsubara
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引用次数: 2

Abstract

Microbially induced carbonate precipitation (MICP) has been recognized as that microbial metabolism may induce a generation of calcium carbonates in the pores and/or on the surface of sand particles. However, only actual observations approach of inner structures by microscopes are difficult to understand the MICP process. In the current work, we propose a mathematical and numerical simulation model based on the reaction-diffusion system and finite difference method, respectively in order to understand dynamically calcium carbonate precipitation process and relationship between bacterial growth and precipitation. As a result, some temporal and spatial precipitation structures of calcium carbonate such as active and inactive bonds structures were obtained through some numerical examples, which are in good agreement with the existing experimental results.
基于反应扩散系统的微生物生长与MICP现象耦合模拟
微生物诱导碳酸盐沉淀(microally induced carbonate precipitation, MICP)被认为是微生物代谢可能在孔隙和/或砂粒表面诱导生成碳酸钙。然而,仅通过显微镜对内部结构进行实际观察是很难理解MICP过程的。本文提出了基于反应扩散系统和有限差分法的数学和数值模拟模型,以了解碳酸钙的动态沉淀过程以及细菌生长与沉淀的关系。通过数值算例得到了碳酸钙的一些时空沉淀结构,如活性键结构和非活性键结构,与已有的实验结果吻合较好。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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