Multi-scale integration simulation of microbially induced carbonate precipitation using reaction-diffusion and homogenization models
Multi-scale integration simulation of microbially induced carbonate precipitation using reaction-diffusion and homogenization models
复制标题
使用反应扩散和均质化模型对微生物诱导碳酸盐沉淀进行多尺度集成模拟
DOI:
10.1007/s10064-022-02957-9
复制
发表时间:
2022
影响因子:
4.2
通讯作者:
Matsubara Hitoshi
中科院分区:
文献类型:
--
作者:
Nishimura Ibuki;Matsubara Hitoshi
Several microorganisms produce various minerals and emit less carbon dioxide than in the case when using concrete piles and/or cement milk as soil improvement materials. Therefore, bio-mediated soil improvement techniques such as microbially induced carbonate precipitation (MICP) are expected to become a feasible option to improve soil properties. Previous studies have determined the optimum MICP conditions, identified highly active species, analyzed changes in micro-structures, and predicted MICP effects based on laboratory experiments, field investigations, and numerical simulations. However, the understanding of the detailed dynamic behavior of MICP phenomena and the relationship between the time-dependent changes in MICP and the soil mechanical properties remains limited. In this study, a novel numerical scheme is proposed to bridge the gap between micro-scale and macro-scale structures in MICP involving the urea hydrolysis reaction; this scheme employs both a reaction–diffusion model for MICP calculation on the micro-scale and a homogenization model for the bridging method. The mechanical behavior of soil during MICP phenomena could also be calculated using the proposed scheme. The calculated concentrations of calcium carbonate relatively corresponded with the experimental results. Additionally, a simulation using the homogenization method revealed a stress concentration relaxation between soil particles during the MICP reaction.