Abstract

Microbially induced carbonate precipitation (MICP) is a promising technology for solidifying sandy soil, ground improvement, repairing concrete cracks, and remediation of polluted land. By solidifying sand into soil capable of growing shrubs, MICP can facilitate peak and neutralization of CO2 emissions because each square meter of shrub can absorb 253.1 grams of CO2 per year. In this paper, based on the critical review of the microbial sources of solidified sandy soil, models used to predict the process of sand solidification and factors controlling the MICP process, current problems in microbial sand solidification are analyzed and future research directions, ideas and suggestions for the further study and application of MICP are provided. The following topics are considered worthy of study: (1) MICP methods for evenly distributing CaCO3 deposit; (2) minimizing NH4+ production during MICP; (3) mixed fermentation and interaction of internal and exogenous urea-producing bacteria; (4) MICP technology for field application under harsh conditions; (5) a hybrid solidification method by combining MICP with traditional sand barrier and chemical sand consolidation; and (6) numerical model to simulate the erosion resistance of sand treated by MICP.

Highlights

  • Induced carbonate precipitation (MICP) is a promising technology applied to many civil and environmental engineering scenarios, especially combating desertification [1]

  • The other method is to use urea-producing bacteria existing in sandy soil, not by introducing exogenous bacteria, but by adding cementation solution and nutrients that facilitate the growth of indigenous bacteria

  • Their results showed that the pore structure has an important influence on the curing rate, the maximum urease rate has an indispensable influence on the hydraulic response of Microbially induced carbonate precipitation (MICP), and the MICP reaction rate is influenced by the concentration of the bacterial and cementation solutions

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Summary

Introduction

Induced carbonate precipitation (MICP) is a promising technology applied to many civil and environmental engineering scenarios, especially combating desertification [1]. Various sand consolidation methods emerged following extensive research, including sand fixation with the sand barrier, chemicals, and microbial grouting [7,8,9]. Microbial sand fixation refers to adding cementation solution to stimulate bacteria and forming calcium carbonate crystals in the sand to consolidate the sand. Progress in the research on microbial mineralized sandy soil is summarized, including ways of solidifying sandy soil, microbial sources of solidified sand, models used to predict the curing process of MICP in the field, factors that influence microbial solidification of sandy soil, the analysis of current problems and discussion on the prospects for the application of microbial sand consolidation technology in the future

Methods of Solidifying Sand
Microbial Sand Consolidation
Other Sand Fixation Methods
Microbial Sources of Solidified Sand
External Bacteria Solidifying the Sandy Soil
Solidification of Sandy Soil by Indigenous Bacteria
Models for Predicting the Curing Process of MICP in the Field
Factors Affecting Microbial Solidification of Sandy Soil
Concentration of Cementation Solution
Bacterial Concentration
Temperature
Sources of Calcium
Findings
Conclusions and Suggestions for Future Research
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