Properties and Behavior of Sandy Soils by a New Interpretation of MICP
- 1Japanese Geotechnical Association for Housing Disaster Prevention, 1622, Oshikiri, Shimizu-ku, Shizuoka 424-0008, Japan.
- 2Department of Geotechnical Engineering, Institute of Civil Engineering, Warsaw University of Life Sciences, Nowoursynowska 159, 02-776 Warsaw, Poland.
- 3Department of Building, Civil and Environment Engineering, Concordia University, 1455 de Maisonneuve Blvd. W., Montreal, QC H3G 1M8, Canada.
- 4Fudo Tetra Co., 7-2, Koami-Cho, Nihonbashi, Chuo-ku, Tokyo 103-0016, Japan.
- 5Chubu Sokuchi Research Institute Co., 801-1 Konami, Suwa City 392-0131, Japan.
- 6Sanko Kaihatsu Co., Ltd., 1320 Gokanjima, Fuji City 416-0946, Japan.
- 0Japanese Geotechnical Association for Housing Disaster Prevention, 1622, Oshikiri, Shimizu-ku, Shizuoka 424-0008, Japan.
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View abstract on PubMed
Summary
This summary is machine-generated.Microbial Induced Carbonate Precipitation (MICP) research faces challenges in quantifying microbial viability. This study establishes a new method using carbonate formation rate (CPR) to reliably estimate bacterial viability for improved MICP applications.
Area Of Science
- Geotechnical Engineering
- Microbiology
- Biogeochemistry
Background
- Microbial Induced Carbonate Precipitation (MICP) is an innovative ground improvement technology with expanding applications in soil stabilization and remediation.
- A significant challenge in MICP research is the accurate and quantitative evaluation of microbial viability, hindering consistent research outcomes and technology adoption.
- Bacterial properties can fluctuate over time and with environmental changes, complicating their use in engineering applications.
Purpose Of The Study
- To develop a reliable method for quantifying microbial viability in MICP applications, overcoming the limitations of traditional urease activity measurements.
- To establish a standard relationship between microbial mass (Optical Density - OD) and carbonate formation rate (CPR) for viable bacteria.
- To enable a unified evaluation of MICP technology, even with aged bacteria or when direct viability testing is not feasible.
Main Methods
- Defined the carbonate formation rate (CPR) as a function of microbial mass (OD) for viable bacteria, replacing urease activity measurements.
- Experimentally established a standard OD-CPR relationship.
- Introduced OD* to represent the required amount of microorganisms and defined the relationship OD = Rcv OD*, where Rcv is the viable bacterial rate, to convert between OD* and OD.
Main Results
- A method for estimating microbial viability was established based on the OD-CPR relationship.
- The Ca<sup>2+</sup>/OD ratio was identified as a critical factor controlling inhibition in MICP.
- Demonstrated that CPR is proportional to viable OD, Rcv, and OD* at a specific Ca<sup>2+</sup>/OD ratio (8.46 M), enabling unified evaluation using OD* with aged bacteria.
Conclusions
- The developed OD-CPR relationship and the use of OD* provide a standardized approach to evaluate MICP efficacy, irrespective of bacterial age or precise viability.
- This method overcomes the variability of bacterial properties, facilitating more consistent and comparable research results in MICP.
- The findings support the broader application and acceptance of MICP technology in geotechnical engineering and environmental remediation.
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