Abstract

The engineering practices for applying the microbial precipitation of carbonates require a design of the blending biocement solution (BCS). The BCS is usually blended with concentrated strains NO-A10, reaction media, such as urea and CaCl2, and a solvent, i.e., water or seawater. To characterize the BCS, the unknown microbial characteristics, such as the cell viability, are complex factors. Therefore, the optical density (OD) was redefined as Rcv OD*, in which OD* was the tentative OD of the BCS used and Rcv was the conversion rate concerning the cell viability. To determine Rcv values, a standard precipitation curve based on the precipitation rate at 24 h was determined. It was found that the curve was expressed by λ1 OD+ λ2 OD2, in which λ1 and λ2 were 8.46 M and −17.633 M, respectively. With this, the Rcv and OD values of unknown BCS were estimated from the results of precipitation tests using arbitrary OD* values. By extending the testing time, the second order term of OD or OD* was negligible. Accordingly, the precipitation amount is expressed as 8.46 OD, in which the OD can be estimated by precipitation tests using arbitrary OD* values of BCSs. Unless the Ca2+ value is dominant, the optimum blending of BCS can be determined by OD. Thus, it is concluded that the blending design of BCS is achieved using 8.46 OD, or 8.46 Rcv OD*, and the standard precipitation curve was defined in this study.

Highlights

  • 8.46 optical density (OD), in which the OD can be estimated by precipitation tests using arbitrary OD* values of biocement solution (BCS)

  • It is concluded that the blending design of BCS is achieved using 8.46 OD, or 8.46 Rcv OD*, and the standard precipitation curve was defined in this study

  • The results showed that the silty surface sediments at depths of up to 6 m below the sea bottom in Tokyo Bay and Osaka Bay showed increasing rates of 7.5 kPa vane shear strength per a 1.0% increase in carbonate content

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Summary

Introduction

The cementation process of natural sediments by carbonates is called carbonate diagenesis. The carbonates existing in the sediments are attributed to the buried effect of dead foraminifers and coccoliths [1–4] or biomineralization [5,6]. It was shown that natural deposited marine soils exhibited significant relationships between unconfined compressive strength and calcium carbonate contents [3]. The results showed that the silty surface sediments at depths of up to 6 m below the sea bottom in Tokyo Bay and Osaka Bay showed increasing rates of 7.5 kPa vane shear strength per a 1.0% increase in carbonate content. Silty sediments at a depth of approximately 24 m below the sea bottom off Haneda Airport showed an increase in unconfined compressive strength of 64 kPa per. Improvement in the carbonation technique in soil has been desired

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