4.7 Article

Homogeneity and mechanical behaviors of sands improved by a temperature-controlled one-phase MICP method

Journal

ACTA GEOTECHNICA
Volume 16, Issue 5, Pages 1417-1427

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s11440-020-01122-4

Keywords

Homogeneity; MICP; Quartz sand; Strength; Temperature

Funding

  1. National Natural Science Foundation of China [41831282, 51922024, 52078085]
  2. Natural Science Foundation of Chongqing, China [cstc2019jcyjjqX0014]
  3. National Science Foundation (NSF) [CMMI-1933355]

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A temperature-controlled one-phase MICP method was proposed to achieve uniform distribution, higher strength, and improved engineering properties of soil, demonstrating advantages over the normal two-phase MICP method in a series of experiments.
Microbially induced carbonate precipitation (MICP) has been actively investigated as a promising method to improve soil properties. A burning issue impeding its wide application is the severe spatial inhomogeneity of the CaCO3 distribution. Inspiring by the temperature sensitivity of the bacteria activity, a temperature-controlled one-phase MICP method is proposed consisting of two major steps: (1) grouting the specimen with the mixture of cementation and bacteria solutions in a low temperature; (2) inducing CaCO3 precipitation by exposing the specimen to room temperature. A series of experiments are conducted to demonstrate the advantages of the proposed method over the normal two-phase MICP method. Specimens treated with the proposed temperature-controlled method present higher CaCO3 contents with a roughly uniform distribution along the height of the specimen; the strength of those specimens are substantially improved with apparent dilatancy due to the effective bond network formed by the homogeneously distributed CaCO3 precipitation. SEM images indicate that the temperature-controlled method tends to form small crystals distributing uniformly on the grain surface, which may increase the roughness of the grain and the residual stress more effectively.

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