高瑜, 姚德, 秦骁, et al. Study on Freeze-thaw Properties for Microbial Mineralization Geotechnical Materials in Salt Corrosion Environment[J]. 2018, 38(5): 787-794.
高瑜, 姚德, 秦骁, et al. Study on Freeze-thaw Properties for Microbial Mineralization Geotechnical Materials in Salt Corrosion Environment[J]. 2018, 38(5): 787-794. DOI: 10.13409/j.cnki.jdpme.2018.05.003.
Study on Freeze-thaw Properties for Microbial Mineralization Geotechnical Materials in Salt Corrosion Environment
the loose sandy soil was improved into microbial mineralized material.The changing rules of freeze-thaw properties of microbial mineralization materials
such as the apparent morphology
mass loss ratio
saturated water content
and unconfined compressive strength
with freezing and thawing cycles were studied through indoor freeze-thaw cycles experiment.Four different freeze-thaw solutions were used in this study.The results show that mineralized material appears spalling phenomenon in aqueous solution and salt solution with the increase of freeze-thaw cycles.Unconfined compressive strength decreases in the whole process of experiment.The loss of mass and the increase of saturated water content heavily affect the anti-frost properties of material.In 5% Na2 SO4 solution
mineralization material’s pulverization rate is faster and the quality loss rate is the largest
the damage is the fastest and most serious;in the NMR spectrum
when the relaxation time is longer than 200 ms
the change of the unfrozen water content is the largest in the freeze-thaw process
which is the main reason for the loss of the quality of the specimens and the destruction of the strength.The frost resistance of the specimens in the deionized aqueous solution is also weaker than in Na2 SO4 solution.The freezing point of the mineralization material reduces and the freezing resistance prolongs due to the presence of NaCl in the 3% NaCl solution and the mixed solution.This research provides basic experimental evidence for the engineering application of microbial mineralized material in cold regions.
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