Experimental study on improvement of weathered Pisha sandstone soil in Inner Mongolia section of the Yellow River Basin based on microbially induced carbonate precipitation technology
|更新时间:2026-06-25
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Experimental study on improvement of weathered Pisha sandstone soil in Inner Mongolia section of the Yellow River Basin based on microbially induced carbonate precipitation technology
WANG Yan-xing, LI Chi, GE Xiao-dong, et al. Experimental study on improvement of weathered Pisha sandstone soil in Inner Mongolia section of the Yellow River Basin based on microbially induced carbonate precipitation technology[J]. 2022, 43(3): 708-718.
DOI:
WANG Yan-xing, LI Chi, GE Xiao-dong, et al. Experimental study on improvement of weathered Pisha sandstone soil in Inner Mongolia section of the Yellow River Basin based on microbially induced carbonate precipitation technology[J]. 2022, 43(3): 708-718.DOI: 10.16285/j.rsm.2021.1010.
Experimental study on improvement of weathered Pisha sandstone soil in Inner Mongolia section of the Yellow River Basin based on microbially induced carbonate precipitation technology
Pishasandstone is a kind of special rock widely distributed in the middle and upperreaches of the Yellow River
which is composed of sand shale and argillaceoussandstone. Due to the low diagenetic degree
the poor cementation between sandgrains
the low structural strength
and containing a large number of clayminerals
its anti-weathering ability is weak. Pisha sandstone becomes sand when encountering wind and becomes mud whenencountering water
which is an important source of "sediment deliveryinto the Yellow River". Based on microbially induced carbonateprecipitation (MICP) technology
the weathered Pisha sandstone soil was improved and reinforced. Aiming to obtain good strengthof improved soil samples and combine with the analysis of physical propertiesand pore structure
the optimal scheme design of improvement for the soilscontaining many fine-grained soils was carried out. Under 12 workingconditions
the artificial control with crystal forms
crystal morphology
andcrystal size were carried out through three experimentalcontrol factors: the concentration of the bacterial solution
the dosage ratioof bacterial solution to calcium source solution
and the molar ratio ofcalcium to urea. The results show that when the urea consumption was 0.4 mol
using the test scheme that the bacterial solution concentration OD was 1.2
the ratio of bacterial solution to calcium source solution was 1:20
and the ratio of calcium to ureawas 1:1
it is found that the calcium carbonate crystal induced by microorganisms wasdeposited in the form of "20−30 μm calcite-vateriteaggregates". These aggregates were filled in the pores of the weatheredPisha sandstone soil to increase the soil compactness
and therefore the sample porosity was reduced by62.4%
enhancing the corrosion resistance. The improved soil also showed goodstrength characteristics with 1 MPa of unconfined compressive strength.Due to the filling and cementation of this calcium carbonate crystal
thestrength remained 43.6% after being saturated with water
which solved theproblem of the soil collapsing in water. The research results expand theapplication of MICP technology in the reinforcement of mixed soil with a largeamount of fine-grained soil and provide a theoretical and experimental basisfor the engineering application of the improvement of weathered Pisha sandstonesoil.