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Volume 56 Issue 7
Jul.  2026
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YAN Bangquan, WEI Mingli, WEI Wei, SHEN Shuiyue, SONG Yaru. Research on the Reduction Effect and Microbial Mineralization Mechanism of Cr-Contaminated Soil[J]. INDUSTRIAL CONSTRUCTION, 2026, 56(7): 187-198. doi: 10.3724/j.gyjzG25080103
Citation: YAN Bangquan, WEI Mingli, WEI Wei, SHEN Shuiyue, SONG Yaru. Research on the Reduction Effect and Microbial Mineralization Mechanism of Cr-Contaminated Soil[J]. INDUSTRIAL CONSTRUCTION, 2026, 56(7): 187-198. doi: 10.3724/j.gyjzG25080103

Research on the Reduction Effect and Microbial Mineralization Mechanism of Cr-Contaminated Soil

doi: 10.3724/j.gyjzG25080103
  • Received Date: 2025-08-01
    Available Online: 2026-08-31
  • Publish Date: 2026-07-20
  • This study systematically investigated the effectiveness of chemical reduction combined with microbial mineralization in remediating Cr(Ⅵ)-contaminated soil. The remediation performance was evaluated under varying cementation solution concentrations and curing ages using unconfined compressive strength tests and toxicity leaching experiments. Microstructural analysis was employed to elucidate the remediation mechanisms at the microscale, providing new theoretical foundations for the remediation of Cr(Ⅵ)-contaminated soil. The results demonstrated that the integrated chemical-microbial reduction-mineralization technology effectively remediated Cr(Ⅵ)-contaminated soil, achieving a compressive strength of 0.227 MPa in the solidified soil and reducing the Cr(Ⅵ) leaching concentration, with a removal efficiency exceeding 96%. Post-treatment analysis revealed that soil pH presented an initial decrease followed by a rise, and electrical conductivity exhibited a marked upward trend, which were primarily driven by urea hydrolysis reactions. Carbonate crystal formation was observed in treated samples, and X-ray diffraction and energy-dispersive spectroscopy (EDS) confirmed that hexavalent and trivalent chromium contaminants were immobilized through surface adsorption or lattice solid-solution mechanisms. Notably, Cr(Ⅲ) predominantly entered the calcite crystal structure through isomorphous substitution, forming stable calcium-chromium coprecipitates (Ca10Cr6O24(CO3)) characterized by low mobility and bioavailability.
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