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高校地质学报 ›› 2026, Vol. 32 ›› Issue (05): 718-728.DOI: 10.16108/j.issn1006-7493.2025052

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海水环境下微生物注浆加固散体状强风化花岗岩模型试验研究

林文彬1, 2, 3,柳嘉豪1,高玉朋4,张智超2, 3,罗承浩5*,卢焱保5,罗立津6   

  1. 1. 福建理工大学 地球科学与工程研究所,福州 350118;
    2. 自然资源部丘陵山地地质灾害防治重点实验室,福州 350002;
    3. 福建省地质灾害重点实验室,福州 350002;
    4. 霍城县住房和城乡建设局 建设工程质量安全监督管理站,伊犁哈萨克自治州 835200;
    5. 福建永强岩土股份有限公司,龙岩 364000;
    6. 福建省微生物研究所,福州 350007
  • 出版日期:2026-10-20 发布日期:2026-10-20

Model-scale Test on Microbial Grouting Strengthening of Granular Strongly Weathered Granite in Seawater Environment

LIN Wenbin1,2,3,LIU Jiahao1,GAO Yupeng4,ZHANG Zhichao2,3,LUO Chenghao5*,LU Yanbao5,LUO Lijin6   

  1. 1. Institute of Earth Sciences and Engineering, Fujian University of Technology, Fuzhou 350118, China;
    2. Key Laboratory of Geohazard Prevention of Hilly Mountains, Fuzhou 350002, China;
    3. Key Laboratory of Geohazard, Fujian Province, Fuzhou 350002, China;
    4. Construction Engineering Quality and Safety Supervision Station, Huocheng County Bureau of Housing and Urban-Rural Development, Ili Kazakh Autonomous Prefecture 835200, China;
    5. Fujian Yonking Construction Geotechnical Co., Ltd., Longyan 364000, China;
    6. Fujian Institute of Microbiology, Fuzhou 350007, China
  • Online:2026-10-20 Published:2026-10-20

摘要: 利用微生物诱导碳酸钙沉淀(MICP)注浆技术对散体状强风化花岗岩进行模型尺度固化试验,并研究固化后试样的
物理力学性能及材料微观性能。试验结果表明,MICP技术能够将模型尺度(Φ25×50 cm)的散体状强风化花岗岩固结成型且质地坚硬。物理力学性能分析结果显示,试样中部固化效果较好,上部较差,下部居中;固化后试样平均碳酸钙生成率和干密度分别达到12.42%和1.85 g/cm3,渗透系数较未加固试样平均下降76.1%;无侧限抗压强度最高为5.01 MPa,平均值为3.42 MPa;固化后试样超声波速沿试样直径方向均值为2.919 km/s,较未加固试样(2.571 km/s)提高了13.5%,沿轴线方向均值为2.957 km/s。微观分析表明,MICP注浆生成的胶结物以条柱形、针簇型、片状的方解石为主,同时生成少量球型的球霰石和菱面体的镁方解石;试样中、下部生成的胶结物分布较均匀且堆积紧密,形成致密胶结网络,而上部胶结物相对松散。研究结果可为MICP技术固化散体状强风化花岗岩提供理论依据和数据支撑。

关键词: 微生物诱导碳酸钙沉淀, 模型尺度, 固化, 散体状强风化花岗岩, 微观试验

Abstract: Model-scale solidification tests were conducted on granular strongly weathered granite using microbially induced
calcite precipitation (MICP) grouting technology. The physical-mechanical properties and microstructural characteristics of the solidified specimens were systematically investigated. The results demonstrate that MICP successfully consolidated the modelscale granular strongly weathered granite (Φ25×50 cm) into a stiff coherent structure. Physical-mechanical analyses revealed spatial heterogeneity of cementation performance: optimal in the middle section, moderate in the lower section, and poorest in the upper section. The solidified specimens exhibited an average calcium carbonate content of 12.42% and a dry density of 1.85 g/cm3. The permeability coefficient decreased by an average of 76.1% compared to untreated material. The maximum unconfined compressive strength reached 5.01 MPa, with an average value of 3.42 MPa. The mean ultrasonic velocity was 2.919 km/s along the diameter direction (13.5% higher than untreated specimens at 2.571 km/s) and 2.957 km/s along the axial direction. Microscopic analyses indicate that MICP grouting mainly produces calcite cement with columnar, acicular-clusters, and platy morphologies, alongside minor spherical vaterite and rhombohedral magnesium-calcite. Cementation within the mid-lower sections shows relatively uniform distribution and dense packing, forming a compact network, whereas the upper section is relatively loose. This study provides theoretical basis and experimental data support for MICP-mediated solidification of granular strongly weathered granite. 

Key words: MICP, model-scale, solidification, granular strongly weathered granite, microscopic test

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