黄锐, 郭成超, 曹鼎峰, 等. 2024. 珊瑚钙质砂-聚氨酯高聚物复合体蠕变村山流变模型改进[J]. 工程地质学报, 32(1): 295-302. doi: 10.13544/j.cnki.jeg.2021-0737.
    引用本文: 黄锐, 郭成超, 曹鼎峰, 等. 2024. 珊瑚钙质砂-聚氨酯高聚物复合体蠕变村山流变模型改进[J]. 工程地质学报, 32(1): 295-302. doi: 10.13544/j.cnki.jeg.2021-0737.
    Huang Rui, Guo Chengchao, Cao Dingfeng, et al. 2024. An improved Murayama rheology model to describe the creep behavior of the mixture composed by calcareous sand and polyurethane polymer grouting[J]. Journal of Engineering Geology, 32(1): 295-302. doi: 10.13544/j.cnki.jeg.2021-0737.
    Citation: Huang Rui, Guo Chengchao, Cao Dingfeng, et al. 2024. An improved Murayama rheology model to describe the creep behavior of the mixture composed by calcareous sand and polyurethane polymer grouting[J]. Journal of Engineering Geology, 32(1): 295-302. doi: 10.13544/j.cnki.jeg.2021-0737.

    珊瑚钙质砂-聚氨酯高聚物复合体蠕变村山流变模型改进

    AN IMPROVED MURAYAMA RHEOLOGY MODEL TO DESCRIBE THE CREEP BEHAVIOR OF THE MIXTURE COMPOSED BY CALCAREOUS SAND AND POLYURETHANE POLYMER GROUTING

    • 摘要: 聚氨酯高聚物注浆可显著提高珊瑚钙质砂地基承载力,但目前缺乏模型准确描述注高聚物浆液加固后珊瑚钙质砂地基的蠕变。本文中推导了改进村山流变模型的理论公式,对复合体蠕变进行分段描述,采用一个与应力大小及时间有关的反比例函数代替传统村山流变模型中的黏滞系数。设计了室内蠕变单轴压缩试验,分别在100 kPa,200 kPa和400 kPa轴向应力下测定并建立了珊瑚钙质砂-高聚物复合体的蠕变量与蠕变时间的关系。试验结果表明:改进村山流变模型可有效描述珊瑚钙质砂-高聚物复合体蠕变全过程,当蠕变时间小于临界时间时,传统村山流变模型有效;当蠕变时间大于临界蠕变时间后,传统村山流变模型偏差随着时间增长而增大,而改进村山流变模型预测值与实测值具有很好一致性;复合体所处的应力水平越高,蠕变量越大,发生加速蠕变的时间也越早。

       

      Abstract: While grouting with polyurethane polymer significantly enhances the bearing capacity of coral calcareous sand foundations, accurately describing the total settlement and creep rate remains challenging. This study introduces an improved Murayama rheology model(IMRM)that pieceswisely describes the creep rate. The IMRM incorporates an inverse proportional function related to stress and time to replace the viscous coefficient in the traditional Murayama rheology model. The validity of the IMRM was assessed through uniaxial oedometer tests under pressures of 100, 200, and 400 kPa. The results indicate that the estimated values from the IMRM align well with the actually measured data throughout the entire experimental period. In contrast, the traditional Murayama rheology model proves effective only before the critical time. Higher stress applied to the soil samples results in larger settlements and an earlier occurrence of the critical time.

       

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