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张鑫蕊, 孔纲强, 杨庆. 温度应力路径对原状海洋土强度特性影响研究[J]. 岩土工程学报, 2024, 46(2): 357-365. DOI: 10.11779/CJGE20221308
引用本文: 张鑫蕊, 孔纲强, 杨庆. 温度应力路径对原状海洋土强度特性影响研究[J]. 岩土工程学报, 2024, 46(2): 357-365. DOI: 10.11779/CJGE20221308
ZHANG Xinrui, KONG Gangqiang, YANG Qing. Influences of temperature stress path on strength characteristics of undisturbed marine sediments[J]. Chinese Journal of Geotechnical Engineering, 2024, 46(2): 357-365. DOI: 10.11779/CJGE20221308
Citation: ZHANG Xinrui, KONG Gangqiang, YANG Qing. Influences of temperature stress path on strength characteristics of undisturbed marine sediments[J]. Chinese Journal of Geotechnical Engineering, 2024, 46(2): 357-365. DOI: 10.11779/CJGE20221308

温度应力路径对原状海洋土强度特性影响研究

Influences of temperature stress path on strength characteristics of undisturbed marine sediments

  • 摘要: 室内温度和海底原位温度的差异导致传统测量所得海洋土物理力学参数存在一定差异。基于温控三轴仪,对我国南海原状海洋土进行了固结不排水剪切试验,实测了海洋土体变、强度、孔压以及模量的变化,探讨温度、温度循环、围压、超固结比等因素对原状海洋土力学性质的影响规律。试验结果表明:升温梯度增大会使正常固结海洋土热固结程度增大,其对应的排水体积和强度也增大;升温对超固结海洋土的排水体积具有增强作用,而温度降低了海洋土的强度;温度循环作用对超固结海洋土的排水体积具有增强作用,其对应的强度也增大;本文试验条件下,当OCR=1时,海洋土25℃下不排水抗剪强度测量结果比5℃下测量结果提高8.0%;当OCR=4时,海洋土25℃下不排水抗剪强度测量结果比5℃下测量结果降低1.9%;经过温度循环5℃—45℃—5℃后的抗剪强度比5℃提高了11.9%;4次或10次温度循环后分别提高了13.8%和17.8%。

     

    Abstract: The difference between the room and the in-situ temperatures leads to that of the measured physical and mechanical parameters of marine sediments. Based on the temperature-controlled triaxial apparatus, the consolidated undrained shear tests are carried out on the undisturbed marine sediments from the South China Sea. The changes of deformation, strength, pore pressure and modulus of the marine sediments are measured, and the influences of temperature, temperature cycle, confining pressure and over-consolidation ratio (OCR) on the mechanical properties of the undisturbed marine sediments are discussed. The results show that the increase of the temperature gradient increases the degree of thermal consolidation of the normally consolidated marine sediments, and the corresponding drainage volume and strength also increase. The temperature increases the drainage volume of the over-consolidated marine sediments, while the temperature decreases the strength of the marine sediments. The temperature cycle can enhance the drainage volume of the over-consolidated marine sediments, and its corresponding strength also increases. When OCR=1, the measured undrained shear strength of marine sediments at 25℃ is 8.0% higher than that at 5℃. When OCR=4, the measured undrained shear strength of marine sediments at 25℃ is 1.9% lower than that at 5℃. The shear strength after the temperature cycle of 5℃—45℃—5℃ is 11.9% higher than that at 5℃. After 4 or 10 temperature cycles, the shear strength increases by 13.8% and 17.8%, respectively.

     

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