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张基伟, 刘书杰, 张松, 李方政, 韩玉福, 王磊. 富水砂层冻结壁形成过程声场响应特征研究[J]. 岩土工程学报, 2020, 42(12): 2230-2239. DOI: 10.11779/CJGE202012009
引用本文: 张基伟, 刘书杰, 张松, 李方政, 韩玉福, 王磊. 富水砂层冻结壁形成过程声场响应特征研究[J]. 岩土工程学报, 2020, 42(12): 2230-2239. DOI: 10.11779/CJGE202012009
ZHANG Ji-wei, LIU Shu-jie, ZHANG Song, LI Fang-zheng, HAN Yu-fu, WANG Lei. Response characteristics of sound fields of stratum frozen wall of water-rich sand during developing process[J]. Chinese Journal of Geotechnical Engineering, 2020, 42(12): 2230-2239. DOI: 10.11779/CJGE202012009
Citation: ZHANG Ji-wei, LIU Shu-jie, ZHANG Song, LI Fang-zheng, HAN Yu-fu, WANG Lei. Response characteristics of sound fields of stratum frozen wall of water-rich sand during developing process[J]. Chinese Journal of Geotechnical Engineering, 2020, 42(12): 2230-2239. DOI: 10.11779/CJGE202012009

富水砂层冻结壁形成过程声场响应特征研究

Response characteristics of sound fields of stratum frozen wall of water-rich sand during developing process

  • 摘要: 为了掌握富水砂层冻结壁形成过程超声波响应特征,利用NM-4A型非金属声波检测仪对广州地铁三号线北延伸冻结段-16 m层位进行超声波检测。基于此,根据孔隙介质热传导与压力声学理论,提出了人工冻结壁热-声耦合数值模拟方法。获得了富水砂层冻结过程中温度场-声场的演化特征与声学特征值变化规律。掌握了不同冻结锋面位置、孔间未交圈距离与波速之间的定量关系。总结了热-声耦合模型在冻结施工中应用思路与流程。①应用热-声耦合数值模拟方法求解出J1J2检测孔间的波速准确率为89.7%~96.97%;②超声波由冻土向未冻土的传播过程中反射与折射现象非常明显,根据声波理论计算出J1J2检测孔间声波平均反射系数为0.278、折射系数为1.278;③冻结早期在未冻土-冻土交界面附近出现明显的声压增高区域,声压场分布不均匀,且声线发生偏移。冻结后期无声压集中现象且声压场分布较均匀;④冻结壁发育过程中,波速随着冻结时间的增加而增加,而峰值声压、声强均随着冻结时间增加呈先减小后增加的趋势;⑤冻结锋面位置、冻结孔间未交圈距离均与波速之间呈非线性单调递增趋势,满足二次函数关系,相关性很好;⑥总结了热-声耦合模型应用思路与流程,可实现冻结壁发育状况的“早期预报、过程监测、效果评价”。

     

    Abstract: The ultrasonic tests on artificial frozen wall of water-rich sand stratum at depth of 16 m in Guangzhou Metro Line 3 are conducted by using NM-4A nonmetal ultrasonic test meter to study the response characteristics of sound fields during developing process of frozen wall. A thermoacoustic coupling numerical simulation method is proposed based on the heat conduction and pressure acoustic theory. The variation rule of temperature-sound field and acoustic characteristic value are obtained. The relationship among freezing front, unclosed distance and wave velocity is grasped. The application process of the thermoacoustic coupling model is summarized. The results are as follows: (1) The accuracy range of wave velocity is 89.7% to 96.97% betweenJ1and J2 holes by the numerical model. (2) The reflection and refraction are obvious when ultrasonic waves transmit from unfrozen soil to frozen soil. The average reflection and refraction coefficients are 0.278 and 1.278 betweenJ1 and J2holes. (3) The concentration area of acoustic pressure appears near the interface between unfrozen and frozen soils, and the sound field is inhomogeneous during early freezing period. Conversely, the sound field is homogeneous, and there is no pressure concentration area. (4) The wave velocity increases with the increasing freezing time, while both the acoustic pressure and the sound intensity increase first, then decrease as the freezing time increases. (5) Both the freezing front and the unclosed distance increase with the increasing wave velocity, and they meet quadratic function relations, indicating that the correlation is very good. (6) The application process of the thermoacoustic coupling model is summarized, which can achieve good effect on developing evaluation of frozen wall.

     

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