人工冻结法是一种利用热交换进行地层加固的施工技术,其加固效果受地层热物理性质影响明显。为了厘清复合地层内冻结加固体的发展规律,通过模型试验方法对于符合地层界面附近的温度场进行了研究。结果表明:复合地层界面附近的冻结壁形态会发生明显变化,整个冻结锋面在过渡区内呈线性增减;由复合地层界面向一侧过渡区边缘的距离为0.8~1.0 m;两个不同地层冻结壁发展速率的差异趋势相变潜热不同步释放会使得部分区域冻结壁在积极冻结中后期出现加速发展特点。针对过渡区温度场分布特点,给出了针对性的温度场解析解,并通过现场实测对其计算可靠性进行了验证。
The artificial ground freezing method is a construction technique that strengthens the formation through heat exchange, and its reinforcement effectiveness is significantly influenced by the thermo-physical properties of the formation. In order to clarify the development trend of frozen reinforcement in complex formations, a study was conducted on the temperature field near the formation interface through model experiments. The results show that: The morphology of the frozen wall near the complex formation interface will undergo significant changes, with the entire frozen front linearly increasing and decreasing in the transition zone. The distance from the complex formation interface to the edge of the transition zone is 0.8~1.0 m. The difference in the development rate of frozen walls of two different formations, as well as the asynchronous release of phase change latent heat, causes some frozen walls in certain areas to exhibit accelerated development characteristics in the later stages of active freezing. In response to the temperature field distribution characteristics in the transition zone, a targeted analytical solution for the temperature field is proposed, and its computational reliability is verified through on-site measurements.
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