基于离散元法的月壤水冰贯入冲击温度场仿真研究

Simulation Study on Heat Generation by Water-Ice Penetration Impact in Lunar Soil based on the Discrete Element Method

  • 摘要: CE-7任务计划采用钻进采样的方案获取原位含有水冰层理信息的月壤水冰样本。在月面极区真空低温环境下,月壤水冰胶结物对温度变化非常敏感,极易发生相变逃逸,导致层理信息丧失,降低其科学价值,这给采样技术带来巨大挑战。基于离散元法在真空低温环境下,对超声波钻贯入冲击不同含水率、初始温度的模拟月壤水冰温度场进行生热仿真研究,建立理论温度场计算模型并通过EDEM软件API接口二次开发出接触模型程序,采用最新月壤水冰热学参数,对真空低温下超声波钻钻进月壤水冰过程中的温度场变化进行仿真分析。其研究方法及所得实验与仿真结果,为真空低温环境中超声波钻冲击月壤水冰过程中的温度场变化研究提供了参考。

     

    Abstract: The CE-7 mission plans to adopt a drilling and sampling scheme to obtain in-situ lunar soil water ice samples with layering information. In the vacuum and low-temperature environment of the lunar polar regions, the lunar soil water ice cemented material is highly sensitive to temperature changes and is prone to phase change and escape, resulting in the loss of layering information and a reduction in its scientific value, which poses a significant challenge to the sampling technology. Based on the discrete element method, the heat generation simulation of the temperature field of the ultrasonic drill penetrating and impacting the simulated lunar soil water ice with different water contents and initial temperatures in a vacuum and low-temperature environment was conducted. A theoretical temperature field calculation model was established, and a contact model program was developed through the EDEM software API interface. Using the latest thermal parameters of lunar soil water ice, the temperature field changes during the ultrasonic drill’s penetration of lunar soil water ice in a vacuum and low-temperature environment were simulated and analyzed.

     

/

返回文章
返回