月壤熔融成型结构聚光太阳能热成像月面原位无损检测仿真研究(特邀)

    Simulation study on in-situ non-destructive detection of melt-formed lunar regolith structures using concentrated solar energy excited thermography (invited)

    • 为实现对月壤熔融成型结构的无损、原位、高效检测,以满足未来月球基地建造与维护的质量控制需求,文中提出并验证了一种基于聚光太阳能激励的红外热成像无损检测方法。该方案旨在利用月球表面充沛的太阳能作为原位激励源,以解决其他激励方式在月面应用时面临的能源可持续性难题。为系统探究该方法的检测机理与可行性,建立了“光–热”耦合的三维有限元仿真模型。首先设计了四组月壤熔融成型结构试件,试件表面中心区域设有不同直径(1~4 mm)与埋藏深度(0.2~0.5 mm)的圆形平底孔缺陷;其次模拟了地球室温环境、月球高温环境、月球低温环境等三种典型应用场景,对缺陷直径设置为1 mm的试件进行脉冲激励热成像仿真,对比了不同场景下的检测效果;最后在月球低温环境下对缺陷直径设置为2~4 mm的三组试件进行了脉冲激励热成像仿真,分析了缺陷直径对检测效果的影响。仿真结果表明:三种场景下温度场演变趋势大致相同,最佳检测窗口普遍出现在加热末期至降温前期,区别在于月球高温环境下,深层缺陷显现较早但背景温度过高导致缺陷轮廓辨识度下降;在相同激励条件下,较大尺寸缺陷产生的热信号具有更强的鲁棒性和更长的可观测时间窗口。

       

      Abstract:
      Objective The planning of lunar bases, represented by the International Lunar Research Station, is advancing lunar exploration into a new phase of “long-term utilization and in-situ resource transformation”. In-situ resource utilization (ISRU) of lunar regolith is crucial for constructing sustainable lunar habitats. However, the extreme lunar environment and manufacturing processes may introduce internal defects into regolith-based components, posing risks to structural integrity. Thus, developing in-situ non-destructive detection techniques is imperative. While infrared thermography offers significant advantages, its conventional excitation sources (e.g., halogen lamps, lasers) rely on external power supplies, presenting limitations for long-term lunar surface operations. To address this problem, this study proposes and investigates a novel in-situ infrared thermographic inspection method utilizing concentrated solar energy as the excitation source.
      Methods A three-dimensional finite element model coupling optical excitation with transient heat transfer was established. Four groups of lunar regolith simulant specimens with standardized dimensions (20 mm×15 mm×5 mm) were designed, each containing an array of flat-bottom hole defects at their surface center. These defects varied systematically in diameter (1-4 mm) and burial depth (0.2-0.5 mm). Numerical simulations were conducted under three characteristic scenarios: earth ambient temperature, lunar high-temperature, and lunar low-temperature environment. First, the detection process of a specimen with 1-mm diameter defects was simulated and compared across all three environments. Subsequently, the influence of defect size was analyzed by simulating specimens with defect diameters of 2-4 mm under the lunar low-temperature condition, using a pulsed heating protocol.
      Results and Discussions From the temperature distribution at typical times in earth ambient temperature scenario (Fig.5), lunar high-temperature scenario (Fig.6), lunar low-temperature scenario (Fig.7), it can be seen that the optimal detection window universally occurs during the late heating to early cooling phases across all scenarios, as the thermal excitation is sufficiently established while background thermal noise remains non-uniform, maximizing the temperature contrast between defects and the substrate. In the lunar high-temperature scenario, the elevated initial temperature combined with intense heating accelerates thermal diffusion, allowing deeper defects to manifest earlier. However, this advantage is offset by a significantly reduced thermal contrast due to the overall high background temperature, which compromises defect contour clarity and identifiable duration. As shown in temperature distribution of specimens with different defect diameters at typical times (Fig.8), under identical excitation conditions, larger defects produce thermal signals with greater robustness and a longer observable time window.
      Conclusions This study establishes a coupled "optical-thermal" 3D finite element simulation model, systematically demonstrating the feasibility of using concentrated solar excited infrared thermography for in-situ defect detection of lunar regolith molten structures. The temperature field evolution trends are generally similar across the three scenarios, with the optimal detection window commonly appearing during the late heating phase to the early cooling phase. The distinction lies in the lunar high-temperature environment, where deeper defects manifest earlier but the excessively high background temperature reduces the recognizability of defect contours. Under identical excitation conditions, larger-sized defects produce thermal signals with stronger robustness and a longer observable time window.

       

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