首页> 外文会议>American Society of Mechanical Engineers(ASME) Summer Heat Transfer Conference(HT2005) vol.1; 20050717-22; San Francisco,CA(UA) >NUMERICAL AND EXPERIMENTAL INVESTIGATION OF THERMAL SIGNATURES OF BURIED LANDMINES IN DRY SOIL
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NUMERICAL AND EXPERIMENTAL INVESTIGATION OF THERMAL SIGNATURES OF BURIED LANDMINES IN DRY SOIL

机译:干土中埋藏地雷的热学特征的数值和实验研究

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This paper reports a numerical and experimental investigation conducted to study the surface thermal signature of buried landmines. Numerical predictions are obtained by solving an unsteady three-dimensional energy balance model for heat transport in dry soil with a buried mine using the conservative finite-volume method. The model is validated by comparing generated results against published analytical and numerical data in addition to indoor measurements performed on dry soil inside an environmental chamber. The thermal signatures are observed while cooling takes place after exposing the soil surface to a radiant heat flux for a specified period. Transient temperature profiles produced numerically agree well with thermocouple measurements recorded at shallow soil depths and with surface IR images. The difference between predicted and measured surface temperatures is less than 0.4℃ and the difference in thermal signature is less than 0.3℃. Sit in The numerical model is also used to predict perturbations of the expected thermal signatures that are compared to the real (measured) ones from the IR images. The thermographic analysis shows good promise as a method for detecting shallowly buried land mines where not only the temperature difference or contrast images generated by the thermal signatures are matched between the IR images and the simulation images with high accuracy, but also the absolute temperatures for many images generated at discrete time intervals.
机译:本文报道了一项数值和实验研究,以研究埋藏地雷的表面热特征。通过使用保守的有限体积方法,通过求解埋藏矿山在干燥土壤中的热传递的非稳态三维能量平衡模型,获得了数值预测。通过对生成的结果与已发布的分析和数值数据进行比较,以及在环境室内对干燥土壤进行的室内测量,来验证模型的有效性。在将土壤表面暴露于辐射热通量达特定时间后进行冷却时,会观察到热信号。在数值上产生的瞬态温度曲线与在浅土深度处记录的热电偶测量值以及表面红外图像非常吻合。预测和测量的表面温度之间的差异小于0.4℃,并且热标记差异小于0.3℃。坐着数值模型还用于预测预期的热特征的扰动,将其与红外图像中的真实(测量)特征进行比较。作为一种检测浅埋地雷的方法,热成像分析显示出良好的前景,该方法不仅可以使红外图像和模拟图像之间高精度匹配由热信号生成的温度差或对比度图像,而且可以使许多人的绝对温度匹配以离散时间间隔生成的图像。

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