The effect of excavation and soil recovery on soil temperature and ground infrared radiation containing a metal-bearing block

IF 5.8 2区 工程技术 Q1 ENGINEERING, MECHANICAL International Journal of Heat and Mass Transfer Pub Date : 2025-02-10 DOI:10.1016/j.ijheatmasstransfer.2025.126802
Shengkang Hu , Yuge Han , Qunqing Lin , Dengfeng Ren
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Abstract

The effect of excavation and soil recovery on the soil temperature field and surface infrared properties is a critical factor in shallow subsurface target detection, yet it has not been sufficiently addressed in existing research. This study employs a combined discrete element method and MIE scattering model to simulate the changes in soil surface morphology and physical properties after the shallow burial of metal blocks in sandy, loamy, and clay soils. By integrating soil heat and moisture transfer with an infrared radiation model, we simulate the resulting temperature field and infrared radiation characteristics of the surface after excavation. The results indicate that the granularity of sandy soils and the high cohesion of clay soils lead to relatively minor changes in surface morphology and physical parameters in comparison to loamy soils. Infrared imaging analysis reveals that buried materials are most easily detected in loamy and clayey soils, while detection is more challenging in sandy soils. Furthermore, the comparison of temperature differences between the surface center and surrounding environment demonstrates that the characteristics of buried objects in loamy and clay soils are most pronounced at 12:00 and 24:00, enhancing the feasibility of underground target detection at these times. The study also found that different excavation speeds had a minimal impact on soil parameters at the surface. Faster excavation speeds increase shear stresses at the subsurface interface, thereby enhancing the density of the subsurface layer. Additionally, stronger solar radiation was found to improve the detection of buried objects, reducing the difficulty of underground target identification. The methodology proposed in this paper provides a more realistic approach to underground target detection by accounting for the dynamic changes in soil properties during excavation and recovery processes.
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开挖和土壤恢复对含金属块体土壤温度和地面红外辐射的影响
挖掘和土壤恢复对土壤温度场和地表红外特性的影响是浅层地下目标探测的关键因素,但现有研究尚未充分解决这一问题。本研究采用离散元法和MIE散射模型相结合的方法,模拟了金属块体在砂质、壤土和粘土中浅埋后土壤表面形态和物理性质的变化。将土壤热湿传递与红外辐射模型相结合,模拟了开挖后地表的温度场和红外辐射特征。结果表明,与壤土相比,砂土的粒度和粘土的高黏聚力导致其表面形态和物理参数的变化相对较小。红外成像分析表明,在壤土和粘性土中最容易检测到埋藏物,而在砂质土中检测更具有挑战性。此外,地表中心与周围环境的温差对比表明,壤土和粘土中埋地目标特征在12:00和24:00时最为明显,增强了在这两个时段探测地下目标的可行性。研究还发现,不同的开挖速度对地表土壤参数的影响最小。更快的开挖速度增加了地下界面处的剪应力,从而提高了地下层的密度。此外,更强的太阳辐射可以提高对地埋目标的检测,降低地下目标识别的难度。本文提出的方法考虑了挖掘和回收过程中土壤性质的动态变化,为地下目标探测提供了一种更为现实的方法。
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来源期刊
CiteScore
10.30
自引率
13.50%
发文量
1319
审稿时长
41 days
期刊介绍: International Journal of Heat and Mass Transfer is the vehicle for the exchange of basic ideas in heat and mass transfer between research workers and engineers throughout the world. It focuses on both analytical and experimental research, with an emphasis on contributions which increase the basic understanding of transfer processes and their application to engineering problems. Topics include: -New methods of measuring and/or correlating transport-property data -Energy engineering -Environmental applications of heat and/or mass transfer
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