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Soil Moisture and Thermal Behavior in the Vicinity of Buried Objects Affecting Remote Sensing Detection: Experimental and Modeling Investigation

机译:埋藏物体附近土壤水分和热行为影响遥感检测:实验和模型研究

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Improvements in buried mine detection using remote sensing technology rest on understanding the effects on sensor response of spatial and temporal variability created by soil and environmental conditions. However, research efforts on mine detection have generally emphasized sensor development, while less effort has been made to evaluate the effects of the environmental conditions in which the mines are placed. If the processes governing moisture and temperature distribution near the ground surface can be captured, sensor development and deployment can be more realistically tailored to particular operational scenarios and technologies. The objective of this study is to investigate the effects of the soil environment on landmine detection by studying the influence of the thermal boundary conditions at the land-atmosphere interface and the buried objects themselves on the spatial and temporal distribution of soil moisture around shallow-buried objects. Two separate large tank experiments were performed with buried objects with different thermal properties. Experimental results were compared to results from a fully coupled heat and mass transfer numerical model. Comparison of experimental and numerical results suggests that the vapor enhancement factor used to adjust the vapor diffusive flux described based on Fick's law is not necessary under dry soil conditions. Data and simulations from this study show that the thermal signature of a buried object depends on the complex interaction among a soil's water content and its thermal and hydraulic properties. Simulated thermal and saturation contrasts were generally very different for a buried landmine than for other buried objects.
机译:使用遥感技术对埋藏地雷探测的改进取决于了解土壤和环境条件对时空变化对传感器响应的影响。但是,有关地雷检测的研究工作通常着重于传感器的开发,而评估地雷放置环境条件的影响的工作却很少。如果可以捕获控制地面附近湿度和温度分布的过程,则可以针对特定的操作场景和技术更切合实际地调整传感器的开发和部署。这项研究的目的是通过研究陆地-大气界面处的热边界条件和埋藏物体本身对浅埋地下土壤水分时空分布的影响,研究土壤环境对地雷探测的影响。对象。对具有不同热特性的掩埋物体进行了两个单独的大罐实验。将实验结果与完全耦合的传热传质数值模型的结果进行了比较。实验和数值结果的比较表明,在干燥的土壤条件下,不需要根据菲克定律描述的用于调节蒸气扩散通量的蒸气增强因子。这项研究的数据和模拟表明,埋藏物体的热特征取决于土壤水分及其热力和水力特性之间的复杂相互作用。通常,埋藏的地雷与其他埋藏物体的模拟热力和饱和度对比有很大不同。

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