Investigation of soil processes on radar signature of landmines

D. Abrams, N. Lamie, G. Koh
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Abstract

Soil properties have a significant impact in the observed responses of various sensors for mine detection. Ground penetrating radar (GPR) is an important sensor for mine detection. The performance GPR is largely governed by the soil moisture content. Characterizing the spatial and temporal changes in the dielectric properties of soil surrounding the landmines represents a major challenge for radar evaluation studies. Laboratory and field studies are currently in progress to better document the effect of soil moisture variability on radar sensing of buried landmines. These studies are conducted using commercially available GPRs operating at 400 MHz and 1.5 GHz. The study site is a government mine test facility with various anti-tank (AT) and anti-personnel (AP) mines buried at different depths. The test lanes at this facility are grass-covered and the sub-surface root system plays an important role in modulating the soil properties. Our goal is to investigate the seasonal changes in soil processes at this site and to document how these processes impact the radar signatures of landmines.
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土壤过程对地雷雷达特征的影响研究
土壤性质对各种地雷探测传感器的观测响应有重要影响。探地雷达(GPR)是一种重要的地雷探测传感器。探地雷达的性能在很大程度上取决于土壤含水量。表征地雷周围土壤介电特性的时空变化是雷达评价研究的一个主要挑战。目前正在进行实验室和实地研究,以便更好地记录土壤湿度变化对雷达感应埋设地雷的影响。这些研究是使用400兆赫和1.5千兆赫的商用GPRs进行的。研究地点是一个政府地雷试验设施,在不同深度埋有各种反坦克(AT)和杀伤人员(AP)地雷。试验车道为草地覆盖,地下根系在调节土壤性质方面起着重要作用。我们的目标是调查该地点土壤过程的季节性变化,并记录这些过程如何影响地雷的雷达特征。
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