Temporal monitoring of the soil freeze-thaw cycles over snow-cover land by using off-ground GPR

K. Jadoon, S. Lambot, M. Dimitrov, L. Weihermuller
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引用次数: 2

Abstract

We performed off-ground ground-penetrating radar (GPR) measurements over a bare agricultural field to monitor the freeze-thaw cycles over snow-cover. The GPR system consisted of a vector network analyzer combined with an off-ground monostatic horn antenna, thereby setting up an ultra-wideband stepped-frequency continuous-wave radar. Measurements were performed during nine days and the surface of the bare soil was exposed to snow fall, evaporation and precipitation as the GPR antenna was mounted 110 cm above the ground. Soil surface dielectric permittivity was retrieved using an inversion of time-domain GPR data focused on the surface reflection. The GPR forward model used combines a full-waveform solution of Maxwell's equations for three-dimensional wave propagation in planar layered media together with global reflection and transmission functions to account for the antenna and its interactions with the medium. Temperature and permittivity sensors were installed at six depths to monitor the soil dynamics in the top 8 cm depth. Significant effects of soil dynamics were observed in the time-lapse GPR, temperature and permittivity data and in particular freeze and thaw events were clearly visible. A good agreement of the trend was observed between the temperature, permittivity and GPR time-lapse data with respect to five freeze-thaw cycles. The GPR-derived permittivity was in good agreement with sensor observations. The proposed method appears to be promising for the real-time mapping and monitoring of the frozen layer at the field scale.
利用离地探地雷达对积雪地区土壤冻融循环的实时监测
我们在一片光秃秃的农田上进行了探地雷达(GPR)测量,以监测积雪上的冻融循环。该探地雷达系统由矢量网络分析仪与离地单站喇叭天线相结合构成超宽带步进频率连续波雷达。测量进行了9天,由于GPR天线安装在离地面110厘米的地方,裸露的土壤表面暴露于降雪、蒸发和降水中。利用聚焦于地表反射的时域探地雷达数据反演反演土壤表面介电常数。所使用的探地雷达正演模型结合了三维波在平面层状介质中传播的麦克斯韦方程组的全波形解,以及考虑天线及其与介质相互作用的全局反射和传输函数。在6个深度安装温度和介电常数传感器,监测土壤顶部8 cm深度的动态。滞时探地雷达观测到土壤动力学的显著影响,温度和介电常数数据,特别是冻结和解冻事件清晰可见。在5次冻融循环中,温度、介电常数和探地雷达时移数据的变化趋势基本一致。gpr导出的介电常数与传感器观测值吻合较好。该方法有望实现冰冻层在野外的实时制图和监测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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