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首页> 外文期刊>Remote Sensing >Temporal Monitoring of the Soil Freeze-Thaw Cycles over a Snow-Covered Surface by Using Air-Launched Ground-Penetrating Radar
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Temporal Monitoring of the Soil Freeze-Thaw Cycles over a Snow-Covered Surface by Using Air-Launched Ground-Penetrating Radar

机译:空中发射探地雷达对积雪表面土壤冻融循环的时空监测

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摘要

We tested an off-ground ground-penetrating radar (GPR) system at a fixed location over a bare agricultural field to monitor the soil freeze-thaw cycles over a snow-covered surface. The GPR system consisted of a monostatic horn antenna combined with a vector network analyzer, providing an ultra-wideband stepped-frequency continuous-wave radar. An antenna calibration experiment was performed to filter antenna and back scattered effects from the raw GPR data. Near the GPR setup, sensors were installed in the soil to monitor the dynamics of soil temperature and dielectric permittivity at different depths. The soil permittivity was retrieved via inversion of time domain GPR data focused on the surface reflection. Significant effects of soil dynamics were observed in the time-lapse GPR, temperature and dielectric permittivity measurements. In particular, five freeze and thaw events were clearly detectable, indicating that the GPR signals respond to the contrast between the dielectric permittivity of frozen and thawed soil. The GPR-derived permittivity was in good agreement with sensor observations. Overall, the off-ground nature of the GPR system permits non-invasive time-lapse observation of the soil freeze-thaw dynamics without disturbing the structure of the snow cover. The proposed method shows promise for the real-time mapping and monitoring of the shallow frozen layer at the field scale.
机译:我们在裸露的农田上的固定位置测试了地面穿透雷达(GPR)系统,以监测积雪表面上的土壤冻融循环。 GPR系统由单喇叭天线和矢量网络分析仪组成,可提供超宽带步进频率连续波雷达。进行了天线校准实验,以从原始GPR数据中滤除天线和反向散射效应。在GPR设置附近,传感器安装在土壤中,以监测不同深度的土壤温度和介电常数的动态。通过对时域GPR数据进行反演来获取土壤介电常数,该数据着重于表面反射。在延时GPR,温度和介电常数测量中观察到土壤动力学的显着影响。特别是,清楚地检测到五次冻结和融化事件,表明GPR信号响应了冻结和融化土壤的介电常数之间的差异。 GPR衍生的介电常数与传感器观测值非常吻合。总体而言,GPR系统的离地性质允许在不干扰雪盖结构的情况下对土壤冻融动力学进行非侵入性的延时观察。所提出的方法为野外尺度的浅层冻结层的实时制图和监测提供了希望。

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