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3D time-lapse imaging of polygonal patterned ground in the McMurdo dry valleys of Antarctica

机译:南极麦克默多干旱谷中多边形地面的3D延时成像

摘要

We surveyed four sets of polygons at 0.5 m line spacing using 100 and 200 MHz antennas for 3D GPR imagingat two field locations in the McMurdo Dry Valleys of Antarctica, one in Victoria Valley and the other in BeaconValley. The aim was to use 3D GPR and time-lapse 3D GPR to resolve subsurface structure and PPG process activityover the thaw season of polygonal patterned ground (PPG) in Antarctica. We applied migration and topographic corrections to the data sets before collating the data into 3D cubes. The subsurface structure can be analyzed using the processed profiles and resulting 3D data cubes. Signal was received down to 12 m (200 MHz) and 20 m (100 MHz) depth. Variations in salt concentrations, soil horizons and crack penetration may be interpreted using these data sets. The time-lapse images from Victoria Valley show reductions in signal through the season provisionally identified with changing quantities of free water and salts associated with PPG activity. The results show that 3D GPR allows the collection of valuable information about the subsurface structure and processes of PPG and provides a way to monitor changes in these processes as climatic conditions evolve.
机译:我们使用100和200 MHz天线在南极McMurdo干旱谷的两个野外地点,维多利亚谷和BeaconValley的两个野外地点,使用100和200 MHz天线对0.5米线距处的四组多边形进行了3D GPR成像。目的是使用3D GPR和延时3D GPR来解决南极洲多边形图案地面(PPG)融化季节的地下结构和PPG过程活动。在将数据整理为3D多维数据集之前,我们对数据集应用了迁移和地形校正。可以使用处理后的轮廓和生成的3D数据立方体来分析地下结构。接收信号的深度低至12 m(200 MHz),深度为20 m(100 MHz)。可以使用这些数据集来解释盐分浓度,土壤层位和裂缝渗透的变化。维多利亚山谷的延时图像显示,整个季节的信号减少,这是由于与PPG活性有关的游离水和盐含量的变化而临时确定的。结果表明,3D GPR允许收集有关PPG地下结构和过程的有价值的信息,并提供了一种方法来监视这些过程随气候条件的变化。

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