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Study of formation of Lena River ice cover according of decade measurements by GPR

机译:GPR十年测量法研究莉娜河冰盖的形成

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Transformation of ice cover relief occurs during its freeze-up and by the action of hydro-meteorological factors. This article is dedicated to study of the formation of the Lena River ice cover based on a decade measurements in the hydrological station “Tabaga” (distance is 2 km). Two methods were applied for measuring the thickness of river ice: drilling method and GPR method. GPR data were obtained by GPR OKO-2 with antenna unit AB-400 (“Logis” LLC., Russia). Discrete drilling data (step is 100 m) and continuous GPR data of decade river - ice thickness measurements (distance between the probe points is 1 m) were presented. GPR data has shown an increase of average value of ice thickness from 93 cm to 142 cm from December to April, which corresponds to observations from the drilling data. Continuous GPR data provides more information and it reflects changes of river ice relief much more exactly than the drilling data. The ability of GPR for determining the dynamics of the seasonal variations in thickness of the Lena River ice cover is demonstrated.
机译:冰盖浮雕的转变发生在其冻结过程中,并且受水文气象因素的影响。本文基于“塔巴加”水文站(距离为2公里)的十年测量结果,致力于研究勒纳河冰盖的形成。测量河冰厚度的方法有两种:钻孔法和GPR法。 GPR数据是由GPR OKO-2使用天线单元AB-400(“ Logis” LLC。,俄罗斯)获得的。给出了离散钻井数据(步长为100 m)和连续十年GPR数据(十年河冰厚度测量)(探测点之间的距离为1 m)。 GPR数据显示,从12月到4月,冰厚度平均值从93 cm增加到142 cm,这与钻探数据的观察结果相对应。连续的GPR数据提供了更多的信息,它比钻井数据更准确地反映了河冰浮雕的变化。证明了GPR能够确定Lena河冰盖厚度季节性变化的动态。

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