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Surface hoar characteristics derived from a snow micropenetrometer using moving window statistical operations

机译:使用移动窗口统计操作从雪显微渗透仪得出的表面灰白特征

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摘要

This study aims to improve analytical techniques for studying stratigraphic dimensions and hardness characteristics of thin weak layers in the mountain snowpack, with particular interest to buried surface hoar layers. By determining which structural characteristics of such weak layers are associated with shear strength, we may be better able to monitor and predict stability, which is relevant for avalanche forecasting and management. We utilize moving window statistical operations to analyze SnowMicroPen (SMP) penetrometer hardness profiles of a buried surface hoar layer. Results indicate that significant weak layer thinning and hardening of the interface between the weak layer and its substratum coincided with significant increases in shear strength, as measured using a size-corrected shear strength index derived from concurrent stability tests. With aging, variations in slab thickness appeared to positively affect the hardness and inversely affect the coefficient of variation (CoV) of hardness of weak layer boundaries. These findings support previous research that proposed the strengthening of buried surface hoar layers results from the gradual penetration of the surface hoar crystals into the substratum which allows stronger bonds to form at this critical interface. These analytical techniques allow stratigraphic dimensions and hardness characteristics to be quantified and analyzed, improving our ability to monitor stratigraphic characteristics associated with shear strength and stability of the mountain snowpack.
机译:这项研究旨在改进分析技术,以研究山区积雪薄薄弱层的地层尺度和硬度特征,特别是对地下埋藏的灰白层感兴趣。通过确定此类薄弱层的哪些结构特征与剪切强度相关联,我们可能能够更好地监视和预测稳定性,这与雪崩的预测和管理有关。我们利用移动窗口统计操作来分析SnowMicroPen(SMP)渗透仪的埋入表面白度层的硬度分布。结果表明,薄弱层和其底层之间的界面明显变薄和变硬,同时剪切强度也显着增加,这是通过使用同时进行的稳定性试验得出的尺寸校正后的剪切强度指数来衡量的。随着时效的发展,板坯厚度的变化似乎对硬度有正面影响,而对薄层边界的硬度的变化系数(CoV)则产生反作用。这些发现支持了先前的研究,该研究提出了增强掩埋的表面灰白层的结果,这是由于表面灰白晶体逐渐渗透到基底中而导致在该关键界面处形成更牢固的键合。这些分析技术可以对地层尺寸和硬度特征进行量化和分析,从而提高了我们监测与山地积雪的剪切强度和稳定性相关的地层特征的能力。

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