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The behaviour of snow under the effect of combined compressive and shear loading

机译:压缩和剪切联合荷载作用下的雪性

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The failure of a weak layer which lies underneath a more cohesive planar slab, is responsible for slab avalanche initiation. The weak layer may fail under combined effect of shear and compressive loading. Therefore, a preliminary study was carried out to understand the effect of combined compressive and shear loading on a weak snow layer. Since it is difficult to transport snow samples containing a weak layer into an environmental chamber, the mechanical measurements were carried out in situ. A digital force gauge attached to shear frame of area 0.01 m(2), was used to measure the shear strength. The compressive pressure was applied on the weak layer with the help of dead weights. The dynamic shear force at high loading rate (average around 25 N s(-1)) was applied for less than 1 sec and it was observed that the samples failed in a brittle manner. Experiments were carried out on round grain snow layer (RGsr), faceted snow (FCso) and near-surface faceted particles (FCsf) weak layer. Multi-axial stress response for FCsf snow layer was found to be entirely different from RGsr and FCso weak snow layers. Positive correlation between shear strength and compressive pressure was observed for RGsr and FCso snow layers. The experimental study revealed that there exists an elliptical envelope of instability for FCsf snow layer. The elliptical envelope for FCsf indicates that if the state of stress in the weak layer lies on the boundary or out of the elliptical envelope, the snowpack is unstable.
机译:位于粘结性更强的平板下面的薄弱层的破坏是导致平板雪崩引发的原因。弱层可能在剪切载荷和压缩载荷的共同作用下失效。因此,进行了一项初步研究,以了解压缩和剪切联合加载对弱雪层的影响。由于很难将包含薄弱层的雪样运输到环境室中,因此机械测量是在原位进行的。连接到面积为0.01 m(2)的剪切架的数字测力计用于测量剪切强度。借助自重将压缩压力施加在薄层上。在高加载速率下(平均25 N s(-1)左右)施加动态剪切力的时间少于1秒,并且观察到样品以脆性方式破坏。在圆粒雪层(RGsr),多面雪(FCso)和近表面多面颗粒(FCsf)薄弱层上进行了实验。发现FCsf雪层的多轴应力响应与RGsr和FCso弱雪层完全不同。 RGsr和FCso雪层的剪切强度与压缩压力之间呈正相关。实验研究表明,FCsf雪层存在椭圆形的不稳定性包络。 FCsf的椭圆包络表示如果弱层中的应力状态位于边界上或超出椭圆包络,则积雪不稳定。

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