来自吱吱作响的沙丘砂的声音力学

Pub Date : 2022-11-01 DOI:10.1250/ast.43.297
A. Patitsas
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引用次数: 0

摘要

验证了沙滩沙或其他吱吱作响的颗粒被杵踩踏或撞击时的声发射源位于杵正下方的薄剪切带中。这个带中的晶粒层以缓慢的令人毛骨悚然的速度相互滑动,通过粘滑效应,从冲击杵到颗粒接触区域剪切带中的弹性振动,产生能量传递。该振动能量依次供给沿垂直颗粒柱的弹性振动模态,或者等效地供给由振动柱组成的杵下剪切带的弹性振动模态,主导频率在1000hz范围内。寻找一个解释声学排放的推动下蓬勃发展的沙丘砂时叶片或自由雪崩,我们采用碰撞剪切带的概念,在那里,由于砂质量的高度流动性,颗粒层滑动一个在另一个以轻快的步伐,颗粒之间的平均碰撞频率在两个相邻的颗粒层定义了声发射的主要频率在100赫兹的范围。
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Sound mechanics from squeaky and booming dune sands
: It is verified that the source of the acoustic emissions when beach sand or other squeaky grains are stepped on or impacted by a pestle lies in a thin shear band directly under the pestle. The grain layers in this band slide one over another at a slow creepy pace giving rise to energy transfer, via the stick-slip effect, from the impacting pestle to the elastic vibrations in the shear bands at the grain contact areas. In turn, this vibration energy feeds the elastic modes of vibration along the vertical grain columns or equivalently, the elastic modes of vibration in the shear band under the pestle comprising the vibrating columns, with dominant frequency in the range of 1,000 Hz. In search of an explanation of the acoustic emissions when booming dune sand is pushed by a blade or is freely avalanching, we adopt the concept of the collision shear band, where, due to the high degree of fluidity of the sand mass, the grain layers slide one over another at a brisk pace so that the average collision frequency between grains in two adjacent grain layers defines the dominant frequency of the acoustic emission in the range of 100 Hz.
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