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3D simulations of a pyroclastic surge as an example of a compressible suspension flow

机译:火山碎屑涌动的3D模拟,以可压缩悬浮流为例

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This paper demonstrates the usefulness of the CIP-combined unified procedure (C-CUP) to perform numerical simulations of a compressible flow of a suspension. As a conspicuous example of such a flow, we present three-dimensional numerical simulations of a pyroclastic surge, which spreads laterally over the ground surface during some volcanic eruptions as occurred at Unzen Volcano in 1991 -1995. Since a pyroclastic surge suspends numerous solid particles, the density of a pyroclastic surge cannot be approximated by the equation of state for an ideal gas. On the other hand, a pyroclastic surge greatly changes its density as it heats and expands the air mixed from the calm surroundings. The above characteristics bring unique features into the motion of a pyroclastic surge. The features are successfully simulated by C-CUP with a slight modification owing to the fact that C-CUP can incorporate the equation of state of an arbitrary form.
机译:本文演示了CIP联合统一程序(C-CUP)进行悬浮液可压缩流数值模拟的有用性。作为这种流动的一个明显例子,我们提出了火山碎屑潮的三维数值模拟,该火山碎屑潮在1991年至1995年的云仙火山爆发时,在某些火山喷发过程中横向分布在地面上。由于火山碎屑涌动会悬浮许多固体颗粒,因此火山碎屑涌动的密度无法通过理想气体的状态方程来估算。另一方面,火山碎屑浪涌在加热和膨胀来自平静环境的空气时会极大地改变其密度。上述特征为火山碎屑浪涌的运动带来了独特的特征。由于C-CUP可以合并任意形式的状态方程,因此可以通过C-CUP成功地对这些特征进行仿真,并稍加修改。

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