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New developments in the analysis of column-collapse pyroclastic density currents through numerical simulations of multiphase flows

机译:多相流数值模拟分析柱塌陷火山碎屑流的新进展

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A granular multiphase model has been used to evaluate the action ofdifferently sized particles on the dynamics of fountains and associatedpyroclastic density currents. The model takes into account the overalldisequilibrium conditions between a gas phase and several solid phases, eachcharacterized by its own physical properties. The dynamics of the granularflows (fountains and pyroclastic density currents) has been simulated byadopting a Reynolds-averaged Navier-Stokes model for describing theturbulence effects. Numerical simulations have been carried out by usingdifferent values for the eruptive column temperature at the vent, solidparticle frictional concentration, turbulent kinetic energy, anddissipation. The results obtained provide evidence of the multiphase nature ofthe model and describe several disequilibrium effects. The low concentration(≤5 × 10−4) zones lie in the upper part of the granularflow, above the fountain, and above the tail and body of pyroclastic densitycurrent as thermal plumes. The high concentration zones, on the contrary,lie in the fountain and at the base of the current. Hence, pyroclasticdensity currents are assimilated to granular flows constituted by a lowconcentration suspension flowing above a high concentration basal layer(boundary layer), from the proximal regions to the distal ones. Interactionsamong the solid particles in the boundary layer of the granular flow arecontrolled by collisions between particles, whereas the dispersal ofparticles in the suspension is determined by the dragging of the gas phase.The simulations describe well the dynamics of a tractive boundary layerleading to the formation of stratified facies during Strombolian to Plinianeruptions.
机译:粒状多相模型已用于评估不同尺寸的颗粒对喷泉和相关的原土碎屑流的动力学的作用。该模型考虑了气相和几种固相之间的总体不平衡条件,每种条件都有其自身的物理特性。通过采用雷诺平均的Navier-Stokes模型来描述湍流效应,已经模拟了颗粒流的动力学(喷泉和碎屑密度流)。通过使用不同的排气孔喷柱温度,固体颗粒摩擦浓度,湍动能和耗散值进行数值模拟。获得的结果提供了该模型多相性质的证据,并描述了几种不平衡效应。低浓度区(≤5×10 −4 )区域位于颗粒流的上部,喷泉上方,热碎裂密度流尾部和主体上方,即热羽。相反,高浓度区位于喷泉中和水流的底部。因此,热碎屑密度流被同化为由低浓度悬浮液构成的颗粒流,该低浓度悬浮液从高浓度基底层(边界层)流过,从近端区域向远端区域流动。颗粒流边界层中固体颗粒之间的相互作用是由颗粒之间的碰撞控制的,而悬浮液中颗粒的分散则是通过气相的拖动来确定的。该模拟很好地描述了牵引边界层的动力学,从而形成了Strombolian到Plinian喷发期间的分层相。

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