Investigation of variable aeration of monodisperse mixtures: implications for Pyroclastic Density Currents

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Gregory Smith, Rebecca Williams , Pete Rowley , Daniel R. Parsons


The high mobility of dense pyroclastic density currents (PDCs) is commonly attributed to high gas pore pressures. However, the influence of spatial and temporal variations in pore pressure within PDCs has yet to be investigated. Theory suggests that variability in the fluidisation and aeration of a current will have a significant control on PDC flow and deposition. In this study, the effect of spatially heterogeneous gas pore pressures in experimental PDCs was investigated. Sustained, unsteady granular currents were released into a flume channel where the injection of gas through the channel base was controlled to create spatial variations in aeration. Maximum current front velocity results from high degrees of aeration proximal to the source, rather than lower sustained aeration along the whole flume channel. However, moderate aeration (i.e. ~0.5 minimum static fluidisation velocity (Umf_st)) sustained throughout the propagation length of a current results in greater runout distances than currents which are closer to fluidisation (i.e. 0.9 Umf_st) near to source, then de-aerating distally. Additionally, although all aerated currents are sensitive to channel base slope angle, the runout distance of those currents where aeration is sustained throughout their lengths increase by up to 54% with an increase of slope from 2° to 4°. Deposit morphologies are primarily controlled by the spatial differences in aeration; where there is large decrease in aeration the current forms a thick depositional wedge. Sustained gas-aerated granular currents are observed to be spontaneously unsteady, with internal sediment waves travelling at different velocities.



Earth Sciences, Geology, Physical Sciences and Mathematics, Volcanology


fluidisation, flume, pyroclastic density currents, pore pressure, aerated currents, slope angle


Published: 2018-03-13 05:52

Last Updated: 2019-01-28 10:38

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