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Investigation of variable aeration of monodisperse mixtures: implications for pyroclastic density currents

Smith, Gregory M.; Williams, Rebecca; Rowley, Pete J.; Parsons, Daniel R.

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Authors

Gregory M. Smith

Rebecca Williams

Dr Peter Rowley Peter.Rowley@uwe.ac.uk
Senior Lecturer in Physical Geography/Earth Science/ Geology

Daniel R. Parsons



Abstract

© 2018, The Author(s). 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 (U mf_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 U mf_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 increases by up to 54% with an increase of slope from 2° to 4°. Deposit morphologies a primarily controlled by the spatial differences in aeration, where there is a 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.

Journal Article Type Article
Acceptance Date Jul 9, 2018
Online Publication Date Jul 18, 2018
Publication Date Aug 1, 2018
Deposit Date Jul 8, 2019
Publicly Available Date Jul 8, 2019
Journal Bulletin of Volcanology
Print ISSN 0258-8900
Electronic ISSN 1432-0819
Publisher Springer (part of Springer Nature)
Peer Reviewed Peer Reviewed
Volume 80
Issue 8
DOI https://doi.org/10.1007/s00445-018-1241-1
Keywords pyroclastic density current, experimental modelling, volcanology, sedimentology, bedforms, granular flow
Public URL https://uwe-repository.worktribe.com/output/1494156
Publisher URL http://doi.org/10.1007/s00445-018-1241-1
Additional Information Additional Information : The final publication is available at Springer via https://doi.org/10.1007/s00445-018-1241-1
Contract Date Jul 8, 2019

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