A combined field and numerical approach to understanding dilute pyroclastic density current dynamics and hazard potential: Auckland Volcanic Field, New Zealand

Brittany D. Brand, Darren M. Gravley, Amanda Clarke, Jan M. Lindsay, Simon H. Bloomberg, Javier Agustin-Flores, Károly Németh

Research output: Contribution to journalArticlepeer-review

25 Scopus citations

Abstract

The most dangerous and deadly hazards associated with phreatomagmatic eruptions in the Auckland Volcanic Field (AVF; Auckland, New Zealand) are those related to volcanic base surges - dilute, ground-hugging, particle laden currents with dynamic pressures capable of severe to complete structural damage. We use the well-exposed base surge deposits of the Maungataketake tuff ring (Manukau coast, Auckland), to reconstruct flow dynamics and destructive potential of base surges produced during the eruption. The initial base surge(s) snapped trees up to 0.5m in diameter near their base as far as 0.7-0.9km from the vent. Beyond this distance the trees were encapsulated and buried by the surge in growth position. Using the tree diameter and yield strength of the wood we calculate that dynamic pressures (Pdyn) in excess of 12-35kPa are necessary to cause the observed damage. Next we develop a quantitative model for flow of and sedimentation from a radially-spreading, dilute pyroclastic density currents (PDCs) to determine the damage potential of the base surges produced during the early phases of the eruption and explore the implications of this potential on future eruptions in the region. We find that initial conditions with velocities on the order of 65ms-1, bulk density of 38kgm-3 and initial, near-vent current thicknesses of 60m reproduce the field-based Pdyn estimates and runout distances. A sensitivity analysis revealed that lower initial bulk densities result in shorter run-out distances, more rapid deceleration of the current and lower dynamic pressures. Initial velocity does not have a strong influence on run-out distance, although higher initial velocity and slope slightly decrease runout distance due to higher rates of atmospheric entrainment. Using this model we determine that for base surges with runout distances of up to 4km, complete destruction can be expected within 0.5km from the vent, moderate destruction can be expected up to 2km, but much less damage is expected up to the final runout distance of 4km. For larger eruptions (base surge runout distance 4-6km), Pdyn of >35kPa can be expected up to 2.5km from source, ensuring complete destruction within this area. Moderate damage to reinforced structures and damage to weaker structures can be expected up to 6km from source. In both cases hot ash may still cause damage due to igniting flammable materials in the distal-most regions of a base surge. This work illustrates our ability to combine field observations and numerical models to explore the depositional mechanisms, macroscale current dynamics, and potential impact of dilute PDCs. Thus, this approach may serve as a tool to understand the damage potential and extent of previous and potential future eruptions in the AVF.

Original languageEnglish (US)
Pages (from-to)215-232
Number of pages18
JournalJournal of Volcanology and Geothermal Research
Volume276
DOIs
StatePublished - Apr 15 2014

Keywords

  • Auckland volcanic field
  • Base surge
  • Maar
  • Phreatomagmatic
  • Volcanic hazard assessment

ASJC Scopus subject areas

  • Geophysics
  • Geochemistry and Petrology

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