Abstract
Some of the least understood and most hazardous geologic processes involve complex multiphase flows, particularly those related to explosive volcanic eruptions. These phenomena inherently involve a wide range of characteristic length and time scales, as well as processes that are coupled across those scales in a range of flow regimes. For example, a pyroclastic density current's (pyroclastic flows and surges) behavior is governed in a complex way by the interactions between individual particles (∼10-4 to 10 1 meters, ∼10-1 to 101 seconds) and by turbulent mixing with surrounding air (∼10-2 to 102 meters, 1 to 102 seconds). Material properties within individual flows can vary over huge ranges; for example, when ascending magma interacts with groundwater in a volcanic conduit, the viscous melt and liquid water are transformed into brittle glass and steam.
| Original language | English |
|---|---|
| Pages (from-to) | 89-90 |
| Number of pages | 2 |
| Journal | Eos |
| Volume | 92 |
| Issue number | 11 |
| DOIs | |
| State | Published - 2011 |
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