Bubble mobility in mud and magmatic volcanoes
The rheology of particle-laden fluids with a yield stress, such as mud or crystal-rich magmas, controls the mobility of bubbles, both the size needed to overcome the yield stress and their rise speed. We experimentally measured the velocities of bubbles and rigid spheres in mud sampled from the Davi...
Saved in:
| Published in: | Journal of volcanology and geothermal research 2015-03, Vol.294 (C), p.11-24 |
|---|---|
| Main Authors: | , , |
| Format: | Article |
| Language: | eng |
| Subjects: | |
| Online Access: | Get full text |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| Summary: | The rheology of particle-laden fluids with a yield stress, such as mud or crystal-rich magmas, controls the mobility of bubbles, both the size needed to overcome the yield stress and their rise speed. We experimentally measured the velocities of bubbles and rigid spheres in mud sampled from the Davis–Schrimpf mud volcanoes adjacent to the Salton Sea, Southern California. Combined with previous measurements in the polymer gel Carbopol, we obtained an empirical model for the drag coefficient and bounded the conditions under which bubbles overcome the yield stress. Yield stresses typical of mud and basaltic magmas with sub-mm particles can immobilize millimeter to centimeter sized bubbles. At Stromboli volcano, Italy, a vertical yield stress gradient in the shallow conduit may immobilize bubbles with diameter ≲1cm and hinder slug coalescence.
•Bubbles are more mobile than rigid particles in muds for the same buoyancy.•A criterion for mobilizing bubbles is bounded for fluids with a yield stress.•Basaltic lavas and natural muds can immobilize centimeter-sized bubbles.•A vertical yield stress gradient in Stromboli's conduit can hinder coalescence. |
|---|---|
| ISSN: | 0377-0273 1872-6097 |