Resources (1-19 of 19)

1. Molten Fuel Coolant Interaction: tx08

   02 Feb 2018 | Contributor(s):: Ingo Sonder, Bernd Zimanowski, Greg A Valentine, Alison Graettinger, Andrew Harp

   Date: 2015-05-20Location: Physikalisch Vulkanologisches Labor, Universität Würzburg, GermanyMolten Fuel Coolant Interaction with Remelted Volcanic Rock. Mixing of ambient temperature water at 3.6 m/s injection speed with natural remelted (basaltic) volcanic rock at...

2. Molten Fuel Coolant Interaction: tx02

   out of 5 stars 

   02 Feb 2018 | Contributor(s):: Ingo Sonder, Bernd Zimanowski, Greg A Valentine, Alison Graettinger, Andrew Harp

   Date: 2015-05-20Location: Physikalisch Vulkanologisches Labor, Universität Würzburg, GermanyMolten Fuel Coolant Interaction with Remelted Volcanic Rock. Mixing of ambient temperature water at 3.6 m/s injection speed with natural remelted (basaltic) volcanic rock at...

3. Explosive Magma-Water Interaction: ir03

   out of 5 stars 

   15 Dec 2017 | Contributor(s):: Ingo Sonder

   Date: 2016-08-10Location: University at Buffalo, Geohazards Field Station, Springville/Ashford, NY, USA.Mixing of ambient temperature water at 1.9 m/s injection speed with natural remelted (basaltic) volcanic rock at 1300ºC.This is video material was recorded for one of our...

4. Explosive Magma-Water Interaction: ir04

   out of 5 stars 

   15 Dec 2017 | Contributor(s):: Ingo Sonder

   Date: 2016-08-12Location: University at Buffalo, Geohazards Field Station, Springville/Ashford, NY, USA.Mixing of ambient temperature water at 2.7 m/s injection speed with natural remelted (basaltic) volcanic rock at 1300ºC.This is video material was recorded for one of our...

5. Explosive Magma-Water Interaction: ir05

   out of 5 stars 

   15 Dec 2017 | Contributor(s):: Ingo Sonder

   Date: 2016-08-12Location: University at Buffalo, Geohazards Field Station, Springville/Ashford, NY, USA.Mixing of ambient temperature water at 2.7 m/s injection speed with natural remelted (basaltic) volcanic rock at 1300ºC.This is video material was recorded for one of our...

6. Explosive Magma-Water Interaction: ir06

   out of 5 stars 

   15 Dec 2017 | Contributor(s):: Ingo Sonder

   Date: 2016-08-24Location: University at Buffalo, Geohazards Field Station, Springville/Ashford, NY, USA.Mixing of ambient temperature water at 2.5 m/s injection speed with natural remelted (basaltic) volcanic rock at 1300ºC.This is video material was recorded for one of our...

7. Explosive Magma-Water Interaction: ir07

   out of 5 stars 

   15 Dec 2017 | Contributor(s):: Ingo Sonder

   Date: 2016-08-24Location: University at Buffalo, Geohazards Field Station, Springville/Ashford, NY, USA.Mixing of ambient temperature water at 1.8 m/s injection speed with natural remelted (basaltic) volcanic rock at 1300ºC.This is video material was recorded for one of our...

8. Explosive Magma-Water Interaction: ir12

   out of 5 stars 

   15 Dec 2017 | Contributor(s):: Ingo Sonder

   Date: 2016-09-21Location: University at Buffalo, Geohazards Field Station, Springville/Ashford, NY, USA.Mixing of ambient temperature water at 2.2 m/s injection speed with natural remelted (basaltic) volcanic rock at 1300ºC.This is video material was recorded for one of our...

9. Explosive Magma-Water Interaction: ir13

   out of 5 stars 

   15 Dec 2017 | Contributor(s):: Ingo Sonder

   Date: 2016-11-02Location: University at Buffalo, Geohazards Field Station, Springville/Ashford, NY, USA.Mixing of ambient temperature water at 2.5 m/s injection speed with natural remelted (basaltic) volcanic rock at 1300ºC.This is video material was recorded for one of our...

10. Explosive Magma-Water Interaction: ir14

    out of 5 stars 

    15 Dec 2017 | Contributor(s):: Ingo Sonder

    Date: 2016-11-27Location: University at Buffalo, Geohazards Field Station, Springville/Ashford, NY, USA.Mixing of ambient temperature water at 2.3 m/s injection speed with natural remelted (basaltic) volcanic rock at 1300ºC.This is video material was recorded for one of our...

11. Explosive Magma-Water Interaction: ir15

    out of 5 stars 

    15 Dec 2017 | Contributor(s):: Ingo Sonder

    Date: 2016-11-27Location: University at Buffalo, Geohazards Field Station, Springville/Ashford, NY, USA.Mixing of ambient temperature water at 4.5 m/s injection speed with natural remelted (basaltic) volcanic rock at 1300ºC.This is video material was recorded for one of our...

12. Explosive Magma-Water Interaction: ir16

    out of 5 stars 

    15 Dec 2017 | Contributor(s):: Ingo Sonder

    Date: 2017-01-21Location: University at Buffalo, Geohazards Field Station, Springville/Ashford, NY, USA.Mixing of ambient temperature water at 2.7 m/s injection speed with natural remelted (basaltic) volcanic rock at 1300ºC.This is video material was recorded for one of our...

13. Explosive Magma-Water Interaction: pr05

    out of 5 stars 

    15 Dec 2017 | Contributor(s):: Ingo Sonder

    Date: 2017-09-13Location: University at Buffalo, Geohazards Field Station, Springville/Ashford, NY, USA.Mixing of ambient temperature water at 1.5 bar with natural remelted (basaltic) volcanic rock at 1300ºC.This is video material was recorded for one of our explosive...

14. Explosive Magma-Water Interaction: pr06

    out of 5 stars 

    05 Oct 2017 | Contributor(s):: Ingo Sonder

    Date: 2017-09-26Location: University at Buffalo, Geohazards Field Station, Springville/Ashford, NY, USA.Mixing of ambient temperature water at 1.5 bar with natural remelted (basaltic) volcanic rock at 1300ºC.This is video material was recorded for one of our explosive...

15. Chaotic Mixing Device

    out of 5 stars 

    09 May 2014 | Contributor(s):: Daniele Morgavi, Diego Perugini, Cristina P. De Campos, Werner Ertel-Ingrisch, Donald B. Dingwell

    Description of device for chaotic mixing experiments developed at LMU München

16. Phreatic explosion apparatus

    out of 5 stars 

    03 Apr 2014 | Contributor(s):: Betty Scheu, Donald B. Dingwell

    Description of an experimental setup to investigate phreatic eruptions in the laboratory

17. Experimental approach to constrain phreatic eruption processes on White Island, New Zealand (IAVCEI 2013 poster presentation)

    out of 5 stars 

    06 Aug 2013 | Contributor(s):: Klaus Mayer, Betty Scheu, Yan Lavallee, Ben Kennedy, H. Albert Gilg, Michael Heap, Mark Letham, Cristian Montanaro, Laura Jacquemard, Noemie Pernin, Donald D. Dingwell

    White Island is New Zealand's most active volcano and primarily characterised by phreatic and phreatomagmatic eruptions. A phreatic eruption on August 2nd, 2012 ended an eleven year quiescence. More than 100 years ofintense hydrothermal activity from magmatic fluids and groundwater has created a...

18. Between cyclic eruptions (VUELCO meeting, Barcelona, 2013)

    out of 5 stars 

    20 Mar 2013 | Contributor(s):: Fabian Ben Wadsworth

    Volcanic unrest begins with precursory signals which are the detectable manifestation of dynamic subsurface changes. In 1997, Vulcanian eruptions from Soufrière Hills volcano (SHV), Montserrat, had a mean repose time of 9.5 hours and produced remarkably regular precursory signals. Cyclic...

19. Constraining conditions for phreatic eruptions and evaluating the influence of hydrothermal alteration on the process: an experimental approach (Vuelco mini conference Barcelona 2013)

    out of 5 stars 

    20 Mar 2013 | Contributor(s):: Klaus Mayer, Betty Scheu

    Phreatic eruptions are caused by rapid evaporation of hydrothermal fluids to steam with the resulting pore overpressure leading to fragmentation of overlying rocks.We investigate White Island (New Zealand) and the active volcanic sites Solfatara and Monte Nuovo in Campi Flegrei (Italy); further...