Preview Paper No 1, Richard Davies:
Preview Paper No, 2:
Preview Paper No 3, Sukendar Asikin:
Preview Paper No 4, Hilarry Hartnett:
Preview Paper No 5 Mark Tingay:
Preview Paper No 6 Awang Harun Satyana:
Preview Paper No 7 Maxwell L. Rudolph:
Preview Paper No 8&9 Sergey Kadurin & Igor Kadurin:
Preview Paper No 10 Agus Guntoro:
Preview Paper No 11 Wataru Tanikawa:
Preview Paper No 13 Sayogi Sudarman:
Preview Paper No 14 Andriano Mazzini:
SIMULATION GIS-3D AS PART OF SERGEY KADURIN AND IGOR KADURIN PRESENTATION
Preview 3d animation:
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Titles and Abstracts of Presentations
Thursday 26 May 2011 – Surabaya
TIME ACTIVITY ABSTRACT
09:15-09:35 Durham University
Presentation by Richard Davies
“LUSI : HOW LONG AND WHAT NEXT”
Richard Davies, Durham University, UK
*Katie Roberts, Durham University, UK
*Simon Mathias, Durham University, UK
Mark Tingay, University of Adelaide, Australia
Richard Swarbrick, Geopressure Technology Ltd., UK
LINK PRESENTATION, PICASSA WEB: https://picasaweb.google.com/hardiprasetyo9/LUSILIBRARYSLIDESPRESENTATIONDAVIES
RIntScienSymposiumFutureLUSI26May2011#
LUSI LIBRARY: SLIDES PRESENTATION, DAVIES. R, Int. Scien. Symposium, Future LUSI, 26 May 2011
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3 Jun 2011
foto: 15 – 1 MB
Umum di web (edit) |
https://lh5.googleusercontent.com/-kSin6ZMJpgk/TehQtmQyFNI/AAAAAAAADSo/OVM9wbpzUcM/s128/Slide1.JPG
Slides Presentation, modified the style from its original, without any change in the subsatntion (keep in original). Prof. Dr. Richard Davies, Durham University, UK, presented at the International Scientific Symposium, On Future LUSI. Was held on 26 May 2011, at the Mercure Hotel, Surabaya, Indonesia. Organized by Humanitus Sidoarjo Fund in cooperatioon/coordination with the BPLS. (The original and Previewed presentation will be completed). Hardi
Outline
1. Introduction to the Geology
2. How long will it last?
3. What next?
Results
Longevity one of the most important results of our research efforts.
But if the dynamics have changed from overpressure driven, to gas slug driven, then the whole basis for estimating both future eruptive activity and eruption longevity has changed. Experience on igneous volcanoes like Stromboli could be used
What next – ideas
Within the next few years Lusi could slow to very low eruption rates (as predicted)
But natural mud volcanoes go through phases of short duration violent eruption (pressure release).
Could Lusi develop clearer phases of activity and dormancy on similar timescales to natural mud volcanoes?
Pressure re-charge?
Dissolved gas may keep very low levels of activity going for several decades
Idea for more joined-up research approach
Set up ‘Lusi research network (LRN) including people researching Lusi (overseas and Indonesian academics) and key stakeholders. Meet once per annum in Surabaya.
1. Discuss ideas and ensure research impact (we’re working on questions with relevance)
2. Discuss sources of new data
3. New research avenues and potential funding streams
4. Requires fund of $25k(?) per annum and some adminstration
09:35-09:55 Arizona State University
Presentation by Loyc Vanderkluysen
“EVOLUTION OF THE LUSI ERUPTION FROM SATELLITE AND GROUND-BASED
REMOTE SENSING”
LUSI operates as an evolving complex system affected by repeated episodes of edifice building, levee collapse, subsidence, blockage of the drainage system and dredging of the Porong river.
We will present thermal remote sensing data from the MODIS and ASTER satellite instruments showing the evolution of the LUSI thermal output over the course of the eruption and outline future work using satellite- and ground-based instruments to monitor LUSI’s evolving morphology and emission of hazardous gases. |
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