Dag Kristian Dysthe

Prof. Dag Kristian Dysthe


Research Focus & Metrics

Academic Career Length

32Years (1995-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 January 2013
Verified
Book Chapter
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JGJean-Pierre Gratier
Jean-Pierre Gratier
DDDag Kristian Dysthe
Dag Kristian Dysthe
FRFrancois Renard
Francois Renard

9 April 2011 in Journal of Geophysical Research
Verified
Journal Article
Closed access
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ARAnja Røyne
Anja Røyne
JBJan Bisschop
Jan Bisschop
DDDag Kristian Dysthe
Dag Kristian Dysthe

1 April 2001 in Geophysical Research Letters
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Journal Article
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FRFrancois Renard
Francois Renard
DDDag Kristian Dysthe
Dag Kristian Dysthe
JFJens Feder
Jens Feder
KBKnut Bjørlykke
Knut Bjørlykke
BJBjørn Jamtveit
Bjørn Jamtveit

7 December 2011 in Journal of Geophysical Research: Solid Earth
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Journal Article
Open access
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MKMaya Kobchenko
Maya Kobchenko
HPHamed Panahi
Hamed Panahi
FRFrancois Renard
Francois Renard
DDDag Kristian Dysthe
Dag Kristian Dysthe
AMAnders Malthe-Sørenssen
Anders Malthe-Sørenssen
PMPaul Meakin
Paul Meakin
9p.International audienceTo better understand the mechanisms of fracture pattern development and fluid escape in low permeability rocks, we performed time-resolved in situ X-ray tomography imaging to investigate the processes that occur during the slow heating (from 60° to 400°C) of organic-rich Green River shale. At about 350°C cracks nucleated in the sample, and as the temperature continued to increase, these cracks propagated parallel to shale bedding and coalesced, thus cutting across the sample. Thermogravimetry and gas chromatography revealed that the fracturing occurring at ∼350°C was associated with significant mass loss and release of light hydrocarbons generated by the decomposition of immature organic matter. Kerogen decomposition is thought to cause an internal pressure build up sufficient to form cracks in the shale, thus providing pathways for the outgoing hydrocarbons. We show that a 2D numerical model based on this idea qualitatively reproduces the experimentally observed dynamics of crack nucleation, growth and coalescence, as well as the irregular outlines of the cracks. Our results provide a new description of fracture pattern formation in low permeability shales

2 October 2018 in Pure and Applied Geophysics
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Journal Article
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FRFrancois Renard
Francois Renard
JMJessica McBeck
Jessica McBeck
BCBenoît Cordonnier
Benoît Cordonnier
XZXiaojiao Zheng
Xiaojiao Zheng
NKNeelima Kandula
Neelima Kandula
DDDag Kristian Dysthe
Dag Kristian Dysthe

26 November 2013 in Physical Review Letters
Verified
Journal Article
Closed access
AFAlexander Farutin
Alexander Farutin
SRSalima Rafaï
Salima Rafaï
DDDag Kristian Dysthe
Dag Kristian Dysthe
ADAlain Duperray
Alain Duperray
PPPhilippe Peyla
Philippe Peyla
CMChaouqi Misbah
Chaouqi Misbah
Microorganisms, such as bacteria, algae, or spermatozoa, are able to propel themselves forward thanks to flagella or cilia activity. By contrast, other organisms employ pronounced changes of the membrane shape to achieve propulsion, a prototypical example being the Eutreptiella gymnastica. Cells of the immune system as well as dictyostelium amoebas, traditionally believed to crawl on a substratum, can also swim in a similar way. We develop a model for these organisms: the swimmer is mimicked by a closed incompressible membrane with force density distribution (with zero total force and torque). It is shown that fast propulsion can be achieved with adequate shape adaptations. This swimming is found to consist of an entangled pusher-puller state. The autopropulsion distance over one cycle is a universal linear function of a simple geometrical dimensionless quantity $A/{V}^{2/3}$ ($V$ and $A$ are the cell volume and its membrane area). This study captures the peculiar motion of Eutreptiella gymnastica with simple force distribution.