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pro vyhledávání: '"Breithaupt, Thomas"'
To examine the microstructural evolution that occurs during transient creep, we deformed olivine aggregates to different strains that spanned the initial transient deformation. Two sets of samples with different initial grain sizes of 5 $\mu$m and 20
Externí odkaz:
http://arxiv.org/abs/2407.04982
The flow of Earth's upper mantle has long been considered to occur by slow and near-continuous creep. Such behaviour is observed in classical high-temperature deformation experiments and is a fundamental component of geodynamic models. However, the l
Externí odkaz:
http://arxiv.org/abs/2406.10092
The rheological behaviour of olivine deforming by dislocation creep controls geodynamic processes that involve steady-state flow or transient viscosity evolution. Longstanding rheological models applied to both contexts assume that dislocation creep
Externí odkaz:
http://arxiv.org/abs/2406.10076
The size distribution of grains is a fundamental characteristic of polycrystalline solids. In the absence of deformation, the grain-size distribution is controlled by normal grain growth. The canonical model of normal grain growth, developed by Hille
Externí odkaz:
http://arxiv.org/abs/2102.01798
Akademický článek
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Publikováno v:
Journal of the Royal Society Interface 17, 20200559 (2020)
Shewanella oneidensis MR-1 are facultative aerobic electroactive bacteria, with an appealing potential for sustainable energy production and bioremediation. They gather around air sources, forming aerotactic bands and biofilms. Though accumulation is
Externí odkaz:
http://arxiv.org/abs/1910.10705
Autor:
Wallis, David, Hansen, Lars. N., Kumamoto, Kathryn M., Thom, Christopher A., Plümper, Oliver, Ohl, Markus, Durham, William B., Goldsby, David L., Armstrong, David E. J., Meyers, Cameron D., Goddard, Rellie, Warren, Jessica M., Breithaupt, Thomas, Drury, Martyn R., Wilkinson, Angus J.
The strength of the lithosphere is typically modelled based on constitutive equations for steady-state flow. However, models of lithospheric flexure reveal differences in lithospheric strength that are difficult to reconcile based on such flow laws.
Externí odkaz:
http://arxiv.org/abs/1909.08427
Akademický článek
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Publikováno v:
Proceedings of the National Academy of Sciences of the United States of America, 2001 Jun . 98(13), 7371-7374.
Externí odkaz:
https://www.jstor.org/stable/3055995
Autor:
Breithaupt, Thomas
Publikováno v:
Biological Bulletin, 2001 Apr 01. 200(2), 150-154.
Externí odkaz:
https://www.jstor.org/stable/1543308