Physics
Scientific paper
Dec 2010
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010agufm.p32a..04k&link_type=abstract
American Geophysical Union, Fall Meeting 2010, abstract #P32A-04
Physics
[3902] Mineral Physics / Creep And Deformation, [5120] Physical Properties Of Rocks / Plasticity, Diffusion, And Creep, [5455] Planetary Sciences: Solid Surface Planets / Origin And Evolution, [5460] Planetary Sciences: Solid Surface Planets / Physical Properties Of Materials
Scientific paper
Both orbital and thermal evolution of recently discovered super-Earths (terrestrial planets whit mass exceeding that of Earth) depends critically on the rheological properties of their mantle. Although direct experimental studies on rheological properties are unavailable under the conditions equivalent to the deep mantles of these planets (~1 TPa and ~5000 K), a review of key materials science observations suggests that the deep mantle of these planets have much lower viscosity than most of the shallower regions of these planets. The key observations are: (i) phase transformations likely occur under these conditions including the B1 to B2 transition in MgO (1) and the dissociation of MgSiO3 into two oxides (MgO and SiO2) (2), (ii) the systematics in high-temperature creep show that materials with NaCl (B1) structures have much smaller viscosity than other oxides compared at the same normalized conditions (3), and (iii) diffusion coefficients in most of materials have a minimum at certain pressure and above that pressure it increases with pressure (due to mechanism transition) (4). In addition, a review of existing studies also shows that the ionic solids with B2 (CsCl) structure have larger diffusion coefficients than their B1 counter parts. Furthermore, if metallization transition occurs in any of these materials, delocalized electrons will further weaken the material. All of these observations or concepts suggest that even though the viscosity of a planet (below the asthenosphere) increases with depth in the relatively shallow regions, viscosity likely starts to decrease with depth below some critical depth (>~2000 km). The inferred low viscosity of super-Earths implies a large tidal dissipation and relatively rapid orbital evolution. Also such a rheological properties likely promote a layered mantle convection that enhances a weak deep mantle and retards the thermal evolution. 1. A. R. Oganov, M. J. Gillan, G. D. Price, Journal of Chemical Physics 118, 10174 (2003). 2. K. Umemoto, R. M. Wentzcovitch, P. B. Allen, Science 311, 983 (2006). 3. S. Karato, Physics of Earth and Planetary Interiors 55, 234 (1989). 4. S. Karato, Programme and Abstracts, The Seismological Society of Japan 1, 216 (1978).
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