Physics
Scientific paper
May 2004
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004agusm.u53a..03s&link_type=abstract
American Geophysical Union, Spring Meeting 2004, abstract #U53A-03
Physics
3900 Mineral Physics, 3909 Elasticity And Anelasticity, 3924 High-Pressure Behavior, 5430 Interiors (8147), 8147 Planetary Interiors (5430, 5724)
Scientific paper
The oceans cover more that 7 percent of the surface area but compose only 0.025 percent of the mass of the Earth. The nominally anhydrous silicate phases thought to compose the upper 660 km of Earth can incorporate more than ten times this much H. Hydrogen is thus a very poorly constrained compositional variable in the Earth. In order to evaluate the possibility of there being a very large reservoir of H in the interior we have conducted experiments to measure the effect of H incorporation on the physical properties of these minerals. At depths less than 410 km, olivine can incorporate 2000 ppm, and possibly as much as 8000 ppm, H2O by weight at pressures above 10 GPa. Clinopyroxene can incorporate a similar amount of H as hydroxyl, and petrologic evidence in natural high-pressure samples suggests it may incorporate 5000 ppm or more. In the subducting basaltic slab after all hydrous phases break down, the pyroxene can carry down 0.1 to 0.2 percent H2O by weight of the slab. If the ultramafic portion below the crustal portion becomes hydrated, the olivine can carry as much or more water into the interior. Based on neutron and X-ray diffraction studies, H is incorporated in these mineral principally by the 2H for Mg mechanism, meaning that H become a much more compatible element at pressures above 10 GPa. Using single crystal X-ray diffraction, we have measured the effect of hydration on compression of ringwoodite to 12 GPa. Using powder diffraction and synchrotron radiation we have measured compression to 50 GPa. Using GHz ultrasonic measurements of P and S-wave travel times, we observe a reduction of P-wave velocity equivalent to an increase in temperature of 600° C and on S-wave velocity of 1000° C. Throughout most of the Transition Zone (TZ), hydration has a larger effect on velocity than does temperature within reasonable ranges of these parameters and a much larger effect than do other compositional variables such as Mg/Fe ratios. In tomographic images of the TZ in regions distant from active subduction, red is more likely to mean `wet' than it is to mean `hot'. Observed seismic velocities in the TZ are consistent with a pyrolite composition with 0.5 to 1.0 percent by weight H2O, but not consistent with dry pyrolite compositions. This would allow for Transition Zone storage of two to three times the amount of water currently in the hydrosphere.
Amulele G.
Frost Dan J.
Holl Christopher M.
Jacobsen Steven D.
Manghnani Murli H.
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