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Published byBennett Nicholson Modified over 9 years ago
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“Snowfall” in Earth’s core and the nature of the inner-core boundary Jeffrey Pigott – Mineral Physics (Ohio State) Jackie Li – Mineral Physics (U of Michigan) Bin Chen – Mineral Physics ( U of Michigan) Matt Armentrout – Mineral Physics (UCLA) Antonio Buono – Mineral Physics (MIT) John Hernlund – Geodynamics (UC-Berkeley) Jodi Gaeman – Geodynamics (U of Maryland) Lauren Waszek – Seismology (Cambridge)
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CIDER 2010 - KITP Outer Core Inner Core F-layer PREM AK135 PREM2 Zou et al., 2008 (JGR) Chen et al., 2008 (GRL) Hauck et al., 2006 (JGR)
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Nov 2010 Equations of state, melting curves, compositional gradients Project still broadly defined in terms of interdisciplinary aspect MP meeting (Ann Arbor)/2010 Fall AGU
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MP meeting (Ann Arbor, Nov 2011) Parameter space for “snowing” using seismic, experimental, and theoretical constraints Snowing – Fe-S, Fe-C?, Fe-Si? No snow – Pure Fe, Fe- H, likely Fe-C and Fe-Si Relationship between melting curve and adiabat Can solid/liquid fraction account for Vp gradient? Top of F-layer
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Geodynamics Evolution of thermal, compositonal, and structural profiles with time Stability of F-layer Origin of stratified layer
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Comments and Suggestions Defined leadership role Positives Easy exchange among different disciplines at CIDER Helpful interaction within MP sub-group Collaboration that otherwise would not have occurred Negatives Difficulty following up with interdisciplinary communication Short (~3-5 day) semi-annual workshops for established groups Difficulty generating a concrete product Viewed as a “side-project”
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