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COMPRES 2006 Snowbird, Utah

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COMPRES 2006 Snowbird, Utah. David Walker, Lamont ... Peritectic. possible. to recognize. when reactants. are spatially. resolved. Fe. FeO. Does this work? ... – PowerPoint PPT presentation

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Title: COMPRES 2006 Snowbird, Utah


1
COMPRES 2006 Snowbird, Utah David Walker,
Lamont-Doherty Earth Observatory, Columbia U.
Why ever would the Earths core leak?
(NSF CSEDI2 progress report)
2
Some plume basalts show correlated Os anomalies.
Core- flavored plume
Liquid metal outer core
Inner core
solid mantle
190Pt-driven
atmosphere
187Re-driven
Maybe Re?
A.Brandon, R.J.Walker et al. (2003)
3
Is the core really leaking?
What could drive it?
Manghnani and Yagi
Yes, perhaps Os isotopes
Hawaiian plume Fe/Mn Ni
Perhaps not radiogenic Sr/Os correlation
4
Cooling drives changes in solubility
Reorient for buoyant slag floating on the core
5
What determines oxygen solubility(P)?
6
But we still need to measure Oxygen solubility
in Fe liquid at high P,T
Does it reach 2 or 20?
Manghnani and Yagi
(A year in the lab can save you an hour in the
library!)
7
How to measure Oxygen solubility in molten Fe
at a megabar?
Underway with COMPRES support for the ALS 12.2.2
team
8
http//xraysweb.lbl.gov/bl1222/home.htm
9
LBL ALS Station 12.2.2
10
Laser
LBL ALS Station 12.2.2
11
In situ DAC X-Radiographic Imaging (XRI)
12
Absorption(?) /or emission
13
Peritectic possible to recognize when
reactants are spatially resolved.
14
50 kilobars
Fe
Does this work?
FeS
Station 12.2.2 ALS
15
It seems to work!
Topography convolved with chemistry -and- resolut
ion limited by phosphor sharpness and sample
preparation
What about Fe-FeO?
16
550 kilobars
FeO
Fe
Consistent with the DAC results of Takafuji et
al. (2005) lt6
17
(No Transcript)
18
Oxygen solubility does not appear to be high
enough to be interesting.
Are there other solutions to the problem?
19
Glatzmaier Roberts 1995
Earths dynamo magnetic field
20
Toroidal magnetic field in the outer core
generates local anodic and cathodic areas at the
CMB 1 V Could this drive any
electrochemical transfers across the CMB?
mantle
low Fe
core
(See Abby Kavners forthcoming paper in EPSL)
21
What does the presence of life do for us?
Core signal generated by recycled oxidized crust.
22
Iron meets oxygen!
rusty surface
Bright inner core
When oxygen does not dissolve in iron.
23
N2 O2
Most effective and quick if oxygen solubility low
Core- flavored plume
Oxidized slab
Os-Sr-Nd-O signal of recycled crust not a show
stopper. It is the key to the delivery mechanism
for the corrosive reaction.
Liquid metal outer core
Inner core
solid mantle
Revenge of the plants!
24
Remaining questions
Does the biosphere-core feedback deserve to be
taken seriously?
Test when does the Os signal start? gt2.8 Gy ago
(Puchtel et al.)
Why not electrochemistry?
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