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20151202225614.7 |
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160906e19860101||| o| f1|||||eng|d |
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|a (TOE)ost5685234
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|a (TOE)5685234
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|a TOE
|c TOE
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|a GDWR
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|a 58
|2 edbsc
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|a 12
|2 edbsc
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|a E 1.99: conf-860858-1
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|a E 1.99:la-ur-86-1330
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|a E 1.99: conf-860858-1
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|a conf-860858-1
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|a la-ur-86-1330
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|a Fe-O-S redox reactions and kinetics in hydrothermal systems
|h [electronic resource]
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260 |
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|a Oak Ridge, Tenn. :
|b distributed by the Office of Scientific and Technical Information, U.S. Department of Energy,
|c 1986.
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300 |
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|a Pages: 5 :
|b digital, PDF file.
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336 |
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|a text
|b txt
|2 rdacontent.
|
337 |
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|a computer
|b c
|2 rdamedia.
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338 |
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|a online resource
|b cr
|2 rdacarrier.
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|a Published through SciTech Connect.
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|a 01/01/1986.
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|a "la-ur-86-1330"
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|a " conf-860858-1"
|
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|a "DE86010187"
|
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|a 5. international meeting on water-rock interaction, Reykjavik, Iceland, 8 Aug 1986.
|
500 |
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|a Seyfried, W.E. Jr.; Janecky, D.R.; Berndt, M.E.
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500 |
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|a Minnesota Univ., Minneapolis (USA)
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520 |
3 |
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|a Oxidation-reduction reactions are important in many hydrothermal systems, predominantly involving the elements O, H, C, S, and Fe, but also significantly affecting a wide variety of minor and trace components. Fe-bearing silicate, oxide, and sulfide minerals are commonly used in hydrothermal experiments and petrographic studies to define the redox state of a system. We have experimentally investigated reactions of magnetite, hematite, pyrite, and pyrrhotite with 0.5 molal NaCl solutions, at temperatures of 300 to 425/sup 0/C and pressures of 400 to 500 bars, using flexible cell hydrothermal equipment (Seyfried et al., 1986). These experiments allow reversible steady-state solution compositions and the rates of equilibration of various redox couples (including H/sub 2/-H/sub 2/O, H/sub 2/S-SO/sub 4/, and CO/sub 2/-CH/sub 4/) to be determined. 18 refs., 2 figs.
|
536 |
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|b W-7405-ENG-36.
|
650 |
|
7 |
|a Hematite.
|2 local.
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650 |
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7 |
|a Redox Reactions.
|2 local.
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650 |
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7 |
|a Magnetite.
|2 local.
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650 |
|
7 |
|a Pyrite.
|2 local.
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650 |
|
7 |
|a Pyrrhotite.
|2 local.
|
650 |
|
7 |
|a Sodium Chlorides.
|2 local.
|
650 |
|
7 |
|a Basalt.
|2 local.
|
650 |
|
7 |
|a High Pressure.
|2 local.
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650 |
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7 |
|a High Temperature.
|2 local.
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7 |
|a Alkali Metal Compounds.
|2 local.
|
650 |
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7 |
|a Chalcogenides.
|2 local.
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650 |
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7 |
|a Chemical Reactions.
|2 local.
|
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|
7 |
|a Chlorides.
|2 local.
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650 |
|
7 |
|a Chlorine Compounds.
|2 local.
|
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|
7 |
|a Halides.
|2 local.
|
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|
7 |
|a Halogen Compounds.
|2 local.
|
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7 |
|a Igneous Rocks.
|2 local.
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|
7 |
|a Iron Compounds.
|2 local.
|
650 |
|
7 |
|a Iron Ores.
|2 local.
|
650 |
|
7 |
|a Iron Oxides.
|2 local.
|
650 |
|
7 |
|a Iron Sulfides.
|2 local.
|
650 |
|
7 |
|a Minerals.
|2 local.
|
650 |
|
7 |
|a Ores.
|2 local.
|
650 |
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7 |
|a Oxide Minerals.
|2 local.
|
650 |
|
7 |
|a Oxides.
|2 local.
|
650 |
|
7 |
|a Oxygen Compounds.
|2 local.
|
650 |
|
7 |
|a Rocks.
|2 local.
|
650 |
|
7 |
|a Sodium Compounds.
|2 local.
|
650 |
|
7 |
|a Sulfide Minerals.
|2 local.
|
650 |
|
7 |
|a Sulfides.
|2 local.
|
650 |
|
7 |
|a Sulfur Compounds.
|2 local.
|
650 |
|
7 |
|a Transition Element Compounds.
|2 local.
|
650 |
|
7 |
|a Volcanic Rocks.
|2 local.
|
650 |
|
7 |
|a Geosciences.
|2 edbsc.
|
650 |
|
7 |
|a Management Of Radioactive And Non-Radioactive Wastes From Nuclear Facilities.
|2 edbsc.
|
710 |
2 |
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|a Los Alamos National Laboratory.
|4 res.
|
710 |
1 |
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|a United States.
|b Department of Energy.
|b Office of Scientific and Technical Information.
|4 dst.
|
856 |
4 |
0 |
|u http://www.osti.gov/scitech/biblio/5685234
|z Online Access
|
907 |
|
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|a .b60114885
|b 03-06-23
|c 05-30-10
|
998 |
|
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|a web
|b 09-09-16
|c f
|d m
|e p
|f eng
|g
|h 0
|i 3
|
956 |
|
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|a Information bridge
|
999 |
f |
f |
|i ba9b5d99-2247-590b-bc7f-b13ece2e8a17
|s 392cc07a-1c22-5f16-bee1-55f22e29e97c
|
952 |
f |
f |
|p Can circulate
|a University of Colorado Boulder
|b Online
|c Online
|d Online
|e E 1.99: conf-860858-1
|h Superintendent of Documents classification
|i web
|n 1
|