Hydrogen grain boundary diffusion in olivine and its contribution to conductivity anomaly
| Project/Area Number |
17J11576
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| Research Category |
Grant-in-Aid for JSPS Fellows
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| Allocation Type | Single-year Grants |
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| Section | 国内 |
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| Research Field |
Petrology/Mineralogy/Economic geology
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| Research Institution | Okayama University |
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Principal Investigator |
Zhao Chengcheng 岡山大学, 自然科学研究科, 特別研究員(DC2)
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| Project Period (FY) |
2017-04-26 – 2019-03-31
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| Project Status |
Completed (Fiscal Year 2018)
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| Budget Amount *help |
¥1,900,000 (Direct Cost: ¥1,900,000)
Fiscal Year 2018: ¥900,000 (Direct Cost: ¥900,000)
Fiscal Year 2017: ¥1,000,000 (Direct Cost: ¥1,000,000)
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| Keywords | Olivine / Redox kinetics / Diffusion / Subducted slab / hydrous forsterite / hydrous olivine / synthesis methods / quality of sintering |
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| Outline of Annual Research Achievements |
Olivine (MgO, SiO2 and Fe2O3 oxide mixture) with 5 wt% Pt powder used as oxygen sensor was synthesized using gas mixture furnace at iron-wustite (IW) buffer and Ni-NiO (NNO) buffered condition at 1300 oC. Diffusion couple method is adopted to investigate the redox kinetics of olivine. Diffusion experiments were conducted for different durations at 1 GPa, 1100-1300 oC using piston cylinder apparatus. After recovery, oxygen fugacity profiles were calculated following the method described by Faul et al. (2019). Diffusion coefficients were obtained using Boltzmann-Matano method. Water content after diffusion was measured using FTIR.
Except one couple, the water content of all the other couples shows < 10 wt. ppm. Redox process in olivine could be viewed as a diffusion-controlled process. Diffusion coefficient in oxidized olivine shows obvious oxygen fugacity dependence, while that in reduced one shows small dependence. The activation enthalpy is calculated to be 235 kJ/mol, which is comparable with that for Fe-Mg diffusion in olivine. However, the magnitude is 2-4 orders higher. Since the activation enthalpy and magnitude are comparable with that of diffusion of hydrous defects related to Mg-vacancies, it is possible that even extremely small amount of water could dominate redox kinetics in olivine. The diffusion length calculated indicate that the influence exerted by slab on the reduced mantle is very limited. Therefore, it is possible that once subducted more, the oxidized slab can bring redox budget to deep mantle as it keeps dry condition.
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| Research Progress Status |
平成30年度が最終年度であるため、記入しない。
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| Strategy for Future Research Activity |
平成30年度が最終年度であるため、記入しない。
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Report
(2 results)
Research Products
(6 results)
