Peculiarities of Serpentine Decomposition in the Presence of Alkaline Chloride: Raman Study at High Pressure and Temperature
- 作者: Likhacheva A.Y.1,2, Goryainov S.V.1, Rashchenko S.V.1,2,3, Safonov O.G.4,5
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隶属关系:
- Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
- Budker Institute of Nuclear Physics, Siberian Branch, Russian Academy of Sciences
- Novosibirsk State University
- Institute of Experimental Mineralogy, Russian Academy of Sciences
- Moscow State University
- 期: 卷 83, 编号 6 (2019)
- 页面: 680-682
- 栏目: Article
- URL: https://journals.rcsi.science/1062-8738/article/view/187405
- DOI: https://doi.org/10.3103/S1062873819060200
- ID: 187405
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详细
In situ Raman spectroscopy combined with a resistively heated diamond anvil cell was used to study the behavior of serpentine (chrysotile) Mg3Si2O5(OH)4 in the presence of NaCl at 100–400°С and 10 kbar. Low H2O activity leads to a decrease in the dehydration temperature by about 200°C compared to a salt-free system, as well as the formation of only anhydrous products.
作者简介
A. Likhacheva
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences; Budker Institute of Nuclear Physics, Siberian Branch, Russian Academy of Sciences
编辑信件的主要联系方式.
Email: alih@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090; Novosibirsk, 630090
S. Goryainov
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
Email: alih@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090
S. Rashchenko
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences; Budker Institute of Nuclear Physics, Siberian Branch, Russian Academy of Sciences; Novosibirsk State University
Email: alih@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090; Novosibirsk, 630090; Novosibirsk, 630090
O. Safonov
Institute of Experimental Mineralogy, Russian Academy of Sciences; Moscow State University
Email: alih@igm.nsc.ru
俄罗斯联邦, Chernogolovka, Moscow oblast, 142432; Moscow, 119991
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