778117
二硫化铁
powder, −325 mesh, 99.8% trace metals basis
别名:
二硫化亚铁
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关于此项目
经验公式（希尔记法）:
FeS2
化学文摘社编号:
分子量:
119.98
MDL number:
UNSPSC Code:
12352300
EC Number:
235-106-8
NACRES:
NA.23
SMILES string
[Fe]1SS1
InChI key
NIFIFKQPDTWWGU-UHFFFAOYSA-N
InChI
1S/Fe.S2/c;1-2/q+2;-2
assay
99.8% trace metals basis
form
powder
reaction suitability
reagent type: catalyst
core: iron
particle size
−325 mesh
mp
450 °C (lit.)
application(s)
battery manufacturing
Quality Level
Application
二硫化铁作为光伏材料 (1) 和锂离子电池正极材料 (2) 引起了人们的极大兴趣。还研究了二硫化铁作为环境污染物封存的潜在材料 (3)。
存储类别
11 - Combustible Solids
wgk
WGK 3
flash_point_f
Not applicable
flash_point_c
Not applicable
Xiaofen Wu et al.
FEMS microbiology ecology, 84(3), 555-563 (2013-02-02)
Soils containing an approximately equal mixture of metastable iron sulfides and pyrite occur in the boreal Ostrobothnian coastal region of Finland, termed 'potential acid sulfate soil materials'. If the iron sulfides are exposed to air, oxidation reactions result in acid
Jiri Kucera et al.
Antonie van Leeuwenhoek, 103(4), 905-919 (2013-01-08)
In contrast to iron-oxidizing Acidithiobacillus ferrooxidans, A. ferrooxidans from a stationary phase elemental sulfur-oxidizing culture exhibited a lag phase in pyrite oxidation, which is similar to its behaviour during ferrous iron oxidation. The ability of elemental sulfur-oxidizing A. ferrooxidans to
M Oggerin et al.
Environmental microbiology, 15(8), 2228-2237 (2013-02-22)
Río Tinto (Huelva, southwestern Spain) is an extreme environment with a remarkably constant acidic pH and a high concentration of heavy metals, conditions generated by the metabolic activity of chemolithotrophic microorganisms thriving in the rich complex sulfides of the Iberian
Zenghui Diao et al.
Water research, 47(13), 4391-4402 (2013-06-15)
Acid mine drainage (AMD) resulting from the oxidation of pyrite and other metal sulfides has caused significant environmental problems, including acidification of rivers and streams as well as leaching of toxic metals. With the goal of controlling AMD at the
James Farquhar et al.
Proceedings of the National Academy of Sciences of the United States of America, 110(44), 17638-17643 (2013-02-15)
It is generally thought that the sulfate reduction metabolism is ancient and would have been established well before the Neoarchean. It is puzzling, therefore, that the sulfur isotope record of the Neoarchean is characterized by a signal of atmospheric mass-independent
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