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343161

Sigma-Aldrich

Iron(II) sulfide

−100 mesh, 99.9% trace metals basis

Synonyme(s) :

Ferrous sulfide

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About This Item

Formule empirique (notation de Hill):
FeS
Numéro CAS:
Poids moléculaire :
87.91
Numéro CE :
Numéro MDL:
Code UNSPSC :
12352302
eCl@ss :
38190405
ID de substance PubChem :
Nomenclature NACRES :
NA.55

Pureté

99.9% trace metals basis

Forme

powder

Pertinence de la réaction

reagent type: catalyst
core: iron

Taille des particules

−100 mesh

Densité

4.84 g/mL at 25 °C (lit.)

Chaîne SMILES 

S=[Fe]

InChI

1S/Fe.S

Clé InChI

MBMLMWLHJBBADN-UHFFFAOYSA-N

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Application


  • Progress in bioleaching: fundamentals and mechanisms of microbial metal sulfide oxidation - part A: This study delves into the microbial oxidation of metal sulfides like Iron(II) sulfide, shedding light on bioleaching processes crucial for the extraction of valuable metals from ores, which is highly relevant for environmental and materials science applications (Vera et al., 2022).

  • Novel QTL Associated with Aerenchyma-Mediated Radial Oxygen Loss (ROL) in Rice: Explores genetic traits influenced by conditions such as the presence of Iron(II) sulfide in paddy fields, providing insights into how rice adapts to iron-rich anaerobic soils, which is vital for agricultural biotechnology and crop science (Duyen et al., 2022).

  • Fe(ii) and Fe(iii) dithiocarbamate complexes as single source precursors: Investigates the synthesis of nanoscale iron sulfides from these precursors, using in situ X-ray absorption spectroscopy, which is essential for developing advanced materials with specific magnetic and electronic properties (Roffey et al., 2019).

Code de la classe de stockage

11 - Combustible Solids

Classe de danger pour l'eau (WGK)

WGK 3

Point d'éclair (°F)

Not applicable

Point d'éclair (°C)

Not applicable


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Les clients ont également consulté

N Finck et al.
Environmental science & technology, 46(18), 10004-10011 (2012-08-21)
The isotope (79)Se may be of great concern with regard to the safe disposal of nuclear wastes in deep geological repositories due to its long half-life and potential mobility in the geosphere. The Se mobility is controlled by the oxidation
Andrew D Henderson et al.
Water research, 47(3), 1267-1276 (2012-12-19)
Iron sulfide (FeS) has been extensively assessed as a reactive medium to remove both metals and halogenated organics from groundwater. However, to address its suitability as a material for permeable reactive barriers (PRBs), its propensity for solids and gas production
Amit Kumar Dutta et al.
ACS applied materials & interfaces, 4(4), 1919-1927 (2012-03-28)
Nanocrystalline FeS and FeSe compounds were prepared by solvothermal decomposition of a precursor complex [Fe(3)(μ(3)-O)(μ(2)-O(2)CCH(2)Cl)(6)(H(2)O)(3)]NO(3)·H(2)O in the presence of thiourea and sodium selenite, respectively. The as-obtained products were characterized by X-ray diffraction analysis (XRD), field emission scanning electron microscopy (FESEM)
The structural plasticity of the proximal [4Fe3S] cluster is responsible for the O2 tolerance of membrane-bound [NiFe] hydrogenases.
Jean-Marie Mouesca et al.
Angewandte Chemie (International ed. in English), 52(7), 2002-2006 (2013-01-09)
Romain Guilbaud et al.
Science (New York, N.Y.), 332(6037), 1548-1551 (2011-06-28)
The iron isotope composition of sedimentary pyrite has been proposed as a potential proxy to trace microbial metabolism and the redox evolution of the oceans. We demonstrate that Fe isotope fractionation accompanies abiotic pyrite formation in the absence of Fe(II)

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