(Q56692120)

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Reaction pathways in the Fe–S system below 100°C

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Reaction pathways in the Fe–S system below 100°C (English)

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Liane G Benning

1

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author name string

Rick T Wilkin

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2

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H.L Barnes

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3

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publication date

June 2000

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published in

Chemical Geology

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volume

167

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issue

1-2

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page(s)

25-51

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cites work

In situ time-resolved X-ray diffraction of iron sulfides during hydrothermal pyrite growth

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7 January 2021

The use of chromium reduction in the analysis of reduced inorganic sulfur in sediments and shales

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Isotope fractionation and sulfur metabolism by pure and enrichment cultures of elemental sulfur-disproportionating bacteria

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Formation of Polysulfides in Aqueous Solution

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Pyrite formation linked with hydrogen evolution under anaerobic conditions

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Pyrite synthesis via polysulfide compounds

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Determination of Metal (Bi)Sulfide Stability Constants of Mn2+, Fe2+, Co2+, Ni2+, Cu2+, and Zn2+by Voltammetric Methods

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Marcasite precipitation from hydrothermal solutions

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Kinetics of pyrite formation by the H2S oxidation of iron (II) monosulfide in aqueous solutions between 25 and 125°C: The rate equation

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Kinetics of pyrite formation by the H2S oxidation of iron (II) monosulfide in aqueous solutions between 25 and 125°C: The mechanism

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Reactions of iron monosulfide solids with aqueous hydrogen sulfide up to 160°C

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Transformation of mackinawite to greigite; an in situ X-ray powder diffraction and transmission electron microscope study

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Identifiers

DOI

10.1016/S0009-2541(99)00198-9

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ADS bibcode

2000ChGeo.167...25B

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(Q56692120)

Reaction pathways in the Fe–S system below 100°C

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