The Oxidation-Reduction Potential in Geology
Autor M. F. Stashchuken Limba Engleză Paperback – 26 apr 2012
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Specificații
ISBN-13: 9781468415957
ISBN-10: 1468415956
Pagini: 136
Ilustrații: X, 122 p.
Dimensiuni: 210 x 279 x 7 mm
Greutate: 0.32 kg
Ediția:1972
Editura: Springer Us
Colecția Springer
Locul publicării:New York, NY, United States
ISBN-10: 1468415956
Pagini: 136
Ilustrații: X, 122 p.
Dimensiuni: 210 x 279 x 7 mm
Greutate: 0.32 kg
Ediția:1972
Editura: Springer Us
Colecția Springer
Locul publicării:New York, NY, United States
Public țintă
ResearchCuprins
1 The Principal Methods of Determining Oxidation — Reduction Conditions.- The Fe../Fe… Ratio and Eh.- The Forms of Sulfur as Indicators of Oxidation — Reduction Conditions.- The Relationship of Organic Matter in Sediments and the Oxidation — Reduction Potential.- Iron-Mineral Indicators of Oxidation — Reduction Conditions.- Garrels’ Thermodynamic Diagrams.- Other Methods of Determining Oxidation-Reduction Conditions.- 2 Thermodynamic Principles for Investigating the Conditions of Mineral Formation.- The Solubility of Compounds and the Maximum Work of a Reaction.- The Concept of the Oxidation-Reduction Potential.- Analysis of Some Errors.- 3 Stability Diagrams of Iron Minerals.- Stability Boundary of the Natural Environment.- 4 Conditions for Formation of Iron Minerals during Sedimentation and Diagenesis.- Change of pH during the Diagenesis of Sediments.- Change of Oxidation — Reduction Potential during Diagenesis of Sediments.- The Distribution of Hydrogen Sulfide.- Analysis of Mineral Formation.- Indicators of Oxidation — Reduction Conditions under Which Sedimentary Rocks Form.- Conclusions.- Literature Cited.