Remote Compositional Analysis Techniques for Understanding Spectroscopy, Mineralogy, and Geochemistry of Planetary Surfaces
Book contents
- Remote Compositional Analysis
- Cambridge Planetary Science
- Remote Compositional Analysis
- Copyright page
- Contents
- Contributors
- Foreword
- Preface
- Acknowledgments
- Part I Theory of Remote Compositional Analysis Techniques and Laboratory Measurements
- 1 Electronic Spectra of Minerals in the Visible and Near-Infrared Regions
- 2 Theory of Reflectance and Emittance Spectroscopy of Geologic Materials in the Visible and Infrared Regions
- 3 Mid-infrared (Thermal) Emission and Reflectance Spectroscopy
- 4 Visible and Near-Infrared Reflectance Spectroscopy
- 5 Spectroscopy of Ices, Volatiles, and Organics in the Visible and Infrared Regions
- 6 Raman Spectroscopy
- 7 Mössbauer Spectroscopy
- 8 Laser-Induced Breakdown Spectroscopy
- 9 Neutron, Gamma-Ray, and X-Ray Spectroscopy
- 10 Radar Remote Sensing
- Part II Terrestrial Field and Airborne Applications
- Part III Analysis Methods
- Part IV Applications to Planetary Surfaces
- Index
- References
7 - Mössbauer Spectroscopy
Theory and Laboratory Spectra of Geologic Materials
from Part I - Theory of Remote Compositional Analysis Techniques and Laboratory Measurements
Published online by Cambridge University Press: 15 November 2019
Book contents
- Remote Compositional Analysis
- Cambridge Planetary Science
- Remote Compositional Analysis
- Copyright page
- Contents
- Contributors
- Foreword
- Preface
- Acknowledgments
- Part I Theory of Remote Compositional Analysis Techniques and Laboratory Measurements
- 1 Electronic Spectra of Minerals in the Visible and Near-Infrared Regions
- 2 Theory of Reflectance and Emittance Spectroscopy of Geologic Materials in the Visible and Infrared Regions
- 3 Mid-infrared (Thermal) Emission and Reflectance Spectroscopy
- 4 Visible and Near-Infrared Reflectance Spectroscopy
- 5 Spectroscopy of Ices, Volatiles, and Organics in the Visible and Infrared Regions
- 6 Raman Spectroscopy
- 7 Mössbauer Spectroscopy
- 8 Laser-Induced Breakdown Spectroscopy
- 9 Neutron, Gamma-Ray, and X-Ray Spectroscopy
- 10 Radar Remote Sensing
- Part II Terrestrial Field and Airborne Applications
- Part III Analysis Methods
- Part IV Applications to Planetary Surfaces
- Index
- References
Summary
The technique of Mössbauer spectroscopy is the gold standard for measurements of the redox state, coordination environment, and site occupancy of iron in geologic materials. Laboratory measurements typically involve measurements on 5–300 mg of powdered material. Mössbauer is also used to identify mineralogy of iron oxide phases and in some cases to constrain the distribution of Fe among mixed silicate phases in a rock. Together, these uses fill a need in the terrestrial and extraterrestrial communities for understanding Fe redox states, and by inference, oxygen fugacity, as oxygen evolves on planetary bodies. This chapter provides a background for understanding the Mössbauer effect and interpretation of its hyperfine parameters.
- Type
- Chapter
- Information
- Remote Compositional AnalysisTechniques for Understanding Spectroscopy, Mineralogy, and Geochemistry of Planetary Surfaces, pp. 147 - 167Publisher: Cambridge University PressPrint publication year: 2019
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