
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
9 - Neutron, Gamma-Ray, and X-Ray Spectroscopy
Theory and Applications
from Part I - Theory of Remote Compositional Analysis Techniques and Laboratory Measurements
Published online by Cambridge University Press: 15 November 2019
- 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
Neutrons, gamma rays, and X-rays are used to measure the subsurface elemental composition of Solar System bodies, providing insights into their formation and evolution. Neutrons and gamma rays are highly penetrating particles made by the steady bombardment of the regolith of airless bodies by galactic cosmic rays. Gamma rays are also made by the decay of natural radioelements. The escaping radiation can be detected in close-proximity orbits and analyzed to determine subsurface elemental composition to depths of a few decimeters. Because the radiation sensors have nearly omnidirectional response, spatial resolution depends on orbital altitude. X-ray fluorescence is induced by solar X-rays. Consequently, X-ray spectroscopy is most useful for studies of objects in the inner Solar System. Characteristic elemental X-rays are made within the uppermost ~100 micrometers of the surface. The suite of elements analyzed overlaps that of nuclear spectroscopy, providing complementary geochemical information. Because X-rays are easily collimated, relatively high spatial resolution measurements are possible. This chapter presents the fundamentals of neutron, gamma-ray, and X-ray production, transport, and detection along with an overview of the measurement principles, including modeling, analysis, and mapping methods.
Keywords
- Type
- Chapter
- Information
- Remote Compositional AnalysisTechniques for Understanding Spectroscopy, Mineralogy, and Geochemistry of Planetary Surfaces, pp. 191 - 238Publisher: Cambridge University PressPrint publication year: 2019
References
- 1
- Cited by