Characterization of Potential Micrometeorites by Synchrotron Analysis

Micrometeorites (MMs) are small particles that account for most of the extraterrestrial material deposited on Earth. Synchrotron X-ray fluorescence and diffraction allowed for chemical and mineral characterization to distinguish MM from atmospheric particulate. The relative components of iron, nicke...

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Main Authors: Madison Esposito, Kevin Souhrada, Erin Garland, Mary Kroll, Robert Bolen, Victoria Hernandez, Janet Kaczmarek, David Meisel, Anya Swiss, Paul Northrup, Vivian Stojanoff, Juergen Thieme, Aleida Perez
Format: Article
Language:English
Published: MDPI AG 2020-07-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/10/7/275
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spelling doaj-1c9d13fcb7984cec8a166ae1aeaae8e02020-11-25T03:01:34ZengMDPI AGGeosciences2076-32632020-07-011027527510.3390/geosciences10070275Characterization of Potential Micrometeorites by Synchrotron AnalysisMadison Esposito0Kevin Souhrada1Erin Garland2Mary Kroll3Robert Bolen4Victoria Hernandez5Janet Kaczmarek6David Meisel7Anya Swiss8Paul Northrup9Vivian Stojanoff10Juergen Thieme11Aleida Perez12Science Department, West Islip High School, West Islip, NY 11795, USAScience Department, Bay Shore High School, Bay Shore, NY 11706, USAScience Department, Bay Shore High School, Bay Shore, NY 11706, USAScience Department, West Islip High School, West Islip, NY 11795, USAScience Department, Eastport South Manor High School, Manorville, NY 11949, USAScience Department, William Floyd High School, Mastic Beach, NY 11951, USAScience Department, Sayville High School, Sayville, NY 11782, USADepartment of Physics and Astronomy, Geneseo University, Geneseo, NY 14454, USAScience Department, William Floyd High School, Mastic Beach, NY 11951, USADepartment of Geosciences, Stony Brook University, Stony Brook, NY 11794, USABrookhaven National Laboratory, Upton, NY 11973, USABrookhaven National Laboratory, Upton, NY 11973, USABrookhaven National Laboratory, Upton, NY 11973, USAMicrometeorites (MMs) are small particles that account for most of the extraterrestrial material deposited on Earth. Synchrotron X-ray fluorescence and diffraction allowed for chemical and mineral characterization to distinguish MM from atmospheric particulate. The relative components of iron, nickel, and other elements were considered in the identification of ferrous MM while high amounts of titanium were considered an indication that the particles were of atmospheric origin. Out of 100 samples collected by high school students and teachers, eight were taken to a synchrotron for analysis. Of those eight, three exhibited extraterrestrial compositions. X-ray absorption near-edge structure analysis revealed that the same three samples contained sulfide, the main sulfur form constituent in MM. X-ray microdiffraction analysis showed the presence of the minerals pentlandite and forsterite. Collectively, these results support the extraterrestrial nature of the three particles.https://www.mdpi.com/2076-3263/10/7/275micrometeoritesmeteoritessynchrotronX-ray fluorescenceX-ray absorption spectroscopyX-ray diffraction
collection DOAJ
language English
format Article
sources DOAJ
author Madison Esposito
Kevin Souhrada
Erin Garland
Mary Kroll
Robert Bolen
Victoria Hernandez
Janet Kaczmarek
David Meisel
Anya Swiss
Paul Northrup
Vivian Stojanoff
Juergen Thieme
Aleida Perez
spellingShingle Madison Esposito
Kevin Souhrada
Erin Garland
Mary Kroll
Robert Bolen
Victoria Hernandez
Janet Kaczmarek
David Meisel
Anya Swiss
Paul Northrup
Vivian Stojanoff
Juergen Thieme
Aleida Perez
Characterization of Potential Micrometeorites by Synchrotron Analysis
Geosciences
micrometeorites
meteorites
synchrotron
X-ray fluorescence
X-ray absorption spectroscopy
X-ray diffraction
author_facet Madison Esposito
Kevin Souhrada
Erin Garland
Mary Kroll
Robert Bolen
Victoria Hernandez
Janet Kaczmarek
David Meisel
Anya Swiss
Paul Northrup
Vivian Stojanoff
Juergen Thieme
Aleida Perez
author_sort Madison Esposito
title Characterization of Potential Micrometeorites by Synchrotron Analysis
title_short Characterization of Potential Micrometeorites by Synchrotron Analysis
title_full Characterization of Potential Micrometeorites by Synchrotron Analysis
title_fullStr Characterization of Potential Micrometeorites by Synchrotron Analysis
title_full_unstemmed Characterization of Potential Micrometeorites by Synchrotron Analysis
title_sort characterization of potential micrometeorites by synchrotron analysis
publisher MDPI AG
series Geosciences
issn 2076-3263
publishDate 2020-07-01
description Micrometeorites (MMs) are small particles that account for most of the extraterrestrial material deposited on Earth. Synchrotron X-ray fluorescence and diffraction allowed for chemical and mineral characterization to distinguish MM from atmospheric particulate. The relative components of iron, nickel, and other elements were considered in the identification of ferrous MM while high amounts of titanium were considered an indication that the particles were of atmospheric origin. Out of 100 samples collected by high school students and teachers, eight were taken to a synchrotron for analysis. Of those eight, three exhibited extraterrestrial compositions. X-ray absorption near-edge structure analysis revealed that the same three samples contained sulfide, the main sulfur form constituent in MM. X-ray microdiffraction analysis showed the presence of the minerals pentlandite and forsterite. Collectively, these results support the extraterrestrial nature of the three particles.
topic micrometeorites
meteorites
synchrotron
X-ray fluorescence
X-ray absorption spectroscopy
X-ray diffraction
url https://www.mdpi.com/2076-3263/10/7/275
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