Deutsch
 
Hilfe Datenschutzhinweis Impressum
  DetailsucheBrowse

Datensatz

 
 
DownloadE-Mail
  Stardust Interstellar Preliminary Examination VI: Quantitative elemental analysis by synchrotron X-ray fluorescence nanoimaging of eight impact features in aerogel

Simionovici, A. S., Lemelle, L., Cloetens, P., Solé, V. A., Sans Tresseras, J.-A., Butterworth, A. L., et al. (2014). Stardust Interstellar Preliminary Examination VI: Quantitative elemental analysis by synchrotron X-ray fluorescence nanoimaging of eight impact features in aerogel. Meteoritics & Planetary Science, 49(9), 1612-1625. doi:10.1111/maps.12208.

Item is

Externe Referenzen

einblenden:

Urheber

einblenden:
ausblenden:
 Urheber:
Simionovici, Alexandre S.1, Autor
Lemelle, Laurence1, Autor
Cloetens, Peter1, Autor
Solé, Vicente A.1, Autor
Sans Tresseras, Juan-Angel 1, Autor
Butterworth, Anna L.1, Autor
Westphal, Andrew J.1, Autor
Gainsforth, Zack1, Autor
Stodolna, Julien1, Autor
Allen, Carlton1, Autor
Anderson, David1, Autor
Ansari, Asna1, Autor
Bajt, Saša1, Autor
Bassim, Nabil1, Autor
Bastien, Ron K.1, Autor
Bechtel, Hans A.1, Autor
Borg, Janet1, Autor
Brenker, Frank E.1, Autor
Bridges, John1, Autor
Brownlee, Donald E.1, Autor
Burchell, Mark1, AutorBurghammer, Manfred1, AutorChangela, Hitesh1, AutorDavis, Andrew M.1, AutorDoll, Ryan1, AutorFloss, Christine1, AutorFlynn, George1, AutorFrank, David R.1, AutorGrün, Eberhard1, AutorHeck, Philipp R.1, AutorHillier, Jon K.1, AutorHoppe, Peter2, Autor           Hudson, Bruce1, AutorHuth, Joachim2, Autor           Hvide, Brit1, AutorKearsley, Anton1, AutorKing, Ashley J.1, AutorLai, Barry1, AutorLeitner, Jan2, Autor           Leonard, Ariel1, AutorLeroux, Hugues1, AutorLettieri, Robert1, AutorMarchant, William1, AutorNittler, Larry R.1, AutorOgliore, Ryan1, AutorOng, Wei Ja1, AutorPostberg, Frank1, AutorPrice, Mark C.1, AutorSandford, Scott A.1, AutorSchmitz, Sylvia1, AutorSchoonjans, Tom1, AutorSilversmit, Geert1, AutorSrama, Ralf1, AutorStadermann, Frank J.1, AutorStephan, Thomas1, AutorSterken, Veerle J.1, AutorStroud, Rhonda M.1, AutorSutton, Steven1, AutorTrieloff, Mario1, AutorTsou, Peter1, AutorTsuchiyama, Akira1, AutorTyliszczak, Tolek1, AutorVekemans, Bart1, AutorVincze, Laszlo1, AutorVon Korff, Joshua1, AutorWordsworth, Naomi1, AutorZevin, Daniel1, AutorZolensky, Michael E.1, Autor mehr..
Affiliations:
1external, ou_persistent22              
2Particle Chemistry, Max Planck Institute for Chemistry, Max Planck Society, ou_1826291              

Inhalt

einblenden:
ausblenden:
Schlagwörter: -
 Zusammenfassung: Hard X-ray, quantitative, fluorescence elemental imaging was performed on the ID22NI nanoprobe and ID22 microprobe beam lines of the European Synchrotron Research facility (ESRF) in Grenoble, France, on eight interstellar candidate impact features in the framework of the NASA Stardust Interstellar Preliminary Examination (ISPE). Three features were unambiguous tracks, and the other five were identified as possible, but not definite, impact features. Overall, we produced an absolute quantification of elemental abundances in the 15 <= Z <= 30 range by means of corrections of the beam parameters, reference materials, and fundamental atomic parameters. Seven features were ruled out as interstellar dust candidates (ISDC) based on compositional arguments. One of the three tracks, I1043,1,30,0,0, contained, at the time of our analysis, two physically separated, micrometer-sized terminal particles, the most promising ISDCs, Orion and Sirius. We found that the Sirius particle was a fairly homogenous Ni-bearing particle and contained about 33 fg of distributed high-Z elements (Z > 12). Orion was a highly heterogeneous Fe-bearing particle and contained about 59 fg of heavy elements located in hundred nanometer phases, forming an irregular mantle that surrounded a low-Z core. X-ray diffraction (XRD) measurements revealed Sirius to be amorphous, whereas Orion contained partially crystalline material (Gainsforth et al. 2014). Within the mantle, one grain was relatively Fe-Ni-Mn-rich; other zones were relatively Mn-Cr-Ti-rich and may correspond to different spinel populations. For absolute quantification purposes, Orion was assigned to a mineralogical assemblage of forsterite, spinel, and an unknown Fe-bearing phase, while Sirius was most likely composed of an amorphous Mg-bearing material with minor Ni and Fe. Owing to its nearly chondritic abundances of the nonvolatile elements Ca, Ti, Co, and Ni with respect to Fe, in combination with the presence of olivine and spinel as inferred from XRD measurements, Orion had a high probability of being extraterrestrial in origin.

Details

einblenden:
ausblenden:
Sprache(n):
 Datum: 2014-09
 Publikationsstatus: Erschienen
 Seiten: -
 Ort, Verlag, Ausgabe: -
 Inhaltsverzeichnis: -
 Art der Begutachtung: -
 Identifikatoren: ISI: 000342912100006
DOI: 10.1111/maps.12208
 Art des Abschluß: -

Veranstaltung

einblenden:

Entscheidung

einblenden:

Projektinformation

einblenden:

Quelle 1

einblenden:
ausblenden:
Titel: Meteoritics & Planetary Science
Genre der Quelle: Zeitschrift
 Urheber:
Affiliations:
Ort, Verlag, Ausgabe: -
Seiten: - Band / Heft: 49 (9) Artikelnummer: - Start- / Endseite: 1612 - 1625 Identifikator: ISSN: 1086-9379