dc.contributor.author
Hunziker, S.
dc.contributor.author
Moragas-Klostermeyer, G.
dc.contributor.author
Hillier, Jon K.
dc.contributor.author
Fielding, L. A.
dc.contributor.author
Hornung, K.
dc.contributor.author
Lovett, J. R.
dc.contributor.author
Armes, S. P.
dc.contributor.author
Fontanese, J.
dc.contributor.author
James, D.
dc.contributor.author
Hsu, H. W.
dc.date.accessioned
2022-09-20T11:23:26Z
dc.date.available
2022-09-20T11:23:26Z
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/36391
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-36107
dc.description.abstract
Impact ionization of high-velocity cosmic dust particles has been used as a basic principle for dust detectors in space for many decades. It has provided optimum means to gain insight into the dust environment in the solar system. The Ulysses Dust Detector System provided for the first time impact ionization-based detection of interstellar dust (ISD) in the solar system and discovered surprisingly heavy ISD particles with sizes up to a few microns. Studies based on astronomical observations of the local interstellar medium, on the other hand, suggested a much smaller upper limit of around 0.25 μm (silica) or 1 μm (graphite) for the size distribution of ISD particles. Therefore, it has been suggested that low-density fluffy dust particles may mimic the impact signals of heavier compact particles. In this work, we discuss a series of impact experiments that have been performed at the Heidelberg dust accelerator facility with the Cosmic Dust Analyzer flight spare unit, to compare the high-velocity impact ionization properties of compact and hollow silicate particles, and carbon aerogel particles with each other and with literature data. The experiments indicate differences in the collected total amount of impact charges and how quickly the charges are collected, between impacts from compact particles and their non-compact counterparts. The results of this first study suggest that fluffy particles generate less ions upon impact than their compact counterparts, opposite to the suggested explanation for the heavy ISD particles. Data from the performed impact experiments indicate that a secondary process (e.g. secondary impacts from ejecta or more target material ionization) could be the main cause for the observed differences. These results imply that the previously detected heavy ISD particles may be real. We identify the key problems with the performed dust experiments and advise that future impact ionization instruments should additionally be calibrated with improved low-density fluffy dust particles that better represent the properties of cosmic dust particles.
en
dc.format.extent
22 Seiten
dc.rights.uri
https://creativecommons.org/licenses/by/4.0/
dc.subject
Impact ionization
en
dc.subject
High-velocity dust impacts
en
dc.subject.ddc
500 Naturwissenschaften und Mathematik::520 Astronomie::520 Astronomie und zugeordnete Wissenschaften
dc.title
Impact ionization dust detection with compact, hollow and fluffy dust analogs
dc.type
Wissenschaftlicher Artikel
dcterms.bibliographicCitation.articlenumber
105536
dcterms.bibliographicCitation.doi
10.1016/j.pss.2022.105536
dcterms.bibliographicCitation.journaltitle
Planetary and Space Science
dcterms.bibliographicCitation.volume
220
dcterms.bibliographicCitation.url
https://doi.org/10.1016/j.pss.2022.105536
refubium.affiliation
Geowissenschaften
refubium.affiliation.other
Institut für Geologische Wissenschaften / Fachrichtung Planetologie und Fernerkundung
refubium.resourceType.isindependentpub
no
dcterms.accessRights.openaire
open access
dcterms.isPartOf.eissn
1873-5088
refubium.resourceType.provider
WoS-Alert