Materials Map

Discover the materials research landscape. Find experts, partners, networks.

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The Materials Map is an open tool for improving networking and interdisciplinary exchange within materials research. It enables cross-database search for cooperation and network partners and discovering of the research landscape.

The dashboard provides detailed information about the selected scientist, e.g. publications. The dashboard can be filtered and shows the relationship to co-authors in different diagrams. In addition, a link is provided to find contact information.

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Materials Map under construction

The Materials Map is still under development. In its current state, it is only based on one single data source and, thus, incomplete and contains duplicates. We are working on incorporating new open data sources like ORCID to improve the quality and the timeliness of our data. We will update Materials Map as soon as possible and kindly ask for your patience.

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1.080 Topics available

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977 Locations available

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in Cooperation with on an Cooperation-Score of 37%

Topics

Publications (3/3 displayed)

  • 2015Investigations of Saturn’s Main Rings over Broad Range of Wavelengthscitations
  • 2015Saturn B and C ring studies at multiple wavelengthscitations
  • 2013Constraints on Saturn ring particle properties and ring structure: Studies of Saturn's rings from UV to far IRcitations

Places of action

Chart of shared publication
Pilorz, Stu
2 / 2 shared
Ciarniello, Mauro
1 / 11 shared
Colwell, Josh
3 / 3 shared
Brooks, Shawn
1 / 3 shared
Hedman, Matt
3 / 3 shared
Filacchione, Gianrico
3 / 20 shared
Showalter, Mark
1 / 1 shared
Nicholson, Phil
3 / 3 shared
Morishima, Ryuji
3 / 3 shared
Deau, Estelle
3 / 3 shared
Spilker, Linda J.
1 / 1 shared
Spilker, Linda
2 / 3 shared
Chart of publication period
2015
2013

Co-Authors (by relevance)

  • Pilorz, Stu
  • Ciarniello, Mauro
  • Colwell, Josh
  • Brooks, Shawn
  • Hedman, Matt
  • Filacchione, Gianrico
  • Showalter, Mark
  • Nicholson, Phil
  • Morishima, Ryuji
  • Deau, Estelle
  • Spilker, Linda J.
  • Spilker, Linda
OrganizationsLocationPeople

document

Investigations of Saturn’s Main Rings over Broad Range of Wavelengths

  • Pilorz, Stu
  • Ciarniello, Mauro
  • Colwell, Josh
  • Bradley, Todd
  • Brooks, Shawn
  • Hedman, Matt
  • Filacchione, Gianrico
  • Showalter, Mark
  • Nicholson, Phil
  • Morishima, Ryuji
  • Deau, Estelle
  • Spilker, Linda J.
Abstract

An abundance of information about the characteristics of Saturn’s ring particles and their regolith can be obtained by comparing the changes in their brightness, color and temperature with changing viewing geometry over a wide range of wavelengths from ultraviolet through the thermal infrared. Data from Cassini’s Composite Infrared Spectrometer (CIRS), Visual and Infrared Mapping Spectrometer (VIMS), Imaging Science Subsystem (ISS) and Ultraviolet Imaging Spectrograph (UVIS) are jointly studied using data from the lit and unlit main rings at multiple geometries and solar elevations over 11 years of the Cassini mission. Using multi-wavelength data sets allows us to test different thermal models by combining the effects of particle albedo, regolith grain size and surface roughness with thermal emissivity and inertia, particle spin rate and spin axis orientation.CIRS temperatures, ISS colors and UVIS brightness appear to vary noticeably with phase angle, but are not a strong function of spacecraft elevation angle. Color, temperature and brightness dependence on solar elevation angle are also observed. VIMS observations show that the infrared ice absorption band depths change with the solar phase angle, in particular between 0-20° and at high phase. This trend indicates that single scattering approximation is correct only at low phases (<20°) while at high phase multiple scattering must be taken into account.These results imply that the individual properties of the ring particles may play a larger role than the collective properties of the rings, in particular at visible wavelengths. The temperature and color variation with phase angle may be a result of scattering within the regolith, as well as scattering between individual particles or clumps in a many-particle-thick layer. Initial results from our joint studies will be presented.This research was carried out in part at the Jet Propulsion Laboratory, California Institute of Technology, under contract with NASA. Copyright 2015 California Institute of Technology. Government sponsorship is acknowledged....

Topics
  • impedance spectroscopy
  • surface
  • grain
  • grain size
  • phase
  • composite