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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Fixsen, D. J.

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in Cooperation with on an Cooperation-Score of 37%

Topics

Publications (2/2 displayed)

  • 2007Electromagnetic and Thermal Properties of a Conductively Loaded Epoxy45citations
  • 2002The Zodiacal Emission Spectrum as Determined by COBE and Its Implications91citations

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Chart of shared publication
Wollack, Edward
1 / 17 shared
Mirel, Paul
1 / 1 shared
Henry, Ross
1 / 1 shared
Kogut, A.
1 / 1 shared
Dwek, Eli
1 / 10 shared
Chart of publication period
2007
2002

Co-Authors (by relevance)

  • Wollack, Edward
  • Mirel, Paul
  • Henry, Ross
  • Kogut, A.
  • Dwek, Eli
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article

The Zodiacal Emission Spectrum as Determined by COBE and Its Implications

  • Dwek, Eli
  • Fixsen, D. J.
Abstract

We combine observations from the DIRBE and FIRAS instruments on the COBE satellite to derive an annually averaged spectrum of the zodiacal cloud in the 10-1000 μm wavelength region. The spectrum exhibits a break at ~150 μm that indicates a sharp break in the dust size distribution at a radius of about 30 μm. The spectrum can be fitted with a single blackbody with a λ<SUP>-2</SUP> emissivity law beyond 150 μm and a temperature of 240 K. We also used a more realistic characterization of the cloud to fit the spectrum, including a distribution of dust temperatures representing different dust compositions and distances from the Sun, as well as a realistic representation of the spatial distribution of the dust. We show that amorphous carbon and silicate dust with respective temperatures of 280 and 274 K at 1 AU, and size distributions with a break at grain radii of 14 and 32 μm, can provide a good fit to the average zodiacal dust spectrum. The total mass of the zodiacal cloud is 2-11 Eg (Eg=10<SUP>18</SUP> g), depending on the grain composition. The lifetime of the cloud, against particle loss by Poynting-Robertson drag and the effects of solar wind, is about 10<SUP>5</SUP> yr. The required replenishment rate is ~10<SUP>14</SUP> g yr<SUP>-1</SUP>. If this is provided by the asteroid belt alone, the asteroids lifetime would be ~3×10<SUP>10</SUP> yr. But comets and Kuiper belt objects may also contribute to the zodiacal cloud.

Topics
  • impedance spectroscopy
  • amorphous
  • Carbon
  • grain