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Closing the Window on Strongly Interacting Dark Matter

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arxiv 1211.1951 v1 pith:DKQO3X3J submitted 2012-11-08 astro-ph.CO

classification astro-ph.CO
keywords darkmatterconstraintearthcrossparticlesanalysisclosing
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Constraints are placed on the spin-independent interaction cross section of dark matter with regular matter by refining two methods. First, dark matter--cosmic ray interactions are considered, wherein cosmic ray protons collide with dark matter to contribute to the gamma ray sky. This constraint is developed using the NFW and Moore dark matter density profiles and new data from the Fermi gamma ray space telescope. Second, the Earth capture scenario is considered, wherein particles that are captured self-annihilate at Earth's center, thus adding to its internal heat flow. The constraint presented here is developed based on analysis of the drift time of dark matter particles through Earth, modeled as a core composed of iron and a mantle composed of oxygen with linear density gradients between layers. An analysis of the cosmic ray constraint (which rules out dark matter--regular matter interaction cross sections greater than its value) shows that it overlaps significantly with the Earth drift time constraint (which rules out cross sections smaller than its value), closing the window on strongly interacting dark matter particles up to a mass of about 10^{17} GeV when combined with other exclusions.

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Cited by 2 Pith papers

Reviewed papers in the Pith corpus that reference this work. Sorted by Pith novelty score. Full citation record

  1. Complementary Planetary Spectroscopy Probes of Dark Matter

    hep-ph 2025-08 conditional novelty 6.0 of 10

    Dark matter annihilation energy deposited in planetary atmospheres and interiors, compared against existing UV airglow and heat flow measurements, yields new sub-GeV scattering constraints and long-lived mediator reach.

  2. Can a Dark Inferno Melt Earth's Core?

    hep-ph 2025-05 conditional novelty 6.0 of 10

    Dark matter annihilation inside Earth would melt a substantial fraction of the inner core for cross sections previously allowed by surface heat-flow limits.

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