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Simulation of the Planetary Interior Differentiation Processes in the Laboratory
Published on: November 15, 2013
Experimental Limits on Planetary Mass Primordial Black Hole Mergers
William M Campbell1, Leonardo Mariani2, Michael E Tobar1
1University of Western Australia, Quantum Technologies and Dark Matter Labs, Department of Physics, 35 Stirling Highway, Crawley, WA 6009, Australia.
The Multimode Acoustic Gravitational Wave Experiment (MAGE) sets new limits on primordial black hole mergers. This experiment constrains merger rates to a distance of the Solar System, advancing gravitational wave astronomy.
Area of Science:
- Physics
- Astronomy
- Cosmology
Background:
- Gravitational wave astronomy seeks to detect ripples in spacetime.
- Primordial black holes are hypothetical black holes formed in the early universe.
- High-frequency gravitational wave detection is an emerging field.
Purpose of the Study:
- To constrain the merger rate density of primordial black hole binaries.
- To establish new bounds using MHz-regime gravitational wave detection.
- To differentiate gravitational wave signals from background noise.
Main Methods:
- Utilizing cryogenic quartz bulk acoustic wave resonators as strain antennas.
- Collecting 61 days of non-continuous data.
- Employing coincident analysis between multiple detectors to exclude non-gravitational signals.
Main Results:
- Established bounds on the observable merger rate density for specific primordial black hole masses.
- Achieved a maximum limit on the merger rate density of R<1.3×10^18 kpc⁻³ yr⁻¹.
- Constrained yearly mergers to a reach of approximately the Solar System's distance (1.0×10⁻⁶ kpc).
Conclusions:
- The MAGE experiment provides significant constraints on primordial black hole merger rates.
- The findings exclude rare, strong events as non-gravitational background signals.
- This work advances the search for high-frequency gravitational waves and their sources.
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