Astronomers measure the gravitational waves caused by two black holes colliding

Publicly released:
Australia; International; ACT
Photo by BoliviaInteligente on Unsplash
Photo by BoliviaInteligente on Unsplash

Astronomers have seen the gravitational waves from the collision of two black holes, and they can use their observations to find out the mass and spin rate of the black hole that was left behind. Aussie and international astronomers used the Laser Interferometer Gravitational-Wave Observatory (LIGO) in January 2025 to observe and analyse gravitational waves created by two black holes colliding. The collision created a direct gravitational wave that provided the research team with data on the rotation of the event horizon and the surface gravity of the single black hole that remained after the collision.

News release

From: Springer Nature

Astronomy: Gravitational wave signal from a black hole collision

The identification of the wave component of the gravitational-wave signal produced from the collision between two black holes is presented in Nature this week. Observations of the binary black hole merger event called GW250114 provides information about the remnant black hole event horizon —the ‘point of no return’.

Understanding the physics that guide a black hole event horizon is difficult as most observations are indirect; gravitational waves, which are formed by the collision of two black holes, could offer a clearer picture. Previous research has suggested that direct waves, a type of gravitational wave that can characterize the behaviour of the remnant black hole, could be emitted during this process, but no observation has been recorded.

Sizheng Ma and colleagues analysed gravitational wave data from GW250114, a signal from the collision of two merging black holes, detected by the Laser Interferometer Gravitational-Wave Observatory (LIGO) in January 2025. They observed a direct wave from the collision, which behaved like a dampened oscillation with a frequency linked to the horizon’s rotation and a decay rate related to its surface gravity.

Careful modelling of the direct wave can tell us the mass and spin rate of the remnant black hole, and the authors make a preliminary attempt with some simplifying assumptions. Future work will require more accurate waveform models and studies across multiple events to assess the robustness and universality of these signals.

Journal/
conference:
Nature
Research:Paper
Organisation/s: The Australian National University, Perimeter Institute for Theoretical Physics, Canada
Funder: This material is based on work supported by NSF’s LIGO Laboratory, which is a major facility fully funded by the National Science Foundation. We are grateful for computational resources provided by the LIGO Laboratory and supported by National Science Foundation grants PHY–0757058 and PHY–0823459. N.L., O.J.P. and L.S. acknowledge support for this research from the Australian Research Council Centre of Excellence for Gravitational Wave Discovery (OzGrav), project no. CE230100016. L.S. is also supported by the Australian Research Council Discovery Early Career Researcher Award, project no. DE240100206. O.J.P. is supported by the Spanish Ministerio de Ciencia, Innovacion y Universidades Ramon y Cajal, RYC2023-044489-I funded by MCIN/AEI/10.13039/501100011033 and the FSE+ and cofinanced by the Universitat de les Illes Balears (UIB). This work was supported by UIB with funds from the Programa de Foment de la Recerca i la Innovació de la UIB 2024-2026 (supported by the yearly plan of the Tourist Stay Tax ITS2023-086); the Spanish Agencia Estatal de Investigación grants RED2024-153978-E, RED2024-153735-E, funded by MICIU/AEI/10.13039/501100011033 and the ERDF/EU; and the Comunitat Autónoma de les Illes Balears through the Conselleria d’Educació i Universitats with funds from the ERDF (SINCO2022/18146). S.M. acknowledges support for this research at Perimeter Institute, in part from the Government of Canada through the Department of Innovation, Science and Economic Development and by the Province of Ontario through the Ministry of Colleges and Universities. Y.C. is supported by the Brinson Foundation, the Simons Foundation (award no. 568762), and by US NSF grants PHY–2309211 and PHY–2309231. This paper carries LIGO document no. DCC–P2500608.
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