Dust-obscured radio-emitting tidal disruption event coincident with a high-energy neutrino event
Tianyao Zhou, Xinwen Shu, Guobin Mou, Lei Yang, Luming Sun, Fangkun Peng, Fabao Zhang, Hucheng Ding, Ning Jiang, Tinggui Wang, Yogesh Chandola, Daizhong Liu, Liming Dou, Yibo Wang, Jianguo Wang, Zhongzu Wu, Chenwei Yang
TL;DR
This work addresses the origin of high-energy neutrinos by systematically searching for neutrino-associated, dust-rich TDEs. By cross-matching mid-infrared outbursts with radio transients and IceCube gold-track events, the authors identify J1513+3111 as a spatially and temporally coincident source with IC170514B, and conduct multi-epoch radio studies to model the outflow–CNM interaction via equipartition-based synchrotron analysis. The results indicate a radio-emitting region of $R_{eq}\sim10^{17}$ cm with total nonthermal energy up to $\sim10^{51}$ erg, and a compact VLBI source with $T_b>5\times10^{6}$ K, supporting a non-thermal outflow scenario. The authors argue that while $p\gamma$ processes with IR/UV photons are inefficient for the sub-PeV neutrino, $pp$ collisions in outflow-Cloud interactions provide a plausible mechanism, predicting measurable multi-messenger signatures for future identifications.
Abstract
Despite the growing number of high-energy neutrinos (TeV-PeV) detected by IceCube, their astrophysical origins remain largely unidentified. Recent observations have linked a few tidal disruption events (TDEs) to the production of high-energy neutrino emission, all of which display dust-reprocessed infrared flares, indicating a dust- and gas-rich environment. By cross-matching the neutrino events and a sample of mid-infrared outbursts in nearby galaxies with transient radio flares, we uncover an optically obscured TDE candidate, SDSS J151345.75 $+$ 311125.2, which shows both spatial and temporal coincidence with the sub-PeV neutrino event IC170514B. Using a standard equipartition analysis of the synchrotron spectral evolution spanning 605 days post mid-infrared discovery, we find a little evolution in the radio-emitting region, with a kinetic energy up to $10^{51}$ erg, depending on the outflow geometry and shock acceleration efficiency assumed. High-resolution European VLBI Network imaging reveals a compact radio emission that is unresolved at a scale of $<$ 2.1 pc, with a brightness temperature of $T_b>5\times10^6$ K, suggesting that the observed late-time radio emission might originate from the interaction between a decelerating outflow and a dense circumnuclear medium. If the association is genuine, the neutrino production is possibly related to the acceleration of protons through pp collisions during the outflow expanding process, implying that the outflow-cloud interaction could provide a physical site with a high-density environment for producing the sub-PeV neutrinos. Such a scenario can be tested with future identifications of radio transients coincident with high-energy neutrinos.
