Program C01-7 | Imaging MeV gamma rays from TGF with high-resolution semiconductor imagers |
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Principal Investigator | NAKAZAWA, Kazuhiro (Nagoya University) |
The MeV gamma rays emitted from lightning activity are the only
direct evidence of large-scale electrostatic acceleration, without no
relation to magnetic field, of electrons in nature (e.g., Dwyer
2012), a high-energy phenomenon that was discovered in the late 1980s
and began to be studied in detail after around 2000.
Thunderstorm gamma rays can be divided into two types: “thunderstorm
gamma ray glow” which is emitted from the thundercloud itself for
several minutes, and “lightning gamma-ray flash” (or Terrestrial
Gamma-ray Flash, a name originating from the fact the it was first
observed by satellites) which is a sudden (about 100 μs) emission
synchronized with lightning discharges. In the winter, the Hokuriku
region is active in lightning activity, and the low cloud height
enables the gamma rays to reach the ground by avoiding atmospheric
absorption, making the region suitable for ground-based
observations. It is attracting attention from around the world. We
have been conducting the GROWTH collaboration and have achieved
world-leading results. In particular, we have confirmed that the
lightning gamma-ray flash has a large dose of around 1.4 μGy in a
short time of around 100 μs. Since this phenomenon contains a large
amount of gamma-rays of >10 MeV, a photonuclear reaction occurs in
the atmosphere, producing a large amount of fast neutrons and
proton-rich nuclei. The main goal of this research is to understand
where the electrons that produce these powerful gamma rays are
accelerated and what is the maximum dose produced.
The ground-based observation of lightning gamma-ray flashes is an
extreme high-luminosity observation, with as many as 10,000 photons
per cm2 arriving in only 100 μs. To capture this,
we are adopting a
semiconductor imager using the recently developed TimePix3 ASIC. The
imager has a temporal resolution of 1.56 ns, a position resolution of
53 μm, and a detector size of
14×14 mm2. Its thickness of
0.5–2 mm)
is thicker than the position resolution, and it therefore can track
the high-energy electrons. Although the electron-positron pairs
produced by 10 MeV gamma-rays penetrate the detector, the direction
of gamma-ray incidence can be determined by observing their tracks.
The goal of this two-year research project is to verify the
observation performance for 10 MeV gamma-rays, to demonstrate the
directional detection capability of the detector, and to actually set
up the detector in the observation hut of the Nagoya University team
in Kanazawa City for observation. If the observation is successful,
we will compare the direction of the 10 MeV gamma-rays with the
positional evaluation of the radio wave observation of the lightning
discharge to identify the location of the electron acceleration.
Fig. 1. (Left) Schematic diagram of electron acceleration in
thundercloud and its observations. (Center) Nagoya-U hut in
Kanazawa City. (Right) Tracking observation of 10 MeV gamma rays interacting in the Si (or CdTe) TimePix3 imager devices
Members
- Principal Investigator
-
NAKAZAWA, Kazuhiro
(Kobayashi-Maskawa Institute for the Origin of Particles and the Universe, Nagoya University)
- Research Collaborators
- TAKAHASHI, Tadayuki (The University of Tokyo)
Reference Materials
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Y. Wada ,T. Enoto ,K. Nakazawa ,Y. Furuta ,T. Yuasa ,Y. Nakamura , …,H. Tsuchiya , “Downward terrestrial gamma-ray flash observed in a winter thunderstorm,” Phys. Rev. Lett. 123, 061103 (2019). -
T. Enoto ,Y. Wada ,Y. Furuta ,K. Nakazawa ,T. Yuasa ,K. Okuda , …,H. Tsuchiya , “Photonuclear reactions triggered by lightning discharge,” Nature 551, 481–484 (2017). DOI: 10.1038/nature24630 . -
K. Nakazawa ,G. Sato ,M. Kokubun ,T. Enoto et al. , “The hard X-ray imager (HXI) onboard Hitomi (ASTRO-H),” J. Astron. Telesc. Instrum. Syst. 4(2), 021410 (2018). -
K. Nakazawa ,K. Oonuki ,T. Tanaka ,Y. Kobayashi et al. , “Improvement of the CdTe diode detectors using a guard-ring electrode,” IEEE Trans. Nucl. Sci. 51(4), 1881–1885 (2004).