Kamioka Liquid Scintillator Antineutrino Detector
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Coordinates: -- The Kamioka Liquid Scintillator Antineutrino Detector (KamLAND) is an experimental device that was built at the Kamioka Observatory, an underground Neutrino Observatory near Toyama, Japan. Its purpose was to detect electron antineutrinos. The device is situated in a horizontal mine drift in the old Kamiokande cavity in the Japanese Alps. The site is surrounded by 53 Japanese commercial nuclear reactors. Nuclear reactors produce electron antineutrinos (ν
e) during the decay of radioactive fission products in the nuclear fuel. Like the intensity of light from a light bulb or a distant star, the isotropically emitted ν
e flux decreases as 1/R2 for increasing distance R from the reactor. The experiment is sensitive up to an estimated ~25% of antineutrinos from nuclear reactors that exceed the threshold energy of 1.8 MeV and thus produce a signal in the detector.
If neutrinos have mass, they may "oscillate" into flavors that an experiment may not be able to detect, leading to a further dimming, or "disappearance," of the electron antineutrinos (see neutrino oscillation). KamLAND is at a flux weighted average distance of ~180 km from the reactors, which makes the experiment sensitive to the neutrino mixing associated with the large mixing angle (LMA) solution to the solar neutrino problem.
The KamLAND Detector
KamLAND consists of an 18 m diameter stainless steel spherical vessel with 1,879 large (50cm diameter) photo-multiplier tubes mounted on the inner surface. The sphere contains a 13 m diameter nylon balloon filled with liquid scintillator. The scintillator consists of 1,000 metric tons of mineral oil, benzene and fluorescent chemicals. Outside of the balloon, non-scintillating, highly purified oil provides buoyancy for the balloon and acts as a shield against external radiation. A 3.2 kiloton* cylindrical water Cherenkov detector surrounds the vessel. It acts as a muon veto counter and provides shielding from cosmic rays and radioactivity.
Electron antineutrinos (ν
e) are detected through the inverse beta decay reaction (ν
e + p → e+ + n ) which has a 1.8MeV ν
e energy threshold. The prompt scintillation light from the positron (e+) gives an estimate of the incident antineutrino energy, Eν = Eprompt + <En> + 0.9 MeV, where Eprompt is the prompt event energy including the positron kinetic energy and the e+–e− annihilation energy. The quantity <En> is the average neutron recoil energy, which is only a few tens of keV. The neutron captures on hydrogen ~200 µs later, emitting a characteristic 2.2 MeV γ ray. This delayed coincidence signature is a very powerful tool for distinguishing antineutrinos from backgrounds produced by other particles.
To compensate for the loss in ν
e flux due to the long baseline, KamLAND has a much larger detection volume compared to earlier experiments. The KamLAND experiment uses a 1 kt detection mass, two orders of magnitude bigger than the previous largest experiment. However, the increased volume of the detector also demands more shielding from cosmic rays, which effectively means that the detector has to be placed underground.
Studying neutrino oscillation
KamLAND started data taking in January 17 2002, and with only 145 days of data, reported its first results (Eguchi et al., 2003). Without neutrino oscillation, the experiment expected to see 86.8±5.6 events, with 2.8 background events after all event cuts. However, only 54 events were observed. KamLAND confirmed this result with a 515 day data sample (Araki et al., 2005), when 365.2±23.7 events were expected in the absence of oscillation, while 258 events were observed (with 17.8±7.3 background events). This establishes antineutrino disappearance at the 99.998% significance level.
The KamLAND detector not only measures the total number of antineutrinos, but also measures their energy. The shape of this spectrum carries additional information that can be used to investigate the neutrino oscillation. Different oscillation hypotheses are investigated by fitting them to the data. Statistical tests show that the distortion of the spectrum is inconsistent with the no-oscillation hypothesis and is also inconsistent with two alternative neutrino disappearance mechanisms, namely the neutrino decay and de-coherence models. However, the spectrum is consistent with neutrino oscillation and a fit provides the values for the Δm2 and θ parameters. Since KamLAND measures Δm2 most precisely and the solar experiments exceed KamLAND's ability to measure θ, the most precise oscillation parameters are obtained by combining the results from solar experiments and KamLAND. Such a combined fit gives Δm2 = 7.9+0.6
−0.5×10−5 eV2 and tan2θ = 0.40+0.10
−0.07 , the best solar neutrino oscillation parameter determination to date.
Geologically produced antineutrinos
KamLAND also published a recent investigation of geologically produced antineutrinos (so-called geoneutrinos). These neutrinos are produced in the decay of thorium and uranium in the Earth's crust and mantle. (Araki et al., 2005)
- Abe S, et al. [KamLAND Collaboration] (2008). "Precision Measurement of Neutrino Oscillation Parameters with KamLAND". Physical Review Letters 100 (22): 221803. arXiv:0801.4589. Bibcode:2008PhRvL.100v1803A. doi:10.1103/PhysRevLett.100.221803. PMID 18643415.
- Araki T, et al. [KamLAND Collaboration] (2005). "Experimental investigation of geologically produced antineutrinos with KamLAND". Nature 436 (7050): 499–503. Bibcode:2005Natur.436..499A. doi:10.1038/nature03980. PMID 16049478.
- Araki T, et al. [KamLAND Collaboration] (2005). "Measurement of neutrino oscillation with KamLAND: evidence of spectral distortion". Physical Review Letters 94 (8): 081801–081806. arXiv:hep-ex/0406035. Bibcode:2005PhRvL..94h1801A. doi:10.1103/PhysRevLett.94.081801. PMID 15783875.
- Eguchi K, et al. [KamLAND Collaboration] (2004). "High sensitivity search for ν
e's from the sun and other sources at KamLAND". Physical Review Letters 92 (7): 071301–071305. arXiv:hep-ex/0310047. Bibcode:2004PhRvL..92g1301E. doi:10.1103/PhysRevLett.92.071301.
- Eguchi K, et al. [KamLAND Collaboration] (2003). "First results from KamLAND: evidence for reactor antineutrino disappearance". Physical Review Letters 90 (2): 021802–021807. arXiv:hep-ex/0212021. Bibcode:2003PhRvL..90b1802E. doi:10.1103/PhysRevLett.90.021802. PMID 12570536.
- "KamLAND". Retrieved June 28, 2007.
- "The Kamioka Liquid-scintillator Anti-Neutrino Detector (KamLAND)". Retrieved November 4, 2005.