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Setup of a Drift Tube Muon Tracker and Calibration of Muon ...

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Counts / 2 MeV / 345.3 days45403530252015DataBPS09(GS98)+LMA−MSWBPS09(AGS05)+LMA−MSW10504 6 8 10 12 14Energy [MeV]Figure 4.9: 8 B neutrino spectrum measured by Borexino. The red dots show thespectrum after data selection <strong>and</strong> background subtraction. Also shown are the expectedvalues from current SSMs with high (BPS09(GS98)) <strong>and</strong> low (BPS09(AGS05))metallicity under the assumption <strong>of</strong> LMA-MSW oscillations. Figure from [75].with the prediction <strong>of</strong> LMA-MSW oscillations assuming ∆m 2 = 7.69 ×10 −5 eV 2 <strong>and</strong>tan 2 θ = 0.45 also included in the plot.The 8 B neutrino flux derived from the data is found to be (2.7±0.4 stat ±0.2 syst )×10 6 cm −2 s −1 above 5 MeV <strong>and</strong> (2.4±0.4 stat ±0.1 syst )×10 6 cm −2 s −1 above 3 MeV. Thiscompares to an expected flux predicted by the SSM <strong>of</strong> (5.88 ± 0.65) × 10 6 cm −2 s −1with no oscillation, thus confirming solar ν e disappearance. The average ν e survivalprobability ¯P ee has been calculated for both energy regions. For a mean energy <strong>of</strong>8.9 MeV a value <strong>of</strong> P ee = 0.29 ± 0.10 for 8 B neutrinos is obtained. Comparing thisresult with the survival probability <strong>of</strong> the mono energetic 0.862 MeV 7 Be neutrinospresented in the previous section allows again to test the matter enhanced oscillationmechanisms <strong>of</strong> solar neutrinos. Both probabilities are shown in Fig. 4.10 among theearlier results from SNO <strong>and</strong> the radio chemical experiments. The data confirm theMSW-LMA solution for matter enhanced oscillations <strong>of</strong> solar neutrinos. However,whereas the MSW-LMA model seems to be favored also in combination with theother solar oscillation experiments, recent analyses including also the KamLANDdata see hints for possible non st<strong>and</strong>ard interactions [76].4.4.3 Anti Electron Neutrinos – Geo-NeutrinosThe observation <strong>of</strong> geo-neutrinos has been first reported by KamLAND in 2005 [49].Although Borexino is smaller than the KamLAND detector it has the advantage <strong>of</strong>a significantly lower anti neutrino background from nuclear power plants. Also, theintrinsic radioactive background is much lower <strong>and</strong> thus a successful observation <strong>of</strong>geo-neutrinos was reported in 2010 [50].The results are based on a 252.6 ton year fiducial exposure. Altogether 21 ¯ν ec<strong>and</strong>idate events could be identified. Anti electron neutrinos have two main sourceson Earth: they are produced at nuclear reactors <strong>and</strong> they are emitted in β − decays.65

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