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Prof. Kazushige Obara07/01/2016, 09:30
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Carsten Rott (Sungkyunkwan University)07/01/2016, 09:35Welcome from the organizers and definition of workshop goalsGo to contribution page
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Prof. Jiro Arafune (Univ. of Tokyo)07/01/2016, 09:45Explanation of basic particle properties of neutrinos are given with the relevant experiments. Several historically important experiments are also briefly introduced including oscillation observation .Go to contribution page
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Hidekazu TANAKA (University of Tokyo)07/01/2016, 10:15This talk will discuss an overview of neutrino oscillation measurementsGo to contribution page
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Kotoyo Hoshina (Earthquake Research Institute, the University of Tokyo)07/01/2016, 11:00For more than 30 years, the idea of probing the interior of the Earth with neutrinos has been discussed. Of all the matter that exists on Earth, only neutrinos can penetrate the maximum thickness of the Earth. Some neutrinos interact with atoms deep inside the Earth where we cannot sample the material. They provide information about the matter density or the electron density of materials along...Go to contribution page
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Akimichi Taketa07/01/2016, 11:30
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William McDonough (University of Maryland)07/01/2016, 13:30Compositional models of the core and lower mantle will be reviewed and assessed. Assumptions in the models along with constraints and uncertainties of the Earth’s interior will be presented. Although a compositional model for the lower mantle that matches that of the upper mantle for major elements is most compatible with observations and constraints, uncertainties are such that competing...Go to contribution page
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Nozomu TAKEUCHI (University of Tokyo)07/01/2016, 14:00I review the seismological studies on the velocity and density in the Earth's core. I will introduce (1) how their models have been obtained, (2) how much uncertainties such models have, and (3) what is important future research topics.Go to contribution page
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Prof. Taku Tsuchiya (Geodynamics Research Center, Ehime University, Japan Dearth-Life Science Institute, Tokyo Institute of Technology, Japan)07/01/2016, 14:30Recent progress in theoretical and computational mineral physics based on the density functional techniques has been dramatic in conjunction with the advancement of computer technologies. It is now possible to predict phase stability and several physical properties of complex minerals quantitatively in the pressure and temperature conditions corresponding directly to the deep planetary...Go to contribution page
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Prof. Hisayoshi Shimizu (Earthquake Research Institute, The University of Tokyo)07/01/2016, 15:00Main part of the geomagnetic field is generated by dynamo process in the Earth’s core. This implies that the geomagnetic field and its secular variation have potential to reveal the dynamics of the Earth’s core. In this talk, I am going to introduce recent progress of the studies of Earth’s core using the geomagnetic field. It has been suggested that decadal variation of the...Go to contribution page
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Prof. Eiji Ohtani (Tohoku University)07/01/2016, 16:00Recent advance in high-pressure mineral physics of the Earth’s central regions are reviewed. The density of the core is lower than that of pure iron under the core conditions. Recent analyses of the equation of state and the sound velocity of solid and liquid iron and iron–nickel alloys strongly suggest that the core contains light elements. Possible candidates for the light elements in the...Go to contribution page
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Shun'ichi Nakai07/01/2016, 16:30The Earth is differentiated and chemically heterogeneous planet. Chondrites, undifferentiated meteorites, have been used to estimate the composition of the Earth. Chondrites are similar in composition to the Sun except volatile elements. They have been considered to keep the composition of the building blocks of the Earth regarding refractory (not volatile) elements. Because both parent and...Go to contribution page
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Fabio Mantovani (INFN - National Institute for Nuclear Physics)07/01/2016, 17:00In July 2005 KamLAND collaboration claimed the first evidence of geoneutrinos on Nature journal. After a decade of measurements, KamLAND (Japan) and Borexino (Italy) experiments confirmed that the technology is ready to measure the geoneutrino signal with enough statistics for answering some fundamental questions of Earth Science. Taking into account that SNO+ (Canada) and JUNO (China)...Go to contribution page
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Carsten Rott (Sungkyunkwan University)08/01/2016, 09:00
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Roger Wendell (The University of Tokyo)08/01/2016, 09:30Hyper-Kamiokande is a next-generation water Cherenkov detector whose expected size and detection efficiency will enable it to make contributions to the field of geophysics, in particular studies of the earth's chemical composition, through observations of atmospheric neutrinos. This talk will focus on the status of the Hyper-Kamiokande project and will discuss sensitivity estimates relevant to...Go to contribution page
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salvatore galata (CNRS)08/01/2016, 10:00
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Olga Suvorova (Russian Academy of Sciences (RU))08/01/2016, 10:30
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Dr Hiroko Watanabe (Tohoku University)08/01/2016, 11:30The **Kam**ioka **L**iquid-scintillator **A**nti-**N**eutrino **D**etector (KamLAND) is located in a rock cavern in the Kamioka mine, 1,000 m below the summit of Mt. Ikenoyama in Japan. KamLAND is marked by the ability to detect low-energy anti-neutrino signals at 1,000 tons of ultra pure liquid scintillator through the inverse \beta reaction, \bar{\nu}_{e} + p \rightarraw e + n. We...Go to contribution page
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William McDonough (University of Maryland)08/01/2016, 12:00
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