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dc.contributor.author纪君儒zh_TW
dc.contributor.author林贵林zh_TW
dc.contributor.author黄明辉zh_TW
dc.contributor.authorChi, Chun-Juen_US
dc.contributor.authorLin, Guey-Linen_US
dc.contributor.authorHuang, Ming-Hueyen_US
dc.date.accessioned2018-01-24T07:37:08Z-
dc.date.available2018-01-24T07:37:08Z-
dc.date.issued2016en_US
dc.identifier.urihttp://etd.lib.nctu.edu.tw/cdrfb3/record/nctu/#GT070152719en_US
dc.identifier.urihttp://hdl.handle.net/11536/138999-
dc.description.abstract本文针对极高能天文微中子与地球交互作用进行研究,藉由引入位于南极且具有冰层厚度与海床高程的BedMap2数位高程模型(DEM),增添当地高能天文微中子与地表层真实环境的蒙地卡罗法模拟。模拟前先由DEM计算出一些目前位于南极,建置中或已建置完成之微中子观测实验位置上,各方向的倾斜深度。以倾斜深度计算结果选定位于罗斯冰棚的ARIANNA实验位址,并套用较为符合其实验设计概念的圆饼状侦测器敏感区(DSR),进行单能量的高能天文涛子微中子模拟。得出模拟结果后初步探讨引入模型时,DSR中各方向与各类事件的事例数角分布,以及引起簇射的事例数能量分布。事例数角分布方面,模拟结果符合根据倾斜深度所推论的结果,对于一些特定种类与天顶角方向的事件,有事例数的方位角分布差异:对于能量10^10 GeV与10^10.5 GeV微中子,浅穿地球微中子在本研究定义之方位角210至300度之间,首次发生的电性流(CC)与中性流(NC)交互作用事件有相对较低的事例数;而以涛子衰变占多数的下行微中子所引发再生事件,在方位角210至240度之间则有相对较高的事例数。而再生事件中,涛子衰变与其他交互作用引起的簇射能量分布也有显着的差异。zh_TW
dc.description.abstractThis is a research of the interaction between ultra-high energy astrophysical neutrinos and earth. By introducing the BedMap2 digital elevation model, which has the ice thickness, bed elevation, and surface elevation that are located in Antarctica, we performed Monte-Carlo simulation on the interaction between neutrinos and the local terrain. Before performing the simulation, we selected some locations of astrophysical neutrino observation experiments. Then we calculated the slant depth of all directions by an algorithm and a numerical integration method. Referring to these results, we selected the location of ARIANNA which is located at Ross shelf for our simulations. We constructed a disk shape detector sensitive region for our simulations and generated monoenergetic tau neutrinos at some energy levels between 10^8 GeV and 10^10.5 GeV. The simulation results coincide with our predictions which are according to the slant depth calculations. For 10^10 GeV and 10^10.5 GeV neutrinos we generated, the number of first-generated earth-skimming (The zenith angle θ is between 90° and 91°.) events is relatively low when the azimuth angle φ is between 210° and 300° (Reference vector is pointed to south.). However, the number of regenerated down-going (0° ≤ θ ≤ 89.5°) events is relatively high when 210° ≤ φ ≤ 240°. Most of the regenerated events are tau decay events. For regenerated events, the distributions of shower energy have significant differences between the showers which are created by tau decay and other interaction events.en_US
dc.language.isozh_TWen_US
dc.subject极高能天文微中子zh_TW
dc.subjectGZK微中子zh_TW
dc.subject蒙地卡罗模拟zh_TW
dc.subject南极大陆zh_TW
dc.subject倾斜深度zh_TW
dc.subject方位角zh_TW
dc.subjectSHINIEzh_TW
dc.subject南极天坛阵列zh_TW
dc.subject南极脉冲瞬态天线zh_TW
dc.subject冰立方zh_TW
dc.subject罗斯冰棚zh_TW
dc.subjectARIANNAzh_TW
dc.subjectBedMap2zh_TW
dc.subjectUltra-High Energy Astrophysical Neutrinosen_US
dc.subjectGZK Neutrinosen_US
dc.subjectMonte-Carlo Simulationen_US
dc.subjectAntarcticaen_US
dc.subjectSlant Depthen_US
dc.subjectAzimuth Angleen_US
dc.subjectSHINIEen_US
dc.subjectARAen_US
dc.subjectANITAen_US
dc.subjectIce-Cubeen_US
dc.subjectRoss Shelfen_US
dc.subjectARIANNAen_US
dc.subjectBedMap2en_US
dc.title区域地层结构对极高能天文微中子观测影响zh_TW
dc.titleThe effect of local geographic structure on the detection of ultra-high energy astrophysical neutrinosen_US
dc.typeThesisen_US
dc.contributor.department物理研究所zh_TW
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