完整后设资料纪录
DC 栏位 | 值 | 语言 |
---|---|---|
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.author | Chi, Chun-Ju | en_US |
dc.contributor.author | Lin, Guey-Lin | en_US |
dc.contributor.author | Huang, Ming-Huey | en_US |
dc.date.accessioned | 2018-01-24T07:37:08Z | - |
dc.date.available | 2018-01-24T07:37:08Z | - |
dc.date.issued | 2016 | en_US |
dc.identifier.uri | http://etd.lib.nctu.edu.tw/cdrfb3/record/nctu/#GT070152719 | en_US |
dc.identifier.uri | http://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.abstract | This 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.iso | zh_TW | en_US |
dc.subject | 极高能天文微中子 | zh_TW |
dc.subject | GZK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.subject | SHINIE | zh_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.subject | ARIANNA | zh_TW |
dc.subject | BedMap2 | zh_TW |
dc.subject | Ultra-High Energy Astrophysical Neutrinos | en_US |
dc.subject | GZK Neutrinos | en_US |
dc.subject | Monte-Carlo Simulation | en_US |
dc.subject | Antarctica | en_US |
dc.subject | Slant Depth | en_US |
dc.subject | Azimuth Angle | en_US |
dc.subject | SHINIE | en_US |
dc.subject | ARA | en_US |
dc.subject | ANITA | en_US |
dc.subject | Ice-Cube | en_US |
dc.subject | Ross Shelf | en_US |
dc.subject | ARIANNA | en_US |
dc.subject | BedMap2 | en_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.title | The effect of local geographic structure on the detection of ultra-high energy astrophysical neutrinos | en_US |
dc.type | Thesis | en_US |
dc.contributor.department | 物理研究所 | zh_TW |
显示于类别: | Thesis |