from    
to    
search  

 


人工智能拓展火灾安全研究的进展
From The Sky To The Sea
清华大学材料科学与工程研究院《材料科学论坛》:基于拓扑缺陷理论的轻合金组织设计新...
Quantum information processing based on bosonic modes
报告题目:
工程物理系第205期“工物学术论坛”:Geoneutrinos and heat production in the Earth
 报告人:
William F. McDonough
Professor,University of Maryland,USA
报告时间:
2016-11-28 16:00
报告地点:
清华大学刘卿楼105会议室
主办单位:
工程物理系
  简介:

报 告 摘 要:The Earth’s engine is driven by unknown proportions of primordial energy and heat produced in radioactive decay. Unfortunately, competing models of Earth’s composition reveal an order of magnitude uncertainty in the amount of radiogenic power driving mantle dynamics. Comparison of the flux measured at large underground neutrino experiments with geologically informed predictions of geoneutrino emission from the crust provides the critical test needed to define the mantle’s radiogenic power. We predict the geoneutrino flux at the site of the Jinping Neutrino Experiment (Sichuan, China). Within 8 years, the combination of existing data and measurements from soon to come experiments, including Jinping, will exclude end-member models at the 1σ level, define the mantle’s radiogenic contribution to the surface heat loss, set limits on the composition of the silicate Earth, and provide significant parameter bounds for models defining the mode of mantle convection. The three Asian detectors,KamLAND, JUNO, and Jinping, are separated by only ~< 3000 km (1 mantle depth); thus their geoneutrino measurements may be harnessed to improve the regional crustal models.

报告人简介:Understanding the composition, structure and evolution of the Earth and the other terrestrial planets are dominant themes of my research. The differentiation of the Earth has created 3 highly stratified and distinct reservoirs (i.e., the core, the mantle-crust system, and the atmosphere-hydrosphere system). These reservoirs are in turn themselves internally differentiated. Chemical and isotopic studies of terrestrial and extra-terrestrial samples provide insights into the timing and details of the differentiation of these reservoirs. In addition to developing models for the compositions of the bulk Earth, core and silicate Earth, I use plasma mass spectrometry to analyze samples for their chemical and isotopic compositions. Data from these mass spectrometers are used to improve our understanding of the processes involved in differentiation and the timing of these events.

 

第205期“论坛”主请人联系方式:
陈少敏   62795757   chenshaomin@tsinghua.edu.cn

今日相关信息
纳米磨损研究进展及展望——环境气氛、界面...
Rare-event Simulation for Vulnerabili...
Higher Categories and Topological Qua...
认识与利用个人文献管理软件
工程物理系第206期“工物学术论坛”:“...
 
同类别相关信息
第421期“工物学术论坛”:放疗联合免...
第420期“工物学术论坛”:肿瘤放射治...
第419期“工物学术论坛”:SBRT技术引...
第418期“工物学术论坛”:超级神冈实...
第417期“工物学术论坛”:美国洪水保...
学术活动