| 基于Fluent数值模拟的冰湖涌浪分析 ——以西藏聂拉木县嘉龙错为例 |
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| 引用本文： | 阿如汉,涂杰楠,刘红岩,童立强,郭兆成.基于Fluent数值模拟的冰湖涌浪分析 ——以西藏聂拉木县嘉龙错为例[J].冰川冻土,2018,40(4):837-845. |
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| 作者姓名： | 阿如汉 涂杰楠 刘红岩 童立强 郭兆成 |
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| 作者单位： | 中国地质大学(北京)工程技术学院,北京,100083;中国国土资源航空物探遥感中心,北京,100083 |
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| 基金项目： | 中国地质调查局"青藏冰川变化与冰湖溃决灾害遥感综合调查"项目（DD20160342）资助 |
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| 摘 要： | 冰湖溃决洪水或泥石流（GLOF）是青藏高原主要灾害之一，其形成的灾害链对人民的生命财产安全造成了严重的威胁，其中冰崩导致的冰湖溃决是GLOF的主要灾害形式，但由于其发生位置偏远、间隔时间长、随机性强，导致实地观测资料缺乏，冰崩入湖形成的涌浪机理和过程仍不清晰，而涌浪的规模是GLOF造成下游灾害大小的最主要因素。为分析冰湖涌浪的产生、沿程传播过程和对冰碛坝的爬坡高度，以西藏聂拉木县嘉龙错为例，采用有限体积法，基于流体计算软件Fluent，模拟了嘉龙错补给冰川发生冰崩导致冰湖涌浪的过程。结果表明：数值模拟能较好地对涌浪的产生、规模、沿程传播和对岸爬坡过程进行再现，涌浪初始高度随着冰湖水深、冰体入湖速度和冰体厚度的增加而增大，涌浪高度增加趋势随着冰体入湖速度和冰湖水深的增加而增大，随着冰体厚度的增加而减小。
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| 关 键 词： | 涌浪 冰湖 数值模拟 Fluent 嘉龙错 |
| 收稿时间： | 2018-01-22 |
| 修稿时间： | 2018-04-26 |
Numerical simulation of the glacier lake surge based on Fluent: a case study of Jialong Co,Nyalam County,Tibet |
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| Aruhan,TU Jienan,LIU Hongyan,TONG Liqiang,GUO Zhaocheng.Numerical simulation of the glacier lake surge based on Fluent: a case study of Jialong Co,Nyalam County,Tibet[J].Journal of Glaciology and Geocryology,2018,40(4):837-845. |
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| Authors: | Aruhan TU Jienan LIU Hongyan TONG Liqiang GUO Zhaocheng |
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| Institution: | 1. College of Engineering and Technology, China University of Geosciences(Beijing), Beijing 100083, China;2. China Aero Geophysical Survey and Remote Sensing Center for Land and Resources, Beijing 100083, China |
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| Abstract: | Glacier lake outburst floods (GLOF) is one of the major disasters in the Tibetan Plateau, which results in a serious threat to people's life and property. The size of the surge caused by glacier collapse is the most important factor of GLOF. However, due to its remote location, long interval time and strong randomness, there is no in-situ observation till now. So far, the research about the size of the surge caused by ice collapse is fruitless till now. By using the finite volume method and CFD software Fluent, the surge process of Jialong Co when the feeding glacier collapsed has been simulated. Process of the initial surge has been analyzed, as well as, the surge wave propagation along the path and the height of the surge at the opposite bank. The results have been compared with the calculation given by PAN Jiazheng's method. Finally, it was found that the numerical simulation could well reproduce the surge wave formation, scale, propagation and slope climbing, so it is believed that the simulation would provide new ideas for the risk assessment and the study of GLOF. |
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| Keywords: | surge glacier lake numerical simulation Fluent Jialong Co |
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