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我国陆架泥质区沉积动力数值模拟研究进展

乔璐璐 ,  史经昊 ,  高飞 ,  印萍 ,  李建超

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文章导航 > 海洋地质与第四纪地质  > 2014 >  34(3): 155-166
乔璐璐, 史经昊, 高飞, 印萍, 李建超. 我国陆架泥质区沉积动力数值模拟研究进展[J]. 海洋地质与第四纪地质, 2014, 34(3): 155-166. doi: 10.3724/SP.J.1140.2014.03155
引用本文: 乔璐璐, 史经昊, 高飞, 印萍, 李建超. 我国陆架泥质区沉积动力数值模拟研究进展[J]. 海洋地质与第四纪地质, 2014, 34(3): 155-166. doi: 10.3724/SP.J.1140.2014.03155
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QIAO Lulu, SHI Jinghao, GAO Fei, YIN Ping, LI Jianchao. NUMERICAL SIMULATION OF SEDIMENT DYNAMIC PROCESSES FOR MUD AREAS ON THE EAST CHINA SEA CONTINENTAL SHELVES: A REVIEW[J]. Marine Geology & Quaternary Geology, 2014, 34(3): 155-166. doi: 10.3724/SP.J.1140.2014.03155
Citation: QIAO Lulu, SHI Jinghao, GAO Fei, YIN Ping, LI Jianchao. NUMERICAL SIMULATION OF SEDIMENT DYNAMIC PROCESSES FOR MUD AREAS ON THE EAST CHINA SEA CONTINENTAL SHELVES: A REVIEW[J]. Marine Geology & Quaternary Geology, 2014, 34(3): 155-166. doi: 10.3724/SP.J.1140.2014.03155
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我国陆架泥质区沉积动力数值模拟研究进展


doi: 10.3724/SP.J.1140.2014.03155
详细信息

  • 1. 海底科学与探测技术教育部重点实验室, 青岛 266100;

  • 2. 中国海洋大学海洋地球科学学院, 青岛 266100;

  • 3. 青岛海洋地质研究所, 青岛 266071

    • 作者简介:

    乔璐璐(1981-),女,副教授,主要从事沉积动力学研究,E-mail:qiaolulu126@sina.com

  • 基金项目:

    国家自然科学基金项目(41030856)；中国地质调查局海洋地质专项(GZH201100203)；山东省优秀中青年科学家科研奖励基金(BS2012HZ022)；海底科学与探测技术教育部重点实验室开放基金

  • 中图分类号: P736.2

NUMERICAL SIMULATION OF SEDIMENT DYNAMIC PROCESSES FOR MUD AREAS ON THE EAST CHINA SEA CONTINENTAL SHELVES: A REVIEW

More Information

  • 1. Key Lab of Submarine Geosciences and Prospecting Techniques, Ocean University of China, Qingdao 266100, China;

  • 2. College of Marine Geosciences, Ocean University of China, Qingdao 266100, China;

  • 3. Qingdao Institute of Marine Geology, Qingdao 266071, China

  • 摘要: 数值模拟技术可以突破时空限制，是研究沉积动力过程的重要手段。近几十年来，借助数值模式对我国陆架泥质区成因和演化进行了研究，包括泥质区形成的动力机制、沉积速率计算、沉积物的输运和堆积过程、古沉积环境反演等方面。在未来的研究中，仍需从地球系统科学的视角，在改进数值模型，提高沉积动力过程数值模拟技术的基础上，建立陆架大区域、多动力因素耦合数值模型，并开展古今沉积环境数值模拟，探索泥质区形成、演化的时空过程，并探讨陆架海沉积体系相互作用等。
    Abstract: Numerical simulation is one of the important methods to study sediment dynamic processes without limitation of time and space. In recent decades, numerical models have been widely applied to the study of some key problems concerning muddy deposits on continental shelves, for example, the genetic mechanism, deposition rate calculation, sediment transport and deposition, and ancient sedimentary environment interpretation, etc. In the future, further study will be focused on improving simulation models for the study of spatial and temporal evolution of muddy areas and their interactions with other depositional systems, from the viewpoint of whole continental shelf, which is influenced by various factors.
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出版历程
  • 收稿日期:  2013-05-14
  • 修回日期:  2013-07-17

我国陆架泥质区沉积动力数值模拟研究进展

doi: 10.3724/SP.J.1140.2014.03155
  • 1. 海底科学与探测技术教育部重点实验室, 青岛 266100;
  • 2. 中国海洋大学海洋地球科学学院, 青岛 266100;
  • 3. 青岛海洋地质研究所, 青岛 266071
    • 作者简介:

    乔璐璐(1981-),女,副教授,主要从事沉积动力学研究,E-mail:qiaolulu126@sina.com

  • 收稿日期: 2013-05-14
  • 修回日期: 2013-07-17
基金项目:

国家自然科学基金项目(41030856)；中国地质调查局海洋地质专项(GZH201100203)；山东省优秀中青年科学家科研奖励基金(BS2012HZ022)；海底科学与探测技术教育部重点实验室开放基金

  • 中图分类号: P736.2

摘要: 数值模拟技术可以突破时空限制，是研究沉积动力过程的重要手段。近几十年来，借助数值模式对我国陆架泥质区成因和演化进行了研究，包括泥质区形成的动力机制、沉积速率计算、沉积物的输运和堆积过程、古沉积环境反演等方面。在未来的研究中，仍需从地球系统科学的视角，在改进数值模型，提高沉积动力过程数值模拟技术的基础上，建立陆架大区域、多动力因素耦合数值模型，并开展古今沉积环境数值模拟，探索泥质区形成、演化的时空过程，并探讨陆架海沉积体系相互作用等。

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