海洋沉积动力过程原位监测平台及其应用

马小川, 范奉鑫, 阎军. 海洋沉积动力过程原位监测平台及其应用[J]. 海洋地质与第四纪地质, 2011, 31(4): 179-185. doi: 10.3724/SP.J.1140.2011.04179
引用本文: 马小川, 范奉鑫, 阎军. 海洋沉积动力过程原位监测平台及其应用[J]. 海洋地质与第四纪地质, 2011, 31(4): 179-185. doi: 10.3724/SP.J.1140.2011.04179
MA Xiaochuan, FAN Fengxin, YAN Jun. IN-SITU MONITORING PLATFORM FOR MARINE SEDIMENT DYNAMICS AND ITS APPLICATION[J]. Marine Geology & Quaternary Geology, 2011, 31(4): 179-185. doi: 10.3724/SP.J.1140.2011.04179
Citation: MA Xiaochuan, FAN Fengxin, YAN Jun. IN-SITU MONITORING PLATFORM FOR MARINE SEDIMENT DYNAMICS AND ITS APPLICATION[J]. Marine Geology & Quaternary Geology, 2011, 31(4): 179-185. doi: 10.3724/SP.J.1140.2011.04179

海洋沉积动力过程原位监测平台及其应用

  • 基金项目:

    中国科学院知识创新工程重要方向资助项目(KZCX2-YW-212-2)

详细信息
    作者简介: 马小川(1985-),男,博士生,主要从事海底地形地貌与海洋沉积动力学研究,E-mail:maxiaochuan1985@126.com
  • 中图分类号: P731.2

IN-SITU MONITORING PLATFORM FOR MARINE SEDIMENT DYNAMICS AND ITS APPLICATION

  • 利用倾斜仪、ADCP、PC-ADP、扇形声纳、OBS等先进仪器组建海洋沉积动力过程原位监测平台,并利用此平台获得了北部湾底部同步连续的波浪数据,流速剖面及近底紊流数据,距底0.5、0.9、1.3 m的悬浮物浓度数据以及不同时间的地貌图像。实际观测表明,原位监测平台能够克服极端条件,系统地监测波流、悬浮物浓度以及地貌演化,获得数据可以为理论研究和工程实践提供支持。根据应用实例,建议加载流速计并减小扇形声纳的扫描范围,来弥补1.2~4 m之间水动力数据的缺失并观测海底微地貌的变化。观测期间水体悬浮物质和海洋生物对光学仪器有较大影响,ABS可能比OBS更适合长期水下悬浮物浓度监测。
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出版历程
收稿日期:  2011-01-21
修回日期:  2011-03-28

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