夏欣, 贾永刚, 杨秀娟. 浅水岸滩蚀积过程原位监测方法研究现状[J]. 海洋地质与第四纪地质, 2009, 29(6): 137-144. DOI: 10.3724/SP.J.1140.2009.06137
引用本文: 夏欣, 贾永刚, 杨秀娟. 浅水岸滩蚀积过程原位监测方法研究现状[J]. 海洋地质与第四纪地质, 2009, 29(6): 137-144. DOI: 10.3724/SP.J.1140.2009.06137
XIA Xin, JIA Yonggang, YANG Xiujuan. METHODS FOR MONITORING IN-SITU EROSION AND DEPOSITION IN SHALLOW WATER AND TIDAL FLAT AREA[J]. Marine Geology & Quaternary Geology, 2009, 29(6): 137-144. DOI: 10.3724/SP.J.1140.2009.06137
Citation: XIA Xin, JIA Yonggang, YANG Xiujuan. METHODS FOR MONITORING IN-SITU EROSION AND DEPOSITION IN SHALLOW WATER AND TIDAL FLAT AREA[J]. Marine Geology & Quaternary Geology, 2009, 29(6): 137-144. DOI: 10.3724/SP.J.1140.2009.06137

浅水岸滩蚀积过程原位监测方法研究现状

METHODS FOR MONITORING IN-SITU EROSION AND DEPOSITION IN SHALLOW WATER AND TIDAL FLAT AREA

  • 摘要: 系统介绍了具有短时间范围浅水岸滩蚀积过程动态原位监测方法,这些方法监测时段为几天至几年时间尺度。按照时间分辨率大小,这些监测方法可分为非连续监测和半连续监测;按照工作原理,可分为测试沉积量和测试沉积物-水界面高程变化两种类型。在分别介绍各种监测方法功能特点的基础上,进一步分析了各方法的优缺点,指出了今后的发展方向,对相关研究具有很好的参考价值。

     

    Abstract: This paper introduced methods for monitoring in-situ erosion and deposition on short-time scale in shallow water and tidal flat area.Monitoring time scale using these methods is about a few weeks to a few years.In according with temporal resolution,these monitoring methods can be divided into discontinuous and semi-continuous ones; in accordance with the working principles,they are used to test accumulation or elevation changes in sediment-water interfaces.After separately introducing the features of a variety of monitoring methods,this paper further analyzes their different advantages and disadvantages,pointing out future development direction.This paper may have a good reference value to related research.

     

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