中国地质调查局青岛海洋地质研究所主办
高级检索

河口冲刷区泥沙空间分布与流速关系遥感解译标志

,  ,  , 

文章导航 > 海洋地质与第四纪地质 > 2008 > 28(2): 31-35

上一篇

下一篇

陈军, 温珍河, 丰佳佳, 陈峰. 河口冲刷区泥沙空间分布与流速关系遥感解译标志[J]. 海洋地质与第四纪地质, 2008, 28(2): 31-35.
引用本文: 陈军, 温珍河, 丰佳佳, 陈峰. 河口冲刷区泥沙空间分布与流速关系遥感解译标志[J]. 海洋地质与第四纪地质, 2008, 28(2): 31-35.
shu
CHEN Jun, WEN Zhen-he, FENG Jia-jia, CHEN Feng. THE REMOTE SENSING DISCRIMINATORY MARK OF THE RELATIONSHIP BETWEEN SEDIMENT SPACIAL DISTRIBUTION AND RIVER FLOW SPEED IN EROSION AREA OF RIVER ESTUARY[J]. Marine Geology & Quaternary Geology, 2008, 28(2): 31-35.
Citation: CHEN Jun, WEN Zhen-he, FENG Jia-jia, CHEN Feng. THE REMOTE SENSING DISCRIMINATORY MARK OF THE RELATIONSHIP BETWEEN SEDIMENT SPACIAL DISTRIBUTION AND RIVER FLOW SPEED IN EROSION AREA OF RIVER ESTUARY[J]. Marine Geology & Quaternary Geology, 2008, 28(2): 31-35.
shu

河口冲刷区泥沙空间分布与流速关系遥感解译标志

  • 1 青岛海洋地质研究所, 青岛 266071;

  • 2 中国地质大学(北京), 北京 100083;

  • 3 福州市勘测院, 福州 350003;

  • 4 中国科学院 测量与地球物理研究所, 武汉 430077

  • 基金项目:

    中国地质调查局"1:100万海洋南通幅海洋区域地质调查"项目(200211000001)

详细信息
    作者简介: 陈军(1982-),男,硕士生,从事海洋地理信息系统研究,E-mail:chenjun820711@163.com

  • 中图分类号: P715.6

THE REMOTE SENSING DISCRIMINATORY MARK OF THE RELATIONSHIP BETWEEN SEDIMENT SPACIAL DISTRIBUTION AND RIVER FLOW SPEED IN EROSION AREA OF RIVER ESTUARY

  • 1 Qingdao Institute of Marine Geology, Qingdao 266071, China;

  • 2 China University of Geoseienees, Beijing 100083, China;

  • 3 Fuzhou Investigation and Surveying Institute, Fuzhou 350003, China;

  • 4 Institute of Geodesy and Geophysics, Chinese Academy of Sciences, Wuhan 430077, China

    摘要
  • 通过对泥沙光学光谱特征和河口冲刷区水动力特征的研究和总结,分析了中巴地球资源卫星(China Brazil Earth Resource Satellite) CCD相机B1,B2和B3波段的太湖遥感图像,初步论证了入汇河流流速与冲刷区跨度的关系,以及遥感定量河口泥沙交换强度和动态反映冲积扇发育方向及强度的可行性,并提出了河口泥沙交换强度的判别标志。
    Based on research and conclusion of the silt spectra feature and the water power of erosion in river mouth area, we analyzed remote sensing images of Taihu area showed in B1, B2 and B3 bands from China Brazil Earth Resource Satellite's CCD cameras. The results preliminarily demonstrated that there was relationship between the radius of erosion area and the speed of river inflow, and it is possible to use remote sensing method to quantitatively analyze exchange intensity of sediments in river estuary and dynamically reflect the development direction of alluvial fan. At the same time discriminatory mark for exchange intensity of sediments in remote sensing images is proposed.
    • HTML全文
  • 加载中
    • 相关文章
  • 施引文献
  • 资源附件(0)
  • 加载中
计量
  • 文章访问数:  849
  • PDF下载数:  2
  • 施引文献:  0
出版历程
收稿日期:  2007-11-11
修回日期:  2008-01-30

目录

    版权所有：中国地质调查局发展研究中心 copyright @2020
    返回