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黄河入海泥沙扩散与河海相互作用 被引量:18

SUSPENDED SEDIMENT DISPERSAL AND INTERACTION OF RIVER SEA OFF THE YELLOW RIVER MOUTH
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摘要 根据黄河口卫星遥感数据和河口滨海区水文、泥沙实测资料,对河口区洪水的平面扩散和含沙水层特征进行分析,结果表明:在洪水期,河口高高潮到低低潮线之间主河道两侧存在大范围漫流区,片状水流汇入网状汊沟入海,主河槽过流仍很明显,随着流量减小,漫流现象减弱乃至消失,推测口门区主河道的造床流量约1000m3/s;TM1~3合成与TM6温度制图发现,在河口浅水区存在河海相互作用的混合带,混合带宽度与河流流量成正比,混合带中富集了大量悬浮泥沙,造成河口区快速沉积,黄河口滨海区切变锋常在此带中形成,实测锋带的总密度高于围域水体,表明切变锋具有二次发射异重流的能力。将实测获得的水体含沙量C、盐度S、流速V、水体剩余密度σt(与温度、盐度有关)、水体总剩余密度σ及水层厚度h进行聚类分析,对黄河口滨海区不同河流来水来沙条件下的水层进行分类,并对各种水层特征及水层垂向组合特征进行了分析,即洪水期滨海区属不均匀流体,成层性明显,河口来水来沙对其分层起重要作用,共区分出6种典型水层,三种异重羽状流层(高、中、低)在大水期经常发生,频率达42.5%。中水期区分出5种水层类型,明显反映出盐水的作用加强,河流作用表现在异轻羽状流层的存在;枯水期? In this paper,a lot of data of Landsat images and measurements are analyzed for studying the surface dispersal and water layer characteristics off the Yellow River mouth during the flood season.The results show that river water flows over the major channel between high high and low low tidal line during the period of flood.The laminar flow water is converged in the net gullies.The major channel is also obvious.The overflow will disappear with the river discharge decreasing.It is predicted that the major channel discharge would be 1000m 3/s.A mixture zone is found off the river mouth based on the Landsat images(TM1,2,3 for suspended silt concentration and TM6 for water temperature).Its width is related to the river discharge and plenty of suspended silts are converged and deposited there.The shearing front is often formed in the mixture zone.The measurement data show that the total density along the front zone is higher than ambient water and some hyperpycnal plumes would be launched from the zone.The water layer characteristics and vertical combination types are studied based on the analysis statistics of silt concentration(C),salinity(S),current velocity(V)and total density(σ and σ t)etc.The results show that the water is unsymmetrical and layered due to the high silt discharge in flood season.The frequency of the hyperpycnal plume is high off the mouth during the period of the river flood (42 5%).Some low density mud layers are identified above the seabed during different periods of the river discarge.
作者 李广雪
出处 《海洋地质与第四纪地质》 CAS CSCD 北大核心 1999年第3期1-10,T001,共11页 Marine Geology & Quaternary Geology
基金 国家自然科学基金
关键词 黄河 入海泥沙 泥沙扩散 河海相互作用 suspended sediment dispersal shear front hyperpycnal plume remote sensing Yellow River mouth
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参考文献15

  • 1李广雪,薛春汀.黄河水下三角洲沉积厚度、沉积速率及砂体形态[J].海洋地质与第四纪地质,1993,13(4):35-44. 被引量:23
  • 2李广雪,成国栋,魏合龙,潘为刚,任于灿,丁东,周永青,赵杰仁.现代黄河口区流场切变带[J].科学通报,1994,39(10):928-932. 被引量:24
  • 3廖家珍 司书亨.黄河河口演变II:河口水文特征及泥沙淤积分布[J].海洋与湖沼,1980,11(4):295-305.
  • 4李泽刚.黄河口拦门沙的形成机制[J].海洋学报,1993,15(1):84-91. 被引量:12
  • 5杨作升 Keller G H 等.现行黄河口水下三角洲海底地貌及不稳定性[J].青岛海洋大学学报,1990,20(1):7-21.
  • 6刘凤岳.黄河入海干流随潮流变化的特征及泥沙运动方向[J].海洋湖沼通报,1985,(2):20-23.
  • 7Li Guangxue,Marine Geology,1998年,149卷,113页
  • 8Li Guangxue,Marine Geology,1998年,149卷,93页
  • 9张宝泉,计算机与环境多因素分析,1993年,359页
  • 10成国栋,黄河三角洲现代沉积作用及模式,1991年,15页

二级参考文献17

  • 1孙效功,海洋学报,1993年,15卷,1期,120页
  • 2黄世光,海洋地质与第四纪地质,1991年,11卷,1期,15页
  • 3王凤聪,海洋湖沼通报,1989年,2期,9页
  • 4叶和松,黄渤海海洋,1989年,7卷,2期,31页
  • 5成国栋,海洋地质与第四纪地质,1987年,7卷,增刊,7页
  • 6任美锷,地理科学,1986年,6卷,1期,1页
  • 7刘凤岳,海洋湖沼通报,1985年,2卷,20页
  • 8张径,山东海洋学院学报,1985年,15卷,2期,96页
  • 9庞家珍,海洋与湖沼,1980年,11卷,4期,295页
  • 10李泽刚,黄河水利科学研究院论文集,1991年

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同被引文献194

引证文献18

二级引证文献133

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