1) Alluvial deposit soil from Yangtze River
长江冲积物
2) Changjiang alluvial plain
长江冲积平原
1.
Application of seismic exploration technique to Quaternary study of Changjiang alluvial plain from Jiujiang city to Huangmei county;
浅层地震技术在九江—黄梅长江冲积平原第四纪研究中的应用
3) Lanjiang River alluvium
兰江冲积
1.
In this paper,the topographic features of Lanjiang River alluvium are described in detail,it s mechanics is discussed,and its deposits are classified.
详细论述了兰江冲积地貌的心洲相与漫滩相的沉积 ,对沉积过程中横向环流的心洲作用、河曲作用、支流作用作了探讨 ,并对堆积物作了详细的分类 。
4) Sediment form the Huanghe and Changjiang estuaries
黄河口与长江口沉积物
5) Changjiang diluted water
长江冲淡水
1.
Numerical model simulation of expansion of Changjiang diluted water in summer;
夏季长江冲淡水扩展的数值模拟
2.
Analysis on the path of transportation and diffusion of Changjiang diluted water;
长江冲淡水输运和扩散途径的分析
3.
The main axis of the Changjiang diluted water expands towards the northeast-north after it leaves the mouth (the river discharge in August 2000 is smaller than the long-term average).
采用CTD、多参数环境监测系统 YSI等仪器设备 ,于 2 0 0 0年 8月在长江口外海区对长江冲淡水结构、羽状锋等进行了现场观测。
6) Changjiang River diluted water
长江冲淡水
1.
Based on the remote sensing data of "NOAA-14"in summer 1997 and 1998, It is found that the spreading direction of the Changjiang River diluted water changed in 7~10 days, and pointed out, that it is unreliable for using the traditional oceanographic observation data to explain the mechanism of the spreading direction change of the Changjiang River diluted water.
以 1 997年和 1 998年两个夏季的 6幅“NOAA- 1 4”卫星遥感图像为据 ,反映了长江冲淡水扩展方向的周、旬时段变化。
2.
The monthly salinity and wind data in summers of 1959, 1975～1982 and 1998 were used to analyse and discuss the spreading paths of the Changjiang River diluted water.
利用 1 95 9,1 975 - 1 982年及 1 998年夏季各月黄、东海盐度分布和相应风场资料 ,分析讨论了长江冲淡水夏季的扩展路径。
补充资料：冲积物
通常指河流沉积。具有分选性好、磨圆度高、层理清楚的特点。一般河流上游冲积物颗粒大，下游颗粒小；河床中心颗粒大，河床边缘颗粒小。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条