1) overbank flow
漫滩流
2) overbank flow
漫滩流动
1.
The 3-D k-ε turbulence hydrodynamic model in curvilinear coordinates is established to simulate the overbank flow in the curved channel with irregular terrain in this paper.
本文采用非正交三维曲线坐标下的k-ε双方程湍流数学模型,对弯曲不规则地形的渠道和漫滩流动进行数值模拟。
3) bankfull discharge
漫滩流量
4) overbank
漫滩
1.
3-D numerical simulation on overbank steady open channel flows in compound channels;
漫滩恒定明渠水流的三维数值模拟
5) inundation
漫滩
1.
A numerical study on storm surge and inundation induced by hurricanes in the nearshore of Tianjin;
天津近岸台风暴潮漫滩数值模式研究
2.
A Numerical Study on Hurricane Induced Storm Surge and Inundation in the Near Shore of TianJin;
天津近岸台风暴潮漫滩数值模拟研究
3.
In order to forecast the storm surge inundation, a two-dimensional forecast model of storm surge inundation is established.
本文建立了一个二维风暴潮漫滩数值预报模式，用交序法对二维全流方程组进行了求解，并采用干湿网格法对岸边界进行处理，实现了岸界的移动。
6) river floodplain
河漫滩
1.
A sediment core of 549 cm is collected from the river floodplain of Yellow River in Sanmenxia Reservoir for the test of the concentrations of organochlorine pesticides(OCPs) and minerals.
沉积柱取于三门峡水库黄河河漫滩,总长549 cm,采用GC-ECD气相色谱仪和X射线衍射仪分别测定了沉积物中有机氯农药的质量分数和矿物成分。
2.
Man-made radionuclide of Cesium-137 can be as environment tracer to research the sediments on river floodplains.
人工同位素137Cs可以作为环境示踪因子研究河漫滩沉积物。
参考词条
补充资料：优流漫陀
【优流漫陀】
（地名）Uruman!d!a，又作优留曼荼。山名。阿育经七曰：“优流漫，山名，此翻大醍醐。”翻梵语曰：“优留曼荼，大醍醐也。”
（地名）Uruman!d!a，又作优留曼荼。山名。阿育经七曰：“优流漫，山名，此翻大醍醐。”翻梵语曰：“优留曼荼，大醍醐也。”
说明：补充资料仅用于学习参考，请勿用于其它任何用途。