1) flood-lake facies
洪水-漫湖相
2) Flooded-lake facies
洪水漫湖
3) flood-overlake
洪水-漫湖
1.
It was showed,by cores observation,grain size analysis,logging data and electron microscope observation in Jiyang Paleogene depression,that the sediment of flood-overlake was controlled by ephemeral flood because the lake was shallow and the weather was dry-half dry.
结果表明,济阳坳陷在孔一段到沙四段沉积早期处于湖盆裂陷初期,沉积作用明显受季节性洪水注入影响,在东营、惠民两凹陷形成洪水-漫湖沉积体系。
4) the flood-over lake sedimentary
洪水-漫湖沉积
5) flood plain facies
漫洪相
6) overbank flood
漫滩洪水
1.
Based on an analysis of field data, it is expounded that the overbank flood is of strong capacity in sediment deposition on the flood plain and scouring in the main channel under the condition of continuous shrinkage of channels on the lower Yellow River.
通过实测资料分析,阐明黄河下游宽河道在持续萎缩的情况下漫滩洪水仍具有较强的淤滩刷槽的行洪特点,指出漫滩洪水造成的滩地淤积主要来自于滩槽水流泥沙的横向交换。
2.
With the model test,this paper researches overbank flood sediment concentration and its gradation change rules from Jahe beach to Gao village river section of lower Yellow River.
通过模型试验,研究了黄河下游夹河滩到高村断面河段漫滩洪水含沙量及颗粒级配的沿程变化规律。
补充资料：河道洪水演进(见河道洪水演算法)
河道洪水演进(见河道洪水演算法)
neaao non郎hUi河道洪水演进yanJ县n 见河道洪水演算法。
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