1) rapids-forming stage
成滩水位
1.
Based on the analyis of rapids characteristics,the rapids-forming stage,the most turbulent stage in the rapids-forming period are determined.
通过滩性分析可以确定滩险成滩水位、最凶水位、消滩水位(流量)的成滩出现时期及滩段凶、险的定量概念。
2) Bankfull stage
平滩水位
1.
431 4×108 t,while by means of morphological change method and under bankfull stage of 34.
431 4亿t;采用地形法,假设平滩水位为34。
3) bankful stage
漫滩水位
4) water level of regulation
浅滩整治水位
5) bankfull cross-section area
平滩水位下断面面积
6) cause of beach formation
成滩原因
1.
Through comparatively integrated prototype measured data, analysed the water sand condition and variation character of Bantan beach located in the backwater effect region of reservoir head after completion of the Xijin hydropower station on Yujiang, the cause of beach formation of Bantan and its principle of regulation were explored also.
通过较为完整的天然实测资料，分析了郁江西津水电站建成后，处于库尾回水变动区内的滩水沙条件及雅性变化特征，探讨了滩的成滩原因及其整治原则。
补充资料：地下水水位观测(见水位观测)
地下水水位观测(见水位观测)
d ixiashui shuiwei guanee地下水水位观测见水位观测。
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