1) River baseline
河道基线
2) channel center line
河道中线
1.
Using the restrain of channel center line to improve the precision of fluvial reservoir modeling;
提高河流相储层建模精度的河道中线约束方法
3) river shoreline
河道岸线
1.
Based on an analysis of the problems existing in the river shoreline space utilization in cities and towns of Guangxi,the author probed into the modes and principals of shoreline space planning in cities and towns.
分析了广西城镇河道岸线空间利用中存在的问题,探讨了城镇岸线空间规划的模式和原则,针对城镇河道岸线空间控制利用规划的误区,提出可持续发展、保护生态等针对性的处理措施和建议。
4) bedrock channel
基岩河道
1.
The quantitative research of geomorphologic revolution in bedrock channel fluvial landscape plays a significant role in the discussion of the relationship among tectonics,climate and surface process.
造山带基岩河道流域地区的地貌演化定量化的分析主要关注气候、构造等外在因素以及河流内在调节机制对地貌演化的影响。
2.
The quantitative research of geomorphologic evolution in bedrock channel fluvial landscape plays a significant role in the discussion of the relationship among tectonics,climate,and surface process.
基岩河道流域地区的地貌演化定量化研究在构造-气候-表面过程关系的探讨中具有十分重要的意义。
5) flow profiles in river
河道水面线
1.
After introducing various uncertain factors including a stochastic initial condition,a stochastic coefficient and a stochastic input term into calculating program of flow profiles in river, a stochastic differential equation is established.
将各种不确定性因素（包括随机初值条件、随机系数和随机作用项等）引入河道水面线的推求过程，建立了计算河道水面线的随机微分方程。
6) water surface curves of natural watercourse
天然河道水面线
1.
The shortcomings of the traditional methods that trial-and-error method, approximate solution and iteration method were used to compute the water surface curves of natural watercourses resulting in large amount of calculations, low precise and complex resolving problems.
传统的计算天然河道水面线的方法是试算法,迭代法和图解法等,这些方法的缺点是计算量大、精度不高,无法控制全河段误差,将其看作是全河段总计算误差,即一复杂非线性优化最小问题,运用实数编码的加速遗传算法求解天然河道水面线。
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