| 1. | The following table shows the scalability from the single - stream power run to the five - stream throughput run 下表展示了从单条流的能力运行到五条流的吞吐量运行的可伸缩性。 |
| 2. | Secondly , the total resistance is studied directly . the relationship between total stream power and effective stream power is proposed by analogizing the method of engelund 二是直接研究河床总阻力,类比engelund的方法,建立了总水流功率与沙粒水流功率的关系。 |
| 3. | The measured data show that the bedload sediment transport rate is related more closely to the effective stream power within the bed - surface layer than to the river stream power 实测资料表明,推移质输沙率与床面层内有效水流功率有良好的相关性,且高于推移质输沙率与水流功率的相关性。 |
| 4. | Based on the relationship between energy and flow within the bed - surface layer , a relationship between the bedload sediment transport rate and effective stream power within the bed - surface layer is derived 摘要基于床面层内的水流能量关系,推导了推移质输沙率与床面层内有效水流功率的关系式。 |
| 5. | Verification results of more than 2800 runs of channel experiment data and field data show that this formula has good applicability and high accuracy , and is better than the other formulae for bedload sediment transport rate based on the stream power 经2800组试验资料与天然河流资料的检验表明,该关系式的适应性良好,计算精度较高,并优于同类型的基于水流功率的推移质输沙率公式。 |
| 6. | The river mouth delta process is affected by river dynamics and coastal dynamics . the process of river delta is estimated by empirical model , analytical model and minimum stream power method . the three models are verified with field data of the yellow river mouth . the computed results are compared with field data . the demerits of the three models are pointed out 采用经验模型、分析模型和最小功率方法研究河口三角洲演变过程.根据黄河河口三角洲资料,利用三个模型计算了河口三角洲岸线或沙咀宽度及岸线的平均延伸情况及对河口近口段河道水位的影响,比较分析了各模型的计算结果,指出了模型不足之处 |
| 7. | Abstract : the effective shear stress of sediment transport is analyzed theoretically and tested by experimental data . the result shows that the effective shear stress is neither the overall shear stress nor the sand grain shear stress , but the geometric mean of these two stresses . the effective shear stress not only generalizes the flow intensity but also summarizes the flow intensities of mean flow velocity , stream power and unit stream power 文摘:本文通过理论分析及实测资料检验表明,无论对于何种泥沙运动状态,决定泥沙运动的有效切应力既不是沙粒切应力又不是全部切应力,而是介于两者之间,近似为沙粒切应力与全部切应力的几何平均值.这一有效切应力不但是对切应力类水流强度指标的总结,还可以概括平均流速和水流功率等水流强度指标 |