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- An estimation method of bed load transport rate based on the grain froude similarity is proposed. 运用沙粒佛汝德相似的原理,提出了推移质输沙率的推算公式。
- In the meanwhile, the result also show that the section configuration and near watercourse characteristic has influenced gravel bed load transport rate. 河床断面形态及其相邻河道特性对输沙率也有较大的影响。
- In this paper,firstly,the formula for estimating the bed load transport rate in the bed of sand waves of prototype by model experiment based on the similarity of grain Froude number was inferred. 基于沙粒佛汝德数相似原理,首先推导出利用模型试验结果估算原型沙波河床上推移质输沙率的推算公式;然后塑造与原型较为一致的床面形态,利用模型试验对推算公式进行了验证。
- Unified form of bed load transport equation 推移质输沙率公式的统一形式
- Bed load transport under influence of wave and current 波浪水流共同作用下推移质输沙
- MEASURES OF FLOW INTENSITY AND BED LOAD TRANSPORT RATE 水流强度指标与推移质输沙率
- Modeling Method of Bed Load Transport Rate in Rivers with Gravel and Cobble Bed 卵砾石河流推移质输沙率的模拟计算方法
- The Stochastic Nature of Gravel Bed Load Transport in Chuanjiang River 川江卵石推移质输移的随机性
- Experimental Study on the Effect of Slope Bed on Bed Load Transport Rate under Wave Action 波浪作用下岸滩坡度对推移质输沙率影响的实验研究
- Determination of Bed Load Transport Rate of Gravel Bed by Simulation of Flume Experiment 用水槽模拟试验求卵石河床推移质输沙率
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- bed load transport rate 推移质输沙率
- The instantaneous sediment transportof suspended and bed load are computed, and the sediment transport rates are time-averaged over one wave period. 计算了波浪周期内各个时刻瞬时的悬移质和推移质泥沙输沙率,并对输沙率进行时间平均求得时间平均的输沙率。
- Based on the study of sediment transport under the actions of tidal currents and wind waves, a mathematical model of suspended load and bed load for Yangtze Estuary is developed. 摘要通过对长江口径流、潮流和波浪共同作用下的泥沙运动规律的研究,开发并建立了长江口全沙(悬沙和底沙)数学模型。
- Aggrading streams heavily charged with bed load may fill their channels nearly to the top of the banks. 带有大量推移质的堆积河流可以把河槽淤高到几乎与岸顶齐平。
- The Yalin's bed load formula and Einstein's suspended load carring power formula have been used as a control to obtain sediment transport and sediment delivery ratio on the hillslope in the mountain watershed. 用Yalin推移质公式和Eim-stein悬移质挟沙能力公式作为控制,求出了坡面径流的输沙量和泥沙输移比。
- rate of bed load transportation 河床质运送速率
- Bed load particles move spasmodically, perhaps at long intervals, and are at rest on the stream bed most of the time. 推移质颗粒多半作间歇运动,而大部分时间则停歇在河床上。
- Education should not be restricted to any one specific age group. 教育不应限制在任何特定的年龄组上。
- In the stream with strong bed load movement there is no benthic macroinvertebrate. 河势散乱且河床运动剧烈的支流物种丰度和密度均很低甚至为零,生态条件差。