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- An estimation method of bed load transport rate based on the grain froude similarity is proposed. 運用沙粒佛汝德相似的原理,提出了推移質(zhì)輸沙率的推算公式。
- In the meanwhile, the result also show that the section configuration and near watercourse characteristic has influenced gravel bed load transport rate. 河床斷面形態(tài)及其相鄰河道特性對輸沙率也有較大的影響。
- 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. 基于沙粒佛汝德數相似原理,首先推導出利用模型試驗結果估算原型沙波河床上推移質(zhì)輸沙率的推算公式;然后塑造與原型較為一致的床面形態(tài),利用模型試驗對推算公式進(jìn)行了驗證。
- Unified form of bed load transport equation 推移質(zhì)輸沙率公式的統一形式
- Bed load transport under influence of wave and current 波浪水流共同作用下推移質(zhì)輸沙
- MEASURES OF FLOW INTENSITY AND BED LOAD TRANSPORT RATE 水流強度指標與推移質(zhì)輸沙率
- Modeling Method of Bed Load Transport Rate in Rivers with Gravel and Cobble Bed 卵礫石河流推移質(zhì)輸沙率的模擬計算方法
- The Stochastic Nature of Gravel Bed Load Transport in Chuanjiang River 川江卵石推移質(zhì)輸移的隨機性
- Experimental Study on the Effect of Slope Bed on Bed Load Transport Rate under Wave Action 波浪作用下岸灘坡度對推移質(zhì)輸沙率影響的實(shí)驗研究
- Determination of Bed Load Transport Rate of Gravel Bed by Simulation of Flume Experiment 用水槽模擬試驗求卵石河床推移質(zhì)輸沙率
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- bed load transport rate 推移質(zhì)輸沙率
- The instantaneous sediment transportof suspended and bed load are computed, and the sediment transport rates are time-averaged over one wave period. 計算了波浪周期內各個(gè)時(shí)刻瞬時(shí)的懸移質(zhì)和推移質(zhì)泥沙輸沙率,并對輸沙率進(jìn)行時(shí)間平均求得時(shí)間平均的輸沙率。
- 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. 摘要通過(guò)對長(cháng)江口徑流、潮流和波浪共同作用下的泥沙運動(dòng)規律的研究,開(kāi)發(fā)并建立了長(cháng)江口全沙(懸沙和底沙)數學(xué)模型。
- Aggrading streams heavily charged with bed load may fill their channels nearly to the top of the banks. 帶有大量推移質(zhì)的堆積河流可以把河槽淤高到幾乎與岸頂齊平。
- rate of bed load transportation 河床質(zhì)運送速率
- 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推移質(zhì)公式和Eim-stein懸移質(zhì)挾沙能力公式作為控制,求出了坡面徑流的輸沙量和泥沙輸移比。
- Bed load particles move spasmodically, perhaps at long intervals, and are at rest on the stream bed most of the time. 推移質(zhì)顆粒多半作間歇運動(dòng),而大部分時(shí)間則停歇在河床上。
- In the stream with strong bed load movement there is no benthic macroinvertebrate. 河勢散亂且河床運動(dòng)劇烈的支流物種豐度和密度均很低甚至為零,生態(tài)條件差。
- Hubbell,D.W.,Stevens,H.H.,Skinner,J.V.,and Beverage,J.P.,1987,Laboratory data on coarse-sediment transport for bed load sampler calibrations : U。S. Geological Survey Water-Supply paper 2299,31 P. 致謝:本課題為中美地表水水文科學(xué)合作協(xié)議附件四全沙輸移項目課題。作者對美國拉斯維拉斯火山觀(guān)測站和中國長(cháng)江委水文局有關(guān)人員為各項試驗給予的幫助表示衷心感謝!