測含沙量斷面 的英文怎麼說

中文拼音 [hánshāliángduànmiàn]
測含沙量斷面 英文
sediment range
  • : 動詞1. (測量) survey; fathom; measure 2. (測度; 推測) conjecture; infer
  • : 動詞1 (東西放在嘴裏 不咽下也不吐出) keep in the mouth 2 (藏在裏面; 包含) contain 3 (帶有某種...
  • : 沙動詞[方言] (搖動以清除雜物) shake
  • : 量動1. (度量) measure 2. (估量) estimate; size up
  • : Ⅰ動詞1 (分成段) break; snap 2 (斷絕;隔斷) break off; cut off; stop 3 (戒除) give up; abstai...
  • : Ⅰ名詞1 (頭的前部; 臉) face 2 (物體的表面) surface; top 3 (外露的一層或正面) outside; the ri...
  • 斷面 : section; fracture surface; plane of fracture
  1. The daling river is a river of much bedload. the average of the loss sand can reach 21434. 3 thousandston, and the ratio is 18. 08 kg / m3. to this day, the ratio of sandiness by measuring in the biggest broken surface is 172 kg / m3. the baishi reservoir lies in the city named beipiao which in the middle reaches of the daling river in liaoning province, the income of the reservoir from the trunk stream is 11457 thousandston, and from the branch of the river is 1160 thousandston

    大凌河是個多河流,多年平均懸移質輸可達2143 . 43萬噸,平均為18 . 08kg m ~ 3 ,實最大為172kg m ~ 3 ,白石水庫位於大凌河中游的遼寧省北票市,年入庫,幹流為1145 . 7萬噸,支流?牛河為1160萬噸。
  2. In this paper, some characteristics of flow movement and sediment transport are analyzed by using the flume experiment data. the cross section of compound channel can be divided into four regions : the undisturbed region in main channel, the interactive region between channel and plain, the undisturbed region in flood plain and the boundary region. in the undisturbed regions, the distribution of longitudinal velocity along the depth has the feature of lograithmic. whereas, in the interactive region, the longitudinal velocity does not obey the logarithmic distribution law, but it can expressed as a revised logarithmic function by using a wake function. on the basis of the kinematic equation the velocity distribution of transverse velocity is obtained. in the boundary region, the longitudinal velocity obeys the law of parabolic distribution. furthermore, according to the simplified diffusion equation, the transverse distribution of sediment concentration in the interactive region is deduced. the analysis is in good agreement with the measured data

    本文根據漫灘水流的運動特點,將漫灘水流的復式分為主槽平衡區、灘槽交互區、灘地平衡區及邊壁區等4個區,並給出了各區寬度的經驗公式.根據灘槽交互區垂線流速分佈的變化特點,提出了附加尾流函數的對數流速分佈公式.在簡化水流運動方程和泥擴散方程的基礎上,對灘槽交互區內垂線平均流速及沿橫向分佈進行了理論分析,提出了反映灘槽水流動交換強度的橫向渦粘性系數及橫向擴散系數的表達式,得到了漫灘水流垂線平均流速及沿橫向分佈的解析解,並與實資料吻合較好
  3. The comparison between the experimental data with numerical simulation show that the model have a higher precision in the lateral scouring and sedimentation deformation, time interval quantity of deposition, and output sediment concentration process during sand peak at various cross section and is applied fairly good to practical engineering

    青銅峽水庫的實資料對模型驗證結果表明:模型在水庫不同橫向沖淤變形、時段淤積峰期出庫過程都具有較高的精度,能較好地運用於工程實際。
  4. How to calculate section average silt content with adcp measuring

    流條件下平均計算
分享友人