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主題 : 全國優秀博士論文:復式河槽水流阻力及泥沙輸移特性研究
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樓主  發表于: 2009-10-10   

全國優秀博士論文:復式河槽水流阻力及泥沙輸移特性研究

作者姓名:楊克君 OC34@YUj[  
  論文題目:復式河槽水流阻力及泥沙輸移特性研究 meey5}  
  作者簡介:楊克君,男,1973年7月出生,2003年9月師從于四川大學曹叔尤教授,于2006年6月獲博士學位。 R?MRRq  
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  中文摘要 U l8G R  
  由沖積河流主槽和河漫灘組成的復式河槽在調節洪水、削減洪峰、貯存泥沙等方面不同于單一河槽。復式河槽隨著流量增大、水位抬高,當水位超過灘地高程時洪水漫灘,產生水流結構、水流阻力、泥沙輸移和河床演變的一系列復雜變化。研究復式河槽水流泥沙的復雜行為可以豐富和完善水力學、泥沙運動力學和河床演變學的研究內容,有重要的學術意義。其成果對防洪工程、航道整治、城市生態水利建設及河灘地合理開發利用等國民經濟和社會發展中的重要問題,有著廣闊的應用情景。本文系統地研究與探討了復式河槽水流阻力、動量交換機理、過流能力、植被作用下的復式河槽水流特性以及全動床復式河槽水流阻力及泥沙輸移特性。其主要研究內容為: go >*n\  
  1.復式河槽水流阻力研究 5x856RQ'  
  (1) 復式河槽阻力系數研究。分析與討論了曼寧系數和達西-韋斯巴赫阻力系數。通過分析英國科學工程研究協會洪水水槽設施 (SERC-FCF) 的大量的試驗資料,建立了綜合阻力系數、局部阻力系數和斷面形態、床面粗糙度之間的關系,并指出單一河槽法與斷面分割法不能準確估算復式河槽過流能力,其原因在于前者沒有考慮阻力系數隨水深的變化特性,而后者忽略了因灘槽動量交換而產生的附加阻力。分析表明,復式河槽阻力系數是雷諾數的復雜函數,但這種函數關系與單一河槽是不同的。 cCx@VT`0  
  (2) 復式河槽綜合糙率計算方法比較與分析。系統地總結了推求復式河槽綜合糙率的各種典型方法。根據是否考慮動量交換及所需的斷面幾何參數,綜合糙率計算方法可以簡單地分為若干類。運用大量的復式河槽水槽試驗資料和野外實測資料,驗證了上述各類方法的有效性,并討論了斷面分割類型對綜合糙率計算的影響。推求復式河槽綜合糙率時,每類方法都將帶來一定的誤差。在各類方法中,Lotter方法類與斷面分割類型密切相關,而 Einstein-Banks方法類與斷面分割類型無關。通過對各類方法比較和分析,發現這些方法估算復式河槽綜合糙率誤差大,并對這些方法產生誤差的原因進行了分析。 p}H:t24Cr5  
  2.復式河槽動量交換機理研究 {9?++G"\  
  (1) 復式河槽動能損失強度分析。為了反映動能損失的強度,針對恒定、均勻、紊動水流,提出了橫向動能校正系數和動能損失率的概念。通過分析復式河槽動能損失的機理發現,復式河槽橫向動能校正系數大于1和動能損失率大于0。通過分析英國SERC-FCF系列試驗成果發現,橫向動能校正系數和動能損失率與復式斷面形態有關。動能損失強度隨著主槽邊坡系數的增大而減弱,隨著灘槽寬度比的增大而增強。對稱復式河槽的動能損失強度大于非對稱的復式河槽。對于所有斷面形態,動能損失強度先隨相對水深的增加而增強,后又隨著的相對水深的增加而減弱,最終表現出單一河槽的特性。 qaJ$0,]H+  
  (2) 復式河槽動量輸運系數研究。從Boussinesq假定出發,并結合灘槽交互區流速分布特點,導出復式河槽動量輸運系數的表達式;接著根據力的平衡,導出垂向表觀剪切應力的表達式;運用SERC-FCF大量的水槽實驗成果,分析了動量輸運系數隨相對水深及灘槽寬度比的變化關系;最后根據獲得的動量輸運系數關系,利用劉沛清方法計算復式河槽過流能力。計算結果表明:本文中的動量輸送系數隨相對水深及灘槽寬度比的變化關系是可行的。 aT|SKb`  
  3.復式河槽過流能力研究 *nS}1(u]  
  (1) 復式河槽過流能力計算方法比較與分析。系統地總結了復式河槽流量計算的各種方法,運用這些方法分別計算整個復式斷面的流量和灘槽流量分配,并利用SERC-FCF水槽實驗成果加以比較。通過比較發現:計算流量時,斷面垂直分割法、單一河槽法和等速剖分法誤差都很大;而其它方法精度都比較高,精度由高到低依次為COHM方法、SKM方法、斷面傾斜分割法類型 1 (IDMT1)、動量傳遞法 (MTM)、謝漢祥法 (XHXM)、斷面疊加法 (SCSM)、童漢毅法 (THYM)。同時,運用流量計算精度比較高的方法計算流量分配。具體對某一斷面形態而言,很難準確說哪種方法的精度最高,但綜合所有系列總體而言,SKM方法最佳,其次是IDMT1和THYM,再次是COHM、MTM、XHXM,最后是SCSM。本文還分析了二次流對過流能力、流量分配及水流阻力的影響。二次流對過流能力的影響不大,但它對流量分配、垂線平均流速及床面剪切應力的橫向分布、灘槽斷面平均流速、灘槽床面平均剪切應力的影響卻十分明顯。通過對各種方法優劣地詳細分析,建議:在計算天然復式河槽過流能力時,COHM方法是一種值得推薦的好方法。 ASGV3r (  
  (2) 復式河槽過流能力的系統動力學模型研究。通過分析SERC-FCF水槽實驗成果,發現灘槽 Darcy-Weisbach阻力系數比值隨著相對水深的增加而減小。主槽阻力系數隨著相對水深的變化而變化,呈拋物線分布。根據獲得的阻力系數關系,運用系統動力學方法,建立了洪水漫灘后,復式河槽過流能力的系統動力學模型。計算結果表明:該模型能確定水位流量關系,其模擬值與實測值吻合較好。 pRR1k?  
  4.植被作用下的復式河槽水流特性研究 p G|-<6WY  
  通過水槽試驗,探討了不同灘地植物 (喬木、灌木和野草) 對復式河槽流速分布的影響。試驗時,選塑料吸管、鴨毛和塑料大草分別模擬喬木、灌木和野草。同時,考慮了流量、床面底坡對流速分布的影響。試驗結果表明,灘地未種樹的復式河槽在大的相對水深時,流速滿足對數分布;灘地種樹后,主槽流速增大,流速分布復雜,灘地流速減小,呈 S 形分布,不同植物的S 形分布是有差別的。這種S 型分布將水流劃分為三區的復雜行為,每區的范圍與水深、垂線位置和植物類型有關。床面坡度對流速分布的影響非常明顯?v向、橫向和垂向三個方向的脈動流速基本上滿足正態分布;時均流速與采樣時間的長短有關;橫向動量交換比垂向動量交換強,橫向動量基本上是主槽向灘地傳遞;不同的灘地植物對水流紊動強度的影響是不同的。灘地種植植物后,水流的紊動強度增強,縱向和垂向的紊動強度相當,都服從S型分布。灘地種植植物前后雷諾應力的空間分布差異很大,不同的灘地植物對雷諾應力的空間分布十分明顯。在主槽邊坡區,雷諾應力變化復雜。由于受植物的影響,tyx 與tzx 基本上都為負,明顯不同于灘地未種植植物的情況。 wHx@&Tp  
  5.全動床復式河槽水流阻力及泥沙輸移特性研究 ]hE%Tk-  
  通過全動床復式河槽水槽試驗,探討了河道完全粗化后能量損失、阻力系數的沿程變化,推移質輸沙率的變化特性,床沙中值粒徑的橫向變化與沿程變化等,并探討了運用仙農熵的概念對泥沙相關特性的模擬。試驗結果表明,對于沖積河流,如果以水面坡度代替能坡,是會產生誤差的。阻力系數與能坡的沿程變化趨勢是相似的,而這種沿程變化趨勢又與床沙代表粒徑變化趨勢總體相一致。河道急劇展寬發生在清水作用初期,而且作用時間很短。在特定的試驗條件下,全動床復式河槽灘岸侵蝕速率在空間上變化趨勢為,越往下游,同流量下的灘岸侵蝕速度越小。與初始河道相比,主槽床面沿程始終處于淤積狀態,而主槽兩側均處于沖刷狀態。沖刷或淤積面積均有沿程減小的趨勢,這與流速總體沿程減小相一致。盡管初始斷面是對稱的,床沙初始級配是相同的,但主槽兩側斷面沖刷面積并不相等。運用仙農熵的概念與理論,推導了清水作用下粗化過程中推移質輸沙率公式。無論是輸沙率單調遞增段還是單調遞減段,推移質輸沙率公式都具有相同的表達形式。據此,導出了隨機變量X表達式的一般形式,并從理論上分析了參數ki的取值與曲線 凹凸的關系。若曲線上凹,ki取負值;反之,若曲線上凸,ki取正值。無論是歸槽水流還是漫灘水流,推移質中值粒徑均有先隨時間大幅度增大的趨勢,后隨著時間的增加中值粒徑增加的幅度減小,最終將趨于某一恒定的值。這種變化特性可用X一般形式的表達式進行預測。全動床復式河槽推移質運動不僅存在縱向的沿程分選,還存在橫向的沿斷面分選。 6sceymq  
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  關鍵詞:復式河槽;水流阻力;動量交換;過流能力;植被;泥沙輸移 #h=pU/R  
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關鍵詞: 博士論文
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沙發  發表于: 2009-10-10   
Flow resistance and sediment transport in compound channels ]g] ]\hS  
Yang Kejun xg(* j[ff3  
ABSTRACT g9~QNA  
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A compound channel comprising the main channel and floodplains exists in natural rivers widely, especially in alluvial streams. It differs from a single channel in adjusting flood, cutting flood peak, transporting sediment etc. When water in the main channel flows in an out-of-bank condition and on to the adjoining floodplain, owing to abrupt change of the shape of cross section and heterogeneous boundary roughness, there are a bank of vertical vortices along the vertical interface between the main channel and its floodplain, which will result in complex variations in flow structure, flow resistance, sediment transport and fluvial processes. The study of the complex behavior of flow movement and sediment transport in compound channels is profoundly important for the basic theory of hydraulics, mechanics of sediment transport and river dynamics. The research results benefit to flood control, channel training, floodplain exploitation etc. The thesis will systematacially investigates flow resistance, mechanism of momentum transfer, conveyance capacity in non-vegetated compound channels, flow structure in a compound channels with vegetated floodplains, flow resistance and sediment transport in a self-formed one. The main contents of the thesis are as follows: kR0/jEz C  
1. Flow resistance in compound channels c`Q#4e]%_  
(1) To study resistance coefficients in compound channels. This thesis analyzes and discusses the effect of cross-sectional shape on Manning’s and Darcy-Weisbach resistance coefficients. By analyzing the experimental data from Science and Engineering Research Council Flood Channel Facility (SERC-FCF), the relationships between overall, zonal, local resistance coefficients and a wide range of geometries and different roughness between the main channels and its associated floodplains have been established. Moreover, the reason why the conventional methods can not assess the conveyance capacity of compound channels is analyzed. The reason is that single channel method doesn’t consider the fact the composite roughness varies with flow depth and cross-sectional division method ignores the extra resistance produced due to the momentum transfer between the main channel and floodplains, in assessing the conveyance capacity in compound channels. According to the experimental results of SERC-FCF, it is shown that the overall Darcy-Weisbach coefficient for a compound channel is the function of Reynolds number, but the function relationship is different from that for a single channel. tl6x@%\  
(2) To compare and analyze the method for predicting composite roughness in compound channels. This thesis systematically sums up all kinds of different representative methods for predicting composite roughness. According to the hydraulic parameter required and whether the momentum transfer is considered or not, they can be simply classified into several groups. A vast number of experimental data and field data for compound channels are applied to check the validity of the mentioned methods. Meanwhile, the effect of the division type of cross section on the computation of composite roughness is analyzed. Any method for predicting composite roughness will result in error. Among them, Lotter method is closely related to the division type of cross section, while Einstein-Banks method is not related to that. By comparing and analyzing the above methods, it is pointed out the methods are not fit to assess the composite roughness in compound channels. The reasons why the methods result in errors are analyzed. D4OJin^}  
2. Mechanism of momentum transfer in compound channels 6N\f>c  
(1) To undertake the analysis of kinetic energy loss intensity in compound channels. The intense momentum transfer on the vertical interface between the main channel and floodplains in a compound channel, makes its conveyance capacity decrease. To reflect the kinetic energy loss intensity in a compound channel, two new concepts, transverse kinetic energy correction coefficient (TKECC) and kinetic energy loss rate (KELR) are put forward for steady, uniform and turbulent flow in the thesis. By the analysis of the mechanism of kinetic energy loss in compound channels, a conclusion is drawn that TKECC is larger than 1 and KELR is larger than 0 in compound channels. By analyzing the experimental data from SERC-FCF, it is found that TKECC and KELR are both related to shapes of cross section. Kinetic energy loss becomes weaker with main channel side slope factor increasing and becomes stronger with the ratio of main channel and floodplain widths increasing. Kinetic energy loss in a symmetric compound channel is stronger than that in an asymmetric one. For all the shapes of cross section, kinetic energy loss increases with the relative depth increasing. After it reaches the largest value, it decreases with the relative depth increasing, and the compound channel ultimately shows a characteristic of single channels. 1[] 9EJ  
(2) To investigate momentum transfer coefficient in compound channels. Momentum transfer coefficient plays an important role in computing conveyance, apparent shear stress on the vertical interface between the main channel and floodplain, mean boundary shear stress on floodplains or in the main channel respectively. In this thesis, beginning with Boussinesq’s assumption and combining the characteristics of velocity distribution in the interacting region, the expression of momentum transfer coefficient is derived theoretically; on the basis of force balance, the expression of vertical apparent shear stress is obtained; applying experimental data from SERC-FCF, the variation of momentum transfer coefficient with relative depth and the ratio of floodplain and main channel width, is analyzed; basing on the momentum transfer coefficient relationship obtained and applying Liu Peiqing method, the conveyance capacity in compound channel is calculated. The computed results show the momentum transfer coefficient relationship obtained is viable. f7_V ]  
3. Conveyance capacity in compound channels %/n#{;c#  
(1) To compare and analyze the method for predicting the conveyance capacity in compound channels. For a compound channel, when water in a main channel flows in an overbank manner and inundates its floodplains, if the conveyance capacity is directly calculated by Manning equation, it results in a deal of error. All kind of methods for predicting discharge are systemically summarized in this thesis and are applied to compute the cross-sectional discharge and the distribution of discharge in the main channel and floodplains, respectively. By comparing with different series of experimental data from SERC-FCF, it is found that the discharge error is large by cross-sectional vertical division method (VDM), single channel method (SCM) and equivalent velocity division method (EVDM). Otherwise, the calculation accuracy is high by the other methods. According to the order from high accuracy to low, the methods are,in turn, channel coherence method (COHM), Shiono and Knight method (SKM), inclined division method type 1 (IDMT1), momentum transfer method (MTM), Xie Hanxiang method (XHXM), superposing cross section method (SCSM), Tong Hanyi Method. In the meantime, the methods with high-calculation accuracy are used to calculate the discharge distribution. It is found that for certain given cross section, it is difficult to determine which method has the highest discharge distribution’s accuracy, but for all the series, as a whole, the highest is SKM, the next is IDMT1 and THYM, and the rest is COHM,MTM,XHXM and SCSM. In addition, the thesis analyses the effect of secondary flow on conveyance capacity, discharge distribution and flow resistance. The results show that it has a very small influence on conveyance capacity, but it does distinct influences on discharge distribution, lateral distributions of depth mean velocity and boundary shear stress, the mean velocities and boundary shear stresses of main channel and floodplains, respectively. By analyzing the merit and demerit of the above mentioned methods, it is pointed out that COHM is a good method in calculating discharge.   亚洲国产精品va在线观看麻豆