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双语推荐:泥沙粒径

泥沙粒径泥沙运动力学研究中的一个重要物理量,不同的代表粒径泥沙输移运动的计算结果会产生不同的影响。文章对比了中值粒径和平均粒径的不同,分析了泥沙粒径和均匀性对冲刷深度的影响,结合铁路工程中常用的桥墩局部冲刷计算公式,对比分析了不同代表粒径条件下的冲刷深度计算结果。提出了代表粒径的选用应结合公式制定时所依据基础资料,同时也要考虑泥沙均匀性的影响,提高计算结果的可靠性和精度。
The sediment grain size is an important physical parameter in studying the mechanics of sediment transport;different typical grain sizes will produce different effects to the calculation results of sediment transport. The paper com-pares the differences of medium and mean grain sizes, analyzes the effects of sediment grain size and uniformity on scour-ing depth. The calculation results of scouring depths of different typical grain sizes are analyzed based on the local bridge pier scour calculation formula commonly used in railway projects. To improve the reliability and accuracy of calculation results, both the selection of sediment grain size and the sediment uniformity influence are required to be considered.

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为研究泥沙粒径对分离鳃的速度场及水沙分离效果的影响,采用层流模型和欧拉模型,运用PC-SIMPLE算法,对分离鳃内的水沙两相流流场进行了三维数值模拟。计算结果表明:当泥沙粒径d=0.0001mm时,分离鳃内的流场与其他泥沙粒径时有所不同;当0.005mm≤d≤0.035mm时,分离鳃内不同粒径泥沙水流的流场相同;当0.015 mm≤d≤0.035 mm时,分离鳃处理泥沙效果最好,且泥沙粒径越大,去除率越高,水沙分离速度就越快。
Three-dimensional numerical simulation adopting the laminar model and Euler model were conducted to the flow field of water-sediment two-phase in gill-sheet separation device to study how the sediment grain size effects upon velocity field and water-sediment separation by using PC-SIMPLE algorithm. The results show that the velocity flow is the same in the gill-sheet separation device when sediment grain size ranges from 0.005 mm to 0.035 mm and when the it is different the sediment grain size is 0.000 1 mm. The best performance is observed when gill-sheet separation device handles sediment grain size that ranges from 0.015 mm to 0.035 mm. Additionally, the greater sediment grain size is, the higher removal is. Meanwhile the faster the water-sediment separation is.

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淤地坝是韭园沟与秃尾河流域重要的水土保持工程之一,淤地坝所处流域和工程结构的不同,淤积物的粒径大小存在差异。通过钻孔取样法采集了韭园沟流域21座淤地坝和秃尾河流域36座淤地坝淤积物样品623个,根据样品的颗分结果,分析得出韭园沟流域淤地坝坝内粗泥沙粒径主要为0.05 mm,秃尾河流域淤地坝坝内粗泥沙粒径主要分布于0.05~0.10 mm之间,说明淤地坝能有效拦截流域内的粗泥沙;两流域淤地坝均呈现库尾泥沙粒径总体大于坝前,库尾泥沙粒径的大小取决于入库泥沙粒径的大小,入库泥沙粒径越大,淤地坝对其分选效果越明显。
Warping dam is one of the important soil and water conservation projects in Jiuyuangou and Tuwei River watersheds. Because of the war-ping dam is different in watershed and engineering structure,the size of sediment in the dam is also different. Through drilling sampling method, it collected 623 samples in 21 warping dams in Jiuyuangou watershed and 36 warping dams in Tuwei River watershed. Analysis of sediment grain size distribution,the size of coarse sand in warping dams of Jiuyuangou watershed was 0. 05 mm,in warping dams of Tuwei River watershed was mainly 0. 05~0. 10 mm. The results show that the dam can effectively intercept the coarse sediment. The sand size of tail dam is larger than the front dam in the two watersheds. The sediment size of tail dam depends on the size of the sediment inflow the dam. The more coarse of the sedi-ments inflow the dam,the results of the separation effect are more obvious.

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根据滴灌实际运行情况,采用分段粒径浑水持续灌溉的试验方法,分析了泥沙颗粒粒径及进口压力对迷宫式流道滴头的流量、均匀度及堵塞的影响。结果表明:在粒径小于0.125 mm 的泥沙颗粒中,较小颗粒的制紊效应要大于较大颗粒的制紊效应,泥沙颗粒粒径及进口压力均是影响灌溉均匀度的因素;含沙量较低时(0.5 g/L),粒径是影响滴头堵塞的主要因素,在0.0308~0.125 mm 粒径范围内,粒径较小时更容易引起堵塞,进口压力不同时容易引起堵塞的敏感粒径范围不同,压力为0.15及0.105 MPa 时,敏感粒径为0.045~0.075 mm ,进口压力降至0.075 MPa后,敏感粒径为0.0308~0.045 mm ;连续灌溉条件下压力不是影响滴头堵塞的主要因素。
According to the actual situation of drip irrigation ,the influences of sediment size distribution and inlet pressure on irriga-tion uniformity ,flow and clogging of labyrinth-path emitters were investigated through the method of muddy water continued irriga-tion .The result showed that turbulence effects caused by smaller particles was more distinguished than bigger ones ;both sediment size distribution and inlet pressure were the factors that affected irrigation uniformity when the particle sized in muddy water were less than 0 .125 mm ;sediment particle size was the main factor of emitter clogging with low sediment concentrations ;emitter clog-ging would be caused more easily by smaller particles ;different inlet pressures correspond to different sensitive size that caused emit -ter clogging easily ;size sensitive is from 0 .045 to 0 .075 mm at the pressure 0 .150 and 0 .105 MPa ,while from 0 .030 8 to 0 .045 mm at the pressure 0 .075 ;inlet pressure was not the main facto

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为了研究黄河下游引黄灌区管道输水临界不淤流速的计算方法,在室内用U—PVC管道,以黄河泥沙为沙样,进行了90、110、125mm三种管径、两种泥沙颗粒级配条件下,不同含沙量浑水管道输水临界不淤流速试验。结果表明:试验条件下,在含沙量、管径相同时,浑水中泥沙粒径越大,临界不淤流速越大;在管径、泥沙粒径相同时,含沙量越大,临界不淤流速越大;在泥沙粒径、含沙量相同时,管径越大,临界不淤流速越小。依据试验成果,利用回归分析方法建立了黄河下游引黄灌区管道输水临界不淤流速计算公式。
A series of experiments on non-silting velocity of muddy water conveyance pipelines with different sediment concentration were carried out to study the calculation method of water conveyance pipelines of irrigation area in the Yellow River downstream. We used U-PVC pipe indoors with the Yellow River sediment as the sand sample and 90 mm,110 mm and 125 mm three pipe diameters and two sediment particle gradations. The results show that the bigger sediment particle in muddy water is,the greater non-silting velocity will be;the higher sediment concentration is, the greater the non-silting velocity will be under the same conditions of sediment concentration and pipe diameter. The bigger pipe diameter is,the smaller the non-silting velocity will be in case of the same sand sample. It has established the calculating formula of non-silting velocity of water conveyance pipelines in the Yellow River downstream irrigation area by using regression analysis on the basis of results.

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为探明泥沙粒径与含沙量对内镶片式斜齿形迷宫流道滴头的堵塞过程和原因,采用筛分法,分选出6个小于0.1 mm的粒径段,配制成不同含沙量的浑水,在恒压条件下,采用周期性间歇灌水试验观测流量变化,通过电镜扫描法观测堵塞泥沙结构。试验结果表明:粒径为0.075≤D0.1 mm和0.03≤D0.038 mm的泥沙易引起滴头堵塞;粒径为0.038≤D0.05和D0.02 mm的泥沙较难引起堵塞,且含沙量变化对堵塞的影响较小;粒径0.02≤D0.03 mm和0.05≤D0.075 mm的堵塞情况介于上述两者之间。当含沙量为1.2~1.3 g/L时,是最易引起堵塞的临界含沙量。当0.038≤D0.1 mm时,泥沙在流道内不易形成团聚体,造成滴头堵塞的原因是泥沙沉降、堆积;当D0.038 mm时,泥沙易在流道中凝结成大的团聚体,是造成滴头堵塞的主要原因。
Drip irrigation technology is widely used due to its advantages including high efficiency water saving, ability to adapt to the terrain and so on, but the problem of emitter clogging has been always a baffled to researchers. Emitter clogging basically has three classes, respectively is physical clogging, chemical clogging and biological clogging, of which the most common is physical clogging and it is represented by sediment clogging. Studies show that even if the irrigation water after precipitation filtration, there is still have particle size of sediment particles which are less than 0.1mm get into the emitters causing emitter clogging. However, previous studies on this problem multi-use of computer simulation method to research the influence of emitter anti-clogging by emitter structures, test verification is relatively rare and most studies only from a macro perspective to observe emitters clogging, no in-depth study on the clogging mechanism. In addition, the previous researches

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通过对泾惠渠灌区2013年夏秋灌期干支斗渠浑水资料的实时取样分析,探究渠灌区渠系挟沙水流含沙量及泥沙级配的时空变化规律,量化描述不同粒径悬移质泥沙颗粒的输移特征,旨在获得灌渠渠系内挟沙水流历经冲淤过程不同粒径悬沙沿程的垂向分布与输移规律,为渠灌区的运行及泥沙问题的处理提供理论基础。灌区内进行的原型取样测流工作在选定的具有代表性的干-支-斗渠线路上进行,观测分析了灌区渠系含沙量及不同粒径泥沙颗粒沿垂线分布的特征,验证分析了挟沙水流历经淤积过程含沙量分布的变化规律。通过对典型渠系线路不同粒径悬移质泥沙的沿程调整计算分析,表明不同粒径泥沙沿程的输移特征不同,各分组沙的冲淤特征并不都和全沙平均计算结果一致,其中级配曲线左端一定粒径范围(约>0.015 mm)的粗沙与全沙具有同冲同淤的规律。该研究可为泾惠渠灌区泥沙处理利用以及渠灌区浑水调控理论与技术的进一步研究提供依据。
Due to non-uniformity of precipitation distribution, irrigation plays an irreplaceable role in agriculture, and diversion channel is the main form in irrigation district. Water and sediment is always indivisible, so it’s always inevitable to divert water at the same time not to divert sediment into the irrigation system. In this paper, the transport characteristics of the suspended sediment in the irrigation canals in the irrigation system are mainly studied. Based on the field data sampled in Jinghuiqu irrigation district during the summer and autumn irrigation period in 2013, the temporal and spatial variation laws of sediment concentration and gradation of the suspended load will be researched and the transport characteristics of the suspended load of different size will be described quantitatively in order to provide basis for sediment treatment and the further research on the theory and technique on regulating the sediment in muddy flow in irrigation channels. The sampl

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为了掌握泥沙介质在水轮机转轮中的分布规律以及对转轮压力场的影响,该文应用固液两流体多相流动模型,充分考虑了固液两相间的相互作用,通过求解雷诺时均N-S方程和重正化群k-ε湍流方程,对不同泥沙介质条件下水轮机转轮通道中的流动进行数值研究。研究结果表明,含沙水会导致水轮机转轮叶片表面压力载荷增大,固液两相间速度差异是导致叶片表面泥沙体积浓度分布的变化的主要原因。小粒径泥沙在叶片表面分布均匀且体积浓度低,大粒径泥沙会集中分布在叶片的前缘及出水边等区域。该研究可为多泥沙电站水轮机转轮抗泥沙设计提供参考。
Sediment erosion of hydraulic turbine is the complicated engineering problem related to such factors as operating conditions of hydraulic turbine, solid-liquid two-phase flow characteristics and sediment properties. In this paper, the three dimensional full channel geometric model of prototype turbine is established to understand change in internal pressure of runner and sediment distribution in runner channel under different sediment flow conditions. The hydraulic turbine mainly consists of spiral case, vane, runner and draft tube. Every part generates its corresponding independent meshes, and then is connected with each other by internal interfaces. The total number of grid cell is 7 888 784 in computational domain. Considering solid-liquid interactions fully, based on Eulerian-Eulerian multiphase flow model, Reynolds-averaged Navier-Stokes and RNG k-ε turbulence equations are numerically solved to study internal flows of hydraulic turbine runner under different sediment f

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采用瓯江口实测泥沙资料,对多个典型挟沙力公式进行了系统比较;对瓯江口同步的平均流速和平均含沙量进行分析,探讨适合该河口的挟沙力关系,并引入泥沙因子,考虑泥沙粒径对水流挟沙力的影响。结果认为:各挟沙力公式的计算结果过程曲线趋势一致,只是存在量级上的差别;结合实测泥沙资料进行分析,采用河口、海岸适用性较好的水流挟沙力公式,考虑泥沙粒径对挟沙力的影响,引入泥沙因子分析拟合瓯江口水流挟沙力公式。旨在揭示不同挟沙力公式之间的联系,以及河口海域水流挟沙力拟合过程,为进一步探讨河口海岸含沙量分布和悬浮泥沙输运提供思路。
Using the sediment data in the Oujiang Estuary, the formulas of sediment-carrying capacity were sys-tematically compared. According to simultaneously averaged velocity and averaged suspended sediment concentra-tion, and also considering the sediment factor, the sediment-carrying capacity in the Oujiang Estuary is discussed. It’s concluded that the results of each formula trend to consistency, and there’s only difference of value in practice. Applying the more reasonable sediment-carrying formula, and considering the grain size of sediment, the formula at the Oujiang Estuary was analyzed and fitted.

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针对黄河内蒙古段河水高含沙问题,通过改变多级斜板水沙分离装置中的斜板间距,探讨了不同流量、不同浓度浑水下斜板间距对泥沙分离率的影响。结果表明:第一级和第二级分沙装置中斜板间距越小,水沙分离效果越好;第三级分离装置的斜板间距减小到2 mm时,其对提高水沙分离率的影响不明显,而且会导致泥沙淤积,不利于排沙。同时分析了不同流量下斜板间距对排沙孔分离出的泥沙中值粒径的影响,结果表明:在同一流量下,排沙孔泥沙颗粒粒径随斜板间距的增大而增大。
For the hyper-concentration flow of the Yellow River in Inner Mongolia,the paper discussed the effect of inclined plate spacing’ s on sediment separation rate in different discharge and concentration by changing the inclined plate spacing’s of multilevel water-sediment separation device. The results show that the smaller the inclined plate spacing is,the better the effect of the water-sediment separation is, in the first and second level water-sediment separator;when the inclined plate spacing of the third separator reduced to 2mm,the effect is not obvious and it is easy to cause sediment deposition disadvantage of desilting. Besides,the paper analyzed the effect of inclined plate spacing’s on sediment median sizes of sediment flushing outlet in different discharge. The results show that the sediment sizes of sediment flushing outlet is increased with the increase of the inclined plate spacing under the same discharge condition.

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