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文章通过对高地下水位灌溉渠道滑塌破坏成因的分析,提出了滤透式刚柔耦合衬护技术,该衬护结构具有固坡、护渠、导渗、排水的多重功能。 相似文献
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位于高地下水位区的渠道衬砌结构抗冻胀设计较为复杂,以喀什河下游灌区改造工程为例,对其渠道衬砌结构抗冻胀设计进行了数值模拟分析,得出本工程渠道衬砌结构的稳定性及冻胀变形、法向与切向冻胀力的分布规律与冻害规律,并为工程渠道抗冻胀提供了理论指导。 相似文献
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针对刚性衬砌渠道冻胀破坏问题,选取宁夏盐环定扬黄灌区衬砌渠道为研究对象,在考虑相变及水分迁移模型基础上,考虑高地下水位对冻胀的影响,建立考虑水分迁移及地下水影响的数学物理模型,并采用Comsol Mutiphysics有限元软件对梯形渠道混凝土衬砌进行冻胀数值模拟,分别从温度场、位移场和应力场对刚性衬砌渠道冻胀破坏等方面进行了研究分析。结果表明:阴坡、阳坡冻胀量较大,渠底较小,渠底中部、渠坡1/3坡板长度处冻胀量分别达到最大值。渠底中部的法向冻胀力较小,两边逐渐增大,阴坡、阳坡的法向冻胀力分布均匀;渠底的切向冻结力成线性分布。阴坡、阳坡靠近坡脚处切向冻结力较大,左、右两端坡顶处切向冻结力较小,渠底衬砌板和两侧衬砌板属于压弯组合变形构件。 相似文献
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考虑冻土与结构相互作用的梯形渠道冻胀破坏弹性地基梁模型 总被引:9,自引:0,他引:9
假定渠基冻土为服从Winkler假设的弹性地基,提出一种针对开放系统混凝土梯形渠道的衬砌冻胀力分布计算方法。基于弹性地基梁理论引入与冻胀变形成比例的附加项来反映衬砌冻胀变形引起的冻胀力释放和削减,导出考虑冻土与衬砌结构耦合作用的冻土地基梁挠曲线微分方程。基于此,对现浇混凝土梯形渠道底板和坡板分别建立冻胀模型,并结合边界条件对方程求解获得渠道底板和坡板挠度和内力的解析表达式,进而建立了基于衬砌冻胀位移计算的渠道衬砌冻胀破坏判断准则。以新疆塔里木灌区某梯形渠道为原型,对衬砌各点冻胀位移进行了计算,并与材料力学方法的计算结果及原型观测值进行了对比分析。结果表明,本文方法由于考虑了衬砌冻胀变形引起的冻胀力释放和削减,冻胀位移计算结果均较材料力学方法小,且与观测值更加符合。研究结果可为现浇混凝土梯形渠道的抗冻胀设计提供参考和理论依据。 相似文献
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寒区衬砌渠道输水能力下降主要是由常年冻融作用下衬砌结构发生冻胀破坏所致,针对渠道衬砌结构冻胀破坏问题提出渠坡板纵向设缝的抗冻措施与数值分析方法。本文通过将渠道衬砌板与冻土视为整体处理的方法构建混凝土衬砌渠道热力耦合冻胀模型,以甘肃省景泰灌区某混凝土衬砌渠道为研究对象,考虑不同设缝措施与纵缝填充的接触本构对3种工况进行抗冻影响因素分析。结果表明:渠底深部基本不受渠道整体几何边界的影响,但渠道边界尺寸和基土热流分布均对基土上部温度场变化具有显著影响。渠道阴坡、渠底和阳坡最大冻深分别为86.3、67.5、58.2 cm。通过合理设缝措施可使渠道阴坡法向冻胀力降低40.7%、底板冻胀量减小63.5%、切向冻胀力降低43.8%,使渠道断面冻胀分布趋于均匀,且模型分析与实测结果相符,表明本文构建模型的合理性。研究结果可为长距离输水渠道数值计算提供理论依据。 相似文献
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针对弧底梯形断面渠道,考虑复合土工膜和渠基土壤的摩擦力,通过分析复合衬砌渠道的冻胀破坏机理,指出弧底梯形复合衬砌渠道坡板可简化为在冻胀力、冻结力、摩擦力共同作用下的悬臂梁,整个衬砌体属于压弯组合变形结构。通过适当的假设和简化,建立了弧底梯形复合衬砌渠道冻胀破坏力学模型,分别求出渠道坡板和弧形底板内力表达式,并对衬砌板的厚度进行验算。对比混凝土渠道,加入复合土工膜后,衬砌体产生允许范围内的冻胀位移量,使渠基土壤对衬砌体的有效冻胀力和有效冻结力减小,改善了衬砌体本身的受力状态,起到防冻胀破坏的作用,揭示了复合衬砌渠道防冻胀破坏的机理;对比梯形渠道,认为弧底梯形渠道坡板与底板整体结构性更强,反拱作用明显,更有利于渠道的防冻胀破坏。 相似文献
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《中国水能及电气化》2017,(2)
在我国冻土地区,混凝土衬砌渠道冻胀破坏损害严重影响渠道稳定性,造成水资源浪费,缩短渠道的使用寿命,制约工程效益的发挥。本文对影响渠道冻胀的因素进行了分析,采用有限元软件ADINA,对不同设缝的混凝土衬砌渠道进行冻胀过程的数值模拟研究,并对应力场、变形场进行分析,进而探究衬砌板的冻胀变形及冻胀力分布,为工程实际应用提供参考。 相似文献
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为对比分析不同材料U形渠道对其抗冻胀效果的影响,采用有限元分析软件ADINA以衬砌板为研究对象进行仿真模拟分析。结果表明,玻璃钢渠道阴、阳坡最大冻胀变形比混凝土大27.44%、27.34%,但冻胀变形变化率减小了4.49%~16.19%,冻胀变形均匀;玻璃钢渠道有很强的适应变形能力,使衬砌板的等效应力、法向冻胀力分别减小了43.86%、39.96%,很大程度上减小了渠道的冻胀破坏,值得实践并推广。 相似文献
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David Watson 《河流研究与利用》1987,1(3):211-227
The effects of large aquatic plants (aquatic macrophytes) have been given limited attention in literature dealing with open channel flow. This is despite a large number of river channels in the U.K. being affected by profuse growths of these plants. This paper contributes to three major areas in relation to aquatic macrophytes and river channels. First, a literature review examines four areas of vegetated channel research. Early work on vegetated channels concentrated upon grass-lined farm drainage channels in the U.S.A. This was complemented by flume studies of predominantly artificial vegetative roughness elements. The review discusses research into large aquatic plants in stream channels, and the discussion draws together a number of disparate areas of research into vegetated channels including theoretical considerations. Secondly, the paper discusses results obtained from laboratory flume experiments, using real plants, and field monitoring on the River Ebble, Wiltshire, U.K. The relationship between discharge and Manning's roughness coefficient (n) is examined. Field monitoring results are presented as generalizations in the relationship between Manning's n when the monitoring sites were vegetated and unvegetated. The relationship between plant cover in the channel and Manning's n is also examined. Two measurements of plant cover are employed: the percentage cross-sectional area of channel vegetated, and biomass per unit area. The field data for Manning's n and discharge are then discussed in detail in a case study of one site on the River Ebble. Finally, the results obtained from field monitoring are compared to previous research. In the light of these comparisons and detailed examination of the field and flume data, a conceptual model of the effects of aquatic plant growth on channel roughness, mean flow depth, and flow stage is represented. Using this model, an estimate can be made of the likely effect of changing plant cover and discharge on flow stage in an open channel. 相似文献
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新疆灌区灌溉水利用系数影响因素研究 总被引:2,自引:0,他引:2
新疆地区各灌区灌溉水利用系数的影响因素有灌区渠系防渗长度、高效节水灌溉面积、井灌排面积、渠道建设长度、总灌溉面积、渠道防渗率等.基于柯布-道格拉斯模型方法,分析计算了各灌区主要因素对灌溉水利用系数的影响效应,并对其发展预期进行了评估.结果表明:节水灌溉面积、渠道防渗长度和井灌排面积三个生产要素,对新疆绝大多数灌区灌溉水利用系数产生正效应,即边际收益大于边际投入;新疆2015年、2020年规划灌溉水利用系数分别为0.520和0.570,已超过国家大型灌区灌溉水利用系数不应低于0.50的要求. 相似文献
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DISCHARGE DISTRIBUTION IN STRAIGHT COMPOUND CHANNELS 总被引:6,自引:3,他引:3
Wang Wei Cai Jin-de Xu Wei-linState Key Hydraulics Lab. of High Speed Flaws Sichuan Union University Chengdu P. R.China 《水动力学研究与进展(B辑)》1998,(4)
The existing methods of computing the flow distribution in compound channels with flood plains have been summarized in this paper. Due to the lower precision of hydraulic computation for a compound cross-section with two flood plains, a new method called the momentum-exchange method herein, is presented and verified with experimental and field data. The results show that the new method is more effective than the previous ones. 相似文献
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采用有限体积法对SKM模型控制方程进行离散,使其可以应用于任意断面形状的天然河道水力要素计算。通过自编程序,将该数值模拟方法应用于长江朱沱水文站和英国特伦特河Yoxall水文站断面深度平均流速及水位流量关系计算,所得数值解与实测结果吻合良好。实例应用结果表明,采用该数值模拟方法可以有效地解决SKM模型在天然河道中的应用难题,其在河道过流能力、水位等方面预测合理可行,具有实际应用价值。 相似文献
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Reduced streamflow via flow diversion has the potential to limit the sediment‐transport capacity of downstream channels and lead to accumulation of fine sediments and habitat degradation. To investigate, we examined the effects of variable levels of flow diversion on fine‐sediment deposition, hydraulic conditions and geomorphic alteration. Our study consisted of a detailed field analysis pairing reaches above and below diversion dams on 13 mountain streams in north‐central Colorado and southern Wyoming USA. Diversions are ubiquitous across the American West, yet previous comparative studies on the effects of flow diversion have yielded mixed results. Through application of strict site‐selection criteria, multiple fine‐sediment measures, and an intensive sampling scheme, this study found that channels downstream of diversions contained significantly more fine sediment and slow‐flowing habitat as compared to upstream control reaches. Susceptibility to fine‐sediment accumulation was associated with decreasing basin size, decreasing bankfull depth and smaller d84, and it appears to be magnified in streams of less than 3% slope. Copyright © 2010 John Wiley & Sons, Ltd. 相似文献
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运用大涡模拟计算了两个非对称复式断面明渠内的水流运动和污染物扩散,其中由亚格子尺度涡运动引起的亚格子应力与物质扩散通过Smagorinsky-Lilly亚网格模型模拟。预测结果与Shiono等使用激光多普勒流速计(LDA)和激光诱导荧光技术(LIF)测量的实验数据进行了对比,计算得到的流场结构和污染物浓度分布均较好地吻合于测量结果。成功地再现了在其中一个复式断面明渠中观测到的横向浓度分布呈现显著双峰值的现象,根据计算的流场得出复式断面明渠中流向交替变化的强烈横向流动是产生这种现象的主要原因。 相似文献