马蹄形过水断面正常水深计算的遗传算法

马蹄形过水断面是无压输水隧洞中常采用的断面形式之一 ,因其几何形状复杂 ,水力计算困难。目前常采用的方法有试算法、图解法和迭代法 ,这些方法由于计算量大且精度不易保证 ,不便于在生产实践中应用推广。将马蹄形过水断面正常水深计算转化为非线性优化问题 ,采用实数编码的遗传算法进行求解 ,实例计算表明该方法精度高、通用性强、操作简便 ,便于在生产实践中应用。     

含刚性沉水植物明渠水流结构的试验研究

【目的】得到含刚性沉水植物明渠的水流结构。【方法】采用粒子图像测速仪(PIV),用有机玻璃棒模拟刚性植物,在不同来水流量、植物密度条件下对明渠水流结构进行了试验研究。【结果】无植物时平均流速沿垂向呈对数分布规律,有植物时则呈现明显的分区分布特性。无植物时紊动强度值沿垂向变化不大,有植物时在植物顶端位置处紊动最剧烈。流量或植物密度越大,植物顶端位置的流速梯度就越大,植物层上方的流速最大值也越大。植物密度越大,植物顶端位置的紊动强度越大,植物密度对水流紊动强度由最大值减小到最小值的区域影响很大。【结论】刚性沉水植物的存在会改变水流结构,增强紊动掺混,增强流体质点交换和能量传递,且上述影响会随着流量或植物密度的增大而增强。     

旱地果园起垄覆膜集雨措施对树体水分利用的影响

针对甘肃陇东黄土高原旱地苹果园季节性干旱问题,以15年生长富2号苹果树为试材,研究果园起垄覆膜、小沟集雨技术措施对土壤水分、主干液流速率、叶片光合速率等的影响。结果表明,在萌芽前晴天,覆黑地膜能显著提高主干液流速率;在果树生长季节,覆黑地膜能降低株间蒸发量,较长时间保持土壤水分,提高水分利用效率和叶片光合能力,同时可以...     

悬板分层水流流动特性的测试研究

随着悬板分层式引水枢纽工程近年逐步被推广应用,对其水流特性及输沙机理的研究也越来越受到人们的重视。本研究利用激光测速仪首次对悬板分层水流流场特性进行了测试,并分析了其对输沙过程的影响     

YTG型双向体积管在计量检定中的应用

体积管是检定流量计的标准器。ＹＴＧ型双向体积管,其外型尺寸、主体结构、检定速度、日常管理等方面,均比单向体积管有明显的优点,并具有独特的容积补偿性,给体积管的管理、使用带来极大方便。介绍了ＹＴＧ型双向体积管的结构、技术指标及其优越性,并建议在条件允许的情况下,尽可能使用双向体积管。     

某高铁隧道小口径井抽水试验探讨

指出了在某高铁隧道勘察中采用小口径抽水试验方法,具有操作简单便捷,成本低的优势。通过小口径井抽水试验查明场地的水文地质条件,得出了水文地质原始数据资料,根据单孔稳定流承压水非完整井的水文地质实际情况,选取合适的公式分别计算出了隧道岩层渗透系数及影响半径,为高铁隧道的勘察设计及顺利施工提供参考。     

王氏唇柱苣苔的离体培养及遗传稳定性

以王氏唇柱苣苔(Chirita wangiana)叶片为外植体进行组培离体快繁研究,并利用流式细胞术对组培苗进行遗传稳定性分析。结果表明:最佳初代诱导培养基为MS添加0.5 mg/L 6-BA+0.1 mg/L NAA;最适继代培养基为MS添加0.5 mg/L 6-BA+0.05 mg/L NAA;最适生根培养基为1/2 MS培养基添加0.5 mg/L IBA和15 g/L蔗糖,所有生根培养基获得的组培苗移栽驯化成活率达到92%以上。组织学切片检测表明,王氏唇柱苣苔叶片为外植体所形成芽体均为器官发生方式形成。流式细胞术检测表明,组培苗倍性没有变化,基因组大小与母本相比仅发生了1.86%的减少;染色体数目为2n=36,跟母本一致,植株形态特征上也无变异。研究结果可为王氏唇柱苣苔的园艺应用快速提供大量遗传稳定的种苗。     

Dynamics in debris-flow activity on a forested cone — A case study using different dendroecological approaches

Dendrogeomorphological analyses of trees affected by debris flows have regularly been used to date past events. However, this method has always been limited to forested cones where trees registered the impact of previous events. The minimum age dating of trees growing in the debris deposits can, in contrast, provide information on the latest possible moment of past activity. In this paper, we report on results obtained from a combination of these two approaches on a forested cone in the Valais Alps (Switzerland). A detailed geomorphic map in a scale of 1:1000 served as a basis for the sampling strategy. Disturbed Larix decidua Mill. and Picea abies (L.) Karst. trees growing in the deposits allowed reconstruction of 49 events between AD 1782 and 2005 as well as the determination of the spatial extent of events. In the debris-flow channels where survivor trees are missing, we selected the oldest post-event trees and assessed their age by counting their growth rings. Missing rings due to lack of center as well as to sampling height were added so as to determine real tree age. The combination of the dendrogeomorphological event reconstruction with the assessment of germination dates of successor trees allowed realistic approximation of the minimum time elapsed since the last debris-flow activity in 23 of the 29 channels present on the current-day cone surface. In general, channels in the northern part of the cone and those close to the currently active channel generally show signs of (sub-) recent activity with one last overbank sedimentation event in the 1980s, whereas signs of debris-flow activity are absent from the channels in the outermost part since the late 19th century. As a consequence of the deeply incised channel and the stabilization measures undertaken along the banks, signs of debris flows are missing in the tree-ring record for the past two decades.