基于RBF神经网络的黄河含沙量测量数据融合研究

针对黄河含沙量高、泥沙时空分布不均和环境变化显著等特点,提出了采用电容式差压法来测量黄河含沙量,建立了基于RBF神经网络的含沙量测量的数学模型。将含沙量信息值与温度、深度和流速值作为RBF网络的输入,进行含沙量测量的反演和误差分析。试验结果表明,基于RBF的数据融合方法能够有效地消除环境影响,提高系统测量的精度和稳定性。     

窗口坝拦截泥石流性能试验研究

泥石流窗口坝是一种常见的泥石流防治工程措施,具有拦砂节流、护床固坡等重要调节功能。为了探寻泥石流的过坝特征,通过室内模拟试验,运用控制变量的方法对不同类型泥石流的过坝情况进行了探讨。试验发现,泥石流过坝前后颗粒组成的变化与泥石流密度相关性较大,在泥石流密度为1 650 kg/m³时,窗口坝对泥石流的筛选能力最强;泥石流过坝后密度降低情况较明显,并且受泥石流窗口坝闭塞类型的影响,不同闭塞类型下泥石流密度降低率具有相似规律,在泥石流密度为1 800 kg/m³左右时,泥石流密度降低率最大;通过回归分析得到了拦排比L与泥石流密度γ_c的关系式。     

最佳鳃片倾斜角下分离鳃内部流场的数值模拟

采用均匀试验设计理论对鳃片倾斜角α与β进行数值模拟方案的设计,通过采用Fluent软件中的欧拉模型,以鳃片3上表面的泥沙速度作为考核指标,对不同鳃片倾斜角下的分离鳃速度流场进行模拟。运用投影寻踪回归分析法(PPR)对数值计算结果进行了分析,得出鳃片β倾斜角对分离鳃水沙分离效果影响是最大的,其次是鳃片α倾斜角的影响;当鳃片倾斜角的组合为α=60°与β=45°时,分离鳃中的速度流场有利于水沙的快速分离且水沙分离效果最佳。     

Relationship between nutrient pollutants and suspended sediments in upper reaches of Yangtze River

In order to study the relationship between nutrient pollutants and suspended sediments(SS) in the upper reaches of the Yangtze River and two tributaries, water samples were collected from September 1, 2010 to September 30, 2011 at the Zhutuo, Cuntang, Beibei, Wulong, Qingxichang,Wanxian, and Fengjie cross-sections. In the laboratory, the SS concentration and the concentration of SS whose particle size was smaller than0.02 mm were measured. The phosphorus(P), nitrogen(N), and permanganate index(CODMn) concentrations in the natural water sample, the settled water sample, and two types of filtered water samples obtained through filter membranes with pore sizes of 0.02 mm and 0.45 mm were monitored synchronously. The results show that there are strong relationships between the P and CODMnconcentrations and the SS concentration. P mainly exists in particulate form, while N mainly exists in dissolved form. SS whose particle size is smaller than 0.02 mm accounts for a high proportion of sediments in the Yangtze River and has a strong effect on water quality. At the seven cross-sections, the amounts of P, N, and CODMnin particulate form in the wet season are higher than in the dry season and the adsorption amounts of P, N, and CODMnper unit mass of sediment are higher in the dry season than in the wet season.     

20世纪80年代以来珠江三角洲网河区河性演变

针对20世纪80年代以来珠江三角洲网河受大规模采沙影响,其河道特性发生的显著变化,基于实测资料,从网河区河道的河床演变、水沙条件、同流量水位变化、西江和北江分流分沙变化、河槽容积及河道行洪能力等方面分析了珠三角网河区河性的演变情况。结果表明:20世纪80年代以来,网河区河床下切严重,来流量变化不大,来沙量大幅下降,同流量下水位下降明显,思贤滘对西江、北江的分水分沙有所调整,河槽容积增大,河道的行洪能力提高。随着规模取沙的减少,2005年后网河区河道进入新的平衡演变阶段。     

Exploring Particle Density Effects on Partial Mobility of Steelhead Spawning Gravels

Yellowbank Creek is a small stream in coastal central California being assessed for salmonid habitat limiting factors and restoration potential. Yellowbank flows through low‐density marine mudstone bedrock, which is the gravel source for the stream. To assess the potential effects of the low‐density substrate on spawning gravels, a tracer stone study comparing the incipient motion of low‐density mudstone particles and typical density granitic particles was used to populate a logistic regression particle entrainment model. A model comparison approach was used to test the strength of the model. Results demonstrate partial mobility of both mudstone and granitic particles under boundary shear conditions ranging from 6.9 to 42.2 N m^‐2. The modelling results quantify the strong negative correlation between particle entrainment and particle density. Mudstone gravel was three times more likely to be entrained than granitic gravel, within the context of the experimental conditions. The effect of density difference on partial mobility was greater in smaller grain size fractions. This work has implications for salmonid spawning success in atypical geologic settings and may assist in prioritization of restoration efforts. Copyright © 2013 John Wiley & Sons, Ltd.     

Downstream Ecological Impacts of Controlled Sediment Flushing in an Alpine Valley River: A Case Study

Sediment flushing may be effective to tackle the loss of reservoir storage as a result of siltation. When operationally possible, the impact of this practice on the downstream aquatic environment can be mitigated by limiting the sediment concentration of the discharged waters (controlled sediment flushing). However, this topic is poorly documented, and concerns arise when limits are discussed. We present the results of a 3‐year field investigation concerning the controlled sediment flushing of a small reservoir on the Adda River, the main tributary of Lake Como—Italy. Two limits for suspended solid concentration (SSC) were adopted: 1.5 g L^?1, as average value throughout the whole working day, and 3.0 g L^?1, as alert threshold to adjust the ongoing activity. These constraints were essentially fulfilled in the course of the documented operations. The first year sediment flushing was more significant than the following year: 25 000 tons of fines below 2 mm in diameter were flushed in six non‐consecutive days in summer 2010, while, one year earlier, 75 000 tons were flushed in 16 non‐consecutive days. In the third year of investigation (2011), no sediment evacuation took place. The benthic macroinvertebrate and the fish communities were surveyed a short distance below the reservoir, that is, in the potentially more affected river reach. Clear pieces of evidence of environmental quality degradation were not detected; the adopted strategies can therefore be considered to be appropriate when planning sediment flushing management in comparable contexts. Copyright © 2014 John Wiley & Sons, Ltd.     

汉江上游干支流沉积物细菌群落多样性和影响因素

为了解汉江上游干支流沉积物细菌多样性以及确定性过程和随机性过程在沉积物细菌群落构建过程中的相对重要性,基于Illumina高通量测序技术,分析了环境因子对细菌群落组成的影响,采用非度量多维尺度(NMDS)排序探究了季节之间沉积物细菌群落的差异,并结合中性群落模型和标准化随机率量化了确定性过程和随机过程对群落构建的影响。结果表明：汉江上游及其支流细菌群落主要由变形菌门(Proteobacteria)、拟杆菌门(Bacteroidetes)、蓝藻门(Cyanophyta)、浮霉菌门(Planctomycetes)和酸杆菌门(Acidobacteria)等组成;细菌群落在不同季节有显著差异;地理距离和环境因子对细菌群落结构影响较小,确定性过程并未在细菌群落组成中起到主导作用;随机过程很大程度上影响了群落在秋季和春季的组成,是沉积物细菌群落构建的主导因素。     

鉴江干流水沙变化探讨

根据鉴江干流主要控制水文站化州、高州站及罗江主要控制水文站合江站的实测径流量和输沙量资料,用Mann-Kendall法、双累积曲线法及Pearson相关分析法等,阐析近20年鉴江不同时段、不同河段水沙变化情况。结果表明:自2010年实施《广东省鉴江流域水资源分配方案》后,径流量、输沙量呈减小或总体平稳趋势,且水沙关系相关密切。     

绿茶提取液沉淀形成机理的研究

以绿茶为试验材料,从茶汤体系的物化性质和化学成分两方面探讨了茶汤沉淀形成的机理。通过对沉淀形成过程中沉淀颗粒形态变化、电解质和氢键裂解剂的作用、红外光谱变化等内容的研究,来判断茶汤形成沉淀前后的性质改变,初步判定经低温贮存后的茶汤体系介于胶体分散系和粗分散系;茶汤颗粒间的氢键、静电作用是影响茶汤沉淀形成的因素,共价键不是沉淀形成的主要因素。通过计算茶汤中各主要成分进入上清相和沉淀相的分配系数,来判断该成分进入上清相和沉淀相的趋势,结果表明:茶多酚是构成茶汤沉淀物的主体物质,其次是果胶、咖啡碱,而在沉淀相中分配系数较大的成分依次是叶绿素、没食子酸、果胶、蛋白质、花青素、咖啡碱、可可碱。