桂花水电站掺气分流墩与消力池联合应用消能效果的研究

通过试验研究了桂花水电站拱坝掺气分流墩的体型、布置和水流流态,消力池和消力池中T型墩的体型和布置,掺气分流墩和消力池联合应用的水流流态和消能效果。试验表明,掺气分流墩与消力池联合应用明显改变了水流流态,具有显著的消能效果。     

黑河下游河道渗漏面积的估算及其精度初步研究

黑河流域是我国西北干旱区内陆河的一个典型流域,其下游生态环境用水主要来源于地下水,地下水的补给主要通过河流的渗漏过程,因此河道渗漏补给是下游生态用水的主要来源。定量确定河道渗漏水量之前,首先需要确定河道渗漏面积。由于野外条件的限制,河道过水过程中黑河下游狼心山至东居延海区间河道的渗漏面积实地测量非常困难。根据水文流量资料选取2001年、2002年、2004年、2009年四年中全断面过水ETM遥感影像数据,在此基础上,运用遥感与GIS技术研究了对应时间黑河下游河道渗漏面积。选取具有不同特征的五段河道,运用AutoCAD软件对遥感提取结果进行误差分析,得到平均相对误差为4.29%,证明直接利用监督分类方法提取得到的结果具有较高的精度。在此基础上,建立渗漏面积与河长之间的关系。为该区域的水文过程及河道周围生态环境等的研究提供了数据和研究基础。     

基于约束区域的BSB联想记忆模型

提出一种根据联想记忆点设计基于约束区域的ＢＳＢ（Ｂｒａｉｎ－Ｓｔａｔｅ－ｉｎｍ－ａ－Ｂｏｘ）神经网络模型,它保证了渐近稳定的平衡点集与样本点集相同,不渐近稳定的平衡点恰为实际的拒识状态,并且吸引域分布合理,从而将ＥＳＢ完善为理想的联想记忆器。     

Estimation of Basins of Attraction for Uncertain Systems with Affine and Lipschitz Dynamics

This paper is devoted to estimation and numerical approximation of basins of attraction for a class of uncertain systems. We consider systems described by a differential equation depending of a disturbance known by its bounds. By using viability theory tools, we derive basins of attraction lower and upper estimates. We present numerical simulation results of the viability kernel algorithm to basin of attraction approximation problems.     

新疆玛纳斯河流域水资源利用与管理

随着社会经济发展,生活水平的提高以及城市规模的扩大,玛纳斯河流域内水资源供需矛盾日益突出,用水结构发生重大变化,水资源污染日趋恶化。探讨流域水资源在利用与管理过程中出现的诸多问题,并提出改进的几点意见与建议。     

变动态存储系数法在辽宁大凌河流域河道洪水演算中的运用研究

本文选用变动态存储系数法进行河道洪水演算,弥补传统水文模型河道洪水演算将洪水传播时间设为定值的不足。论文选取辽宁大凌河上游大城子水文站2000-2013年15场洪水资料对模型进行率定和验证,并和传统水文模型河道洪水演算方法模拟结果进行对比研究,结果表明相比于传统水文模型,采用变动态存储系数法的洪水模拟精度有所提高,15场洪水模拟合格率提高20%。研究成果对于大凌河流域水文模拟,特别是分布式水文模拟提供较为重要的参考价值。     

IMPLEMENTING ENVIRONMENTAL FLOWS IN COMPLEX WATER RESOURCES SYSTEMS – CASE STUDY: THE DUERO RIVER BASIN,SPAIN

European river basin authorities are responsible for the implementation of the new river basin management plans in accordance with the European Water Framework Directive. This paper presents a new methodology framework and approach to define and evaluate environmental flow regimes in the realistic complexities that exist with multiple water resource needs at a basin scale. This approach links river basin simulation models and habitat time series analysis to generate ranges of environmental flows (e‐flows), which are evaluated by using habitat, hydropower production and reliability of water supply criteria to produce best possible alternatives. With the use of these tools, the effects of the proposed e‐flows have been assessed to help in the consultation process. The possible effects analysed are impacts on water supply reliability, hydropower production and aquatic habitat. After public agreements, a heuristic optimization process was applied to maximize e‐flows and habitat indicators, while maintaining a legal level of reliability for water resource demands. The final optimal e‐flows were considered for the river basin management plans of the Duero river basin. This paper demonstrates the importance of considering quantitative hydrologic and ecological aspects of e‐flows at the basin scale in addressing complex water resource systems. This approach merges standard methods such as physical habitat simulations and time series analyses for evaluating alternatives, with recent methods to simulate and optimize water management alternatives in river networks. It can be integrated with or used to complement other frameworks for e‐flow assessments such as the In‐stream Flow Incremental Methodology and Ecological Limits of Hydrologic Alteration. Copyright © 2011 John Wiley & Sons, Ltd.     

Spatial distribution and habitat characterization of schistosomiasis host snails in lake and land habitats of western Kenya

Intermediate host snails of schistosomiasis were surveyed in this study to determine their abundance and distribution in the lake and land aquatic habitats of Lake Victoria basin of Kenya. Several sites were sampled at eight locations, both in the lake and on the land. The habitat and/or vegetation type (i.e. open water, hippo grass, hyacinth, ambatch trees, other vegetation, stream, swamp, pond, dam) of the sampled aquatic sites within the locations were also differentiated, water physicochemical parameters were determined, and the abundance of different species or taxa of phytoplankton and zooplankton were enumerated and correlated with the abundance of schistosomiasis snails in the sites. The results indicated significantly more Biomphalaria sudanica snails than Bulinus africanus snails in different physical habitats on land (Student's t‐test, P < 0.05), as well as in different locations on land (Student's t‐test, P = 0.026). Regression analyses revealed that several physicochemical parameters, including dissolved oxygen (R² = ?0.659; n = 8; P = 0.014), pH (R² = 0.728; n = 8; P = 0.007) and turbulence (R² = ?0.616; n = 8; P = 0.02), were predictive of Biomphalaria spp. abundance, while pH (R² = 0.610; n = 8; P = 0.02) and turbulence (R² = ?0.578; n = 8; P = 0.028) were predictive of Bulinus spp. abundance in different locations in the lake. Cyanobacteria (R² = 0.638; n = 8; P = 0.02) and chlorophyceae (R² = ?0.50; n = 8; P = 0.05) were shown to be predictive of both Biomphalaria spp. and Bulinus spp. abundance in different locations in the lake. Zooplankton abundance varied significantly between different locations in the lake (One‐way anova , P < 0.001). Bosmina spp. were found to be predictive of both Biomphalaria spp. (R² = ?0.627; n = 8; P = 0.01) and Bulinus spp. (R² = ?0.50; n = 8; P = 0.05) in different locations in the lake. The results from this study will help inform policy regarding control measures for schistosomias and intermediate snail hosts in Lake Victoria waters, as well as in adjacent terrestrial aquatic habitats and even beyond.     

GRACE反演近年青藏高原及雅鲁藏布江流域陆地水储量变化

利用2005年至2010年6年的GRACE(Gravity Recovery and Climate Experiment)数据反演,研究了青藏高原地区以及雅鲁藏布江流域的季节及年陆地水储量的变化情况.结果显示:在研究区,伴随着显著地季节性波动,年水储量均有明显的下降趋势.同时,流域GRACE数据反演结果和国际上几种模式的水文模拟结果比较表明,GRACE在两个流域上的反演结果与CPC水文模型模拟结果变化趋势较为一致,但水储量年、季变化幅度偏大,而与GLDAS发布的CLM与VIC模型的结果则相差甚远,主要原因归结为青藏高原地区气候条件复杂导致模型的不确定性及误差较大,而大多水文模型缺乏对地下水变化的模拟能力所致.     

江苏太湖流域降雨径流年际变化分析

以江苏太湖流域（1956—2012）降雨为基础,分析江苏太湖流域径流及时空变化特征,研究该流域降雨径流的年际年内变化及两者的变化关系。结果表明：降雨径流都呈增长趋势。降雨平均每10年增加29mm,径流平均每10年增加26mm;降雨在年内季节分配上,夏季、冬季呈加大趋势,春季、秋季呈减小趋势;加大的降水年内分配的不均导致径流在年内分配的更加不均匀,径流集中在汛期,汛期径流量约达年径流量的84．8％,加大了某季节内的洪水、干旱风险。