中国洪水预报系统在贝江勾滩洪水预报中的应用

采用中国洪水预报系统的应用平台建立贝江勾滩水文站降雨径流模型洪水预报方案,利用系统自动进行模型参数的率定,该方案在精度的评定及实际应用中取得较满意的效果,解决了勾滩站长期没有洪水预报方案指导防洪的迫切的问题,为中国洪水预报在柳江流域的应用积累了经验.     

采用浊度监测实现悬移质泥沙监测自动化的探讨

介绍了南宁水文站通过对水体浊度参数测试,得到浊度与含沙量关系,研究新悬移质泥沙监测模式,实现悬移质泥沙监测自动化,推进水文信息化进程适应经济发展,为防灾减灾决策,及时、准确提供科学依据。     

引水济湖工程措施的生态环境影响评价方法

在湖泊引水方案和二维环境流体动力学模型影响预测计算结果的基础上,提出引水后湖泊环境生态影响预测评价方法:①从湖泊水景的自然度、自净(健康)度、景观度、亲水度、连通度5个方面,构造了引江济湖工程对湖泊生态-环境-景观综合影响指数评价法;②从水环境质量、生物多样性、防洪排涝、景观生态结构等方面应用质量指标法进行工程对湖泊健康综合影响评价。实例应用表明,两种评价方法可以对湖泊引水影响效果进行科学评价,结论也比较一致,为正确实施引水济湖方案提供了科学评估方法和依据。     

浅析东雷抽黄灌区泵站更新改造设计中的几个重要环节

通过渭南市东雷抽黄大型灌溉泵站的更新改造设计,提出泵站在改造设计中应注意的几个重要环节,以期为其他大型灌排泵站的更新改造提供参考与帮助。     

坝王河羡塘至大井、小井河段开发方式研究

针对坝王河流域忽明忽暗、明伏交替、落水洞遍布、地下暗河系统发育等强喀斯特特点,拟对羡塘至大井、小井河段的开发采取分段开发的思路,上河段为合理规避河段喀斯特渗漏问题,采用长隧洞引水方式;下河段为避开地下暗河系统和渗漏河段,选择成库条件较为可靠的坝址和引水线路较短的开发方案.其工程经验可供类似流域开发借鉴.     

深覆盖层河道闸坝电站防沙布置试验研究

某闸坝式水电站坝址覆盖层深厚,河道欠宽阔,发电引用流量比例较高,受调节库容限制,库区泥沙将很快输移到达坝前,引水防沙问题突出。本文对施工围堰作为其电站枢纽引水防沙体系的效果进行了水工模型试验研究和分析。对四种挡沙坎布置型式进行了对比试验研究。表明,利用原有挡水围堰,结合纵向挡沙坎与排沙底孔联合作用既有利于施工方便,拉沙效果又较好,可达到电站＂门前清＂,较好的解决了大流量闸坝式电站的引水与防沙之间的矛盾。本研究成果的成功实施可减少工程投资,缩短工期,尤其对于在低水头、大单宽的多沙河流上修建的闸坝工程具有较好的借鉴意义。     

黄河下游河湾平面参数特性及其实验研究

以黄河下游,尤其是游荡型河段的研究资料为背景,通过模型试验,在分析河势变化过程的基础上,运用数学统计与理论探讨,研究了不同水沙条件下河湾中心角、河湾半径和河湾跨度的变化趋势,初步揭示了随水沙、比降条件的改变,河势的变化过程,总结出河流在边界条件改变后河势演变的特点,对预测河道演变趋势,有效地河道整治具有一定的意义。     

区域层面河湖功能区划研究——以太湖流域为例

河湖功能区划是加强流域管理的一项新举措.对于自然属性和社会经济属性较为均一的区域,河流功能难以按其沿河道的空间分异性进行划分.基于这一特点,提出了区域层面河湖功能区划的概念,建立了由因素层、区划层和功能层构成的区域层面河湖功能区划体系,并提出了区划的方法和程序.进行了太湖流域区域层面河湖功能区划实践,将该区域共划分为3类13个河湖功能区,给出了每一区的功能定位和管理措施.结果表明,区域层面河湖功能区划的概念与方法合理可行,为平原河网区的河湖管理提供了一个新途径.     

Large wood aids spawning Chinook salmon (Oncorhynchus tshawytscha) in marginal habitat on a regulated river in California

To determine whether large wood (LW, ≥1‐m length, ≥10‐cm diameter) plays a role in Chinook salmon (Oncorhynchus tshawytscha) redd (i.e. egg nest) placements in a regulated, Mediterranean‐climate, medium‐sized river (where channel width is less than the upper quartile of length of potential instream wood pieces), characteristics of 527 large wood pieces, locations of 650 redds, and mesohabitat delineations (riffle, run, glide, pool) were collected during a spawning season along a 7.7 km reach directly below Camanche Dam on the Mokelumne River, CA. LW was regularly distributed across the study reach an average 70 LW pieces km^‐1. Some LW clustering was evident at islands and meander bends. Spawners built 85% of redds within one average channel width (31 m) of LW. Spawners utilized LW within a 10 m radius 36% of the time in the upper 3 km rehabilitated reach, and 44% of the time in the lower 4.7 km marginal habitat reach. A greater percentage of LW was utilized in riffles in the upper 3 km reach where 90% of redds were built, while a larger percentage of spawners used LW in riffles in the lower 4.7 km reach. LW‐redd interactions occurred at greater rates than by random chance alone in the lower 4.7 km reach, which implies that LW aids spawning in marginal habitats. River managers and salmonid spawning habitat rehabilitation (SHR) projects should take LW additions into consideration as an important component of river rehabilitation. Copyright © 2010 John Wiley & Sons, Ltd.     

Water quality in the southern Tibetan Plateau: chemical evaluation of the Yarlung Tsangpo (Brahmaputra)

Yarlung Tsangpo (Brahmaputra) is the largest river system draining the northern slopes of the Himalayan ranges on the southern Tibetan Plateau. It remains one of only two large non‐regulated rivers in China. In this paper the chemical composition of Yarlung Tsangpo and its major tributaries (Raga Tsangpo, Nyangchu and Lhasa River) are studied. Water samples (n = 55) were collected and measured for major ions, trace elements and nutrients in order to: (1) define the present chemical quality of this water course; (2) address possible mechanisms governing the water chemical compositions, and (3) identify potential sources for contaminants. Multivariable analysis shows that geology and climate are the major explanatory variables for the spatial variation in water chemistry in this river system. In general, water chemistry is mainly controlled by carbonate weathering, with Ca²⁺ and HCO being the dominant ions. In addition, runoff from brackish/saline lakes and geothermal waters, enriched in Na⁺, Cl^?, SO, Mg²⁺ and Li, are major contributors of elevated concentrations of these solutes in the headwater regions resulting in a relatively high loading of total dissolved solids (TDS, 146–397 mg L^?1). Levels of most heavy metals and total dissolved nutrients were generally found to be low. However, elevated As concentration (avg. 95 μg L^?1) in the headwaters and additions from untreated wastewater were evident at some locations. Copyright © 2009 John Wiley & Sons, Ltd.