REASONABLY FULL HYDROLOGIC DEVELOPMENT OF RESERVOIR SITES1

The size of multipurpose reservoir development is usually determined by an economic analysis of reservoir capabilities and the present and projected water resources needs which can be satisfied. This analysis is referred to as project formulation, wherein optimum conditions are sought. In responding to multiple objectives, i.e., national economic development, regional development and environmental quality, which are being considered in river basin planning in recent years, reservoirs should provide for reasonably full hydrologic development. Additional storage will be needed to provide opportunities for economic development, as well as meet unexpected development. Also, it provides more flow regulation capability for quality of environment considerations. An analysis has been made on twelve reservoir sites in the New York State portion of the Susquehanna River Basin to determine the so-called “reasonably full hydrologic development of reservoir sites.” Hydrologic, economic, environmental and physical characteristics of the sites are taken into consideration. For normal conditions, it can be concluded that a yield equivalent to about 80 percent of the average discharge (runoff) can be considered as reasonably full hydrologic development for reservoir sites in the Susquehanna River Basin in New York. The same technique can be applied elsewhere to determine reasonably full hydrologic development of reservoir sites.     

DEEP PERCOLATION IN A SAND HILL AREA1

Records for two rivers flowing in a Sand Hill area are used to derive a value for the infiltration reaching the water table. The infiltration is 0.23 feet per year which is 13 per cent of the precipitation.     

污水地下渗滤系统基质床特性模拟

为提高污水地下渗滤系统(Subsurface Waste-water Infiltration System,SWIS)的生物脱氮效率,改进了基质床体结构组成,采用土柱模拟试验对比了基质床改进前后ORP特征及氨化、硝化及反硝化细菌数量的变化。结果表明,在地下渗滤系统中,氨氮的去除率(Q)随基质层深度的变化规律为Q(100 cm)Q(80 cm)Q(20 cm)≈Q(40 cm)Q(60 cm)。改进后基质铺设顺序依次为:0~60 cm填充炉渣和草甸棕壤(两者体积比为3∶7),60~130 cm铺设活性污泥、炉渣和草甸棕壤(三者体积比为1∶2∶7)。基质床结构组成改进后,20~60 cm区域氧化电位(ORP)大幅提高,尤其60 cm深度处ORP从0提高到180 m V,有效促进了硝化反应的进行;床体氨化、硝化及反硝化细菌数量大幅度提高,对NH+4-N及TN的脱除效率分别较改进前提高了12.6%和10.5%,出水NH+4-N及TN质量浓度满足城市景观地表水水质标准(GB/T 18921—2002)。     

基于水生态系统结构特征的滇池流域水生态功能三级分区

水生态功能分区的目的是为了实现中国流域的"分区、分类、分级、分期"管理的精细管理理念,而水生态系统结构是水生态系统完整性的基础,也是区分不同区域生境特征与功能差异的重要指标.因此,为了实现更精细化的湖泊流域管理,在滇池流域完成水生态功能二级分区基础上,基于水生态系统结构特征进一步对滇池流域进行三级区划,进而反映流域水生态功能的空间异质性.以反映水生态系统结构的物理、化学与生物特征为依据,分别构建了滇池流域陆域与湖体的三级分区指标体系;通过对三级分区单元指标综合值进行聚类分级,最终将滇池流域的水生态功能三级分区划分为20个陆域区和4个湖体区,并利用底栖与藻类的生物数据对分区进行合理性评价.最后基于生态服务功能理论,结合滇池流域自身特点与管理需求,将滇池流域三级分区定义为不同的水生态功能类型.通过对滇池流域水生态功能三级分区的划分以及主体功能的确定,不仅为滇池流域水生态健康管理构建了空间管理单元,而且为湖泊水生态功能分区的研究提供了案例.     

海河流域河流空间分布特征及演变趋势

海河流域涵盖我国"京津冀"经济圈,河流对流域内人类生存和经济发展具有重要支撑作用,研究河流空间分布及演变趋势对于合理利用河流水资源、保护河流生态和实现经济可持续发展具有重要意义.本文运用遥感资料的GIS分析方法,对海河流域的河流地貌、水系结构、河流曲率和河网密度、闸坝等指标进行分析,发现:1海河流域河流地貌划分为上游山区段、中部平原段和下游滨海段,3个区段水系形状依次为树枝状(受人为干扰小),编织状(中度人为干扰),稀疏编织状(人为干扰强烈);2流域水库和水闸修建阻断河流纵向连续性,五大水系(滦河、北三河、永定河、大清河、子牙河)连续性指标值低于5;320世纪60年代—80年代—2000年,流域河流平均曲率不断减小,河网密度呈现不定向波动,反映出人为控制对河道形态改变程度大.今后应减少人类活动对河流自然属性的改变,河流治理和修复过程中应充分考虑保护和改造河流地貌、水系结构、河流曲率和河网密度.     

概率法计算不同下沉深度下凹绿地蓄水效率的研究

作为一种简单而实用的城市雨水渗蓄技术,下凹绿地具有削减洪峰流量、截留滞纳雨水的功能.结合天津市多年降雨统计资料,采用概率分析方法,探讨下凹绿地的蓄渗效率.结果表明:在绿地率为30％左右的条件下,即使是在土壤稳渗系数相对较低的地区开发下凹绿地,下挖深度只要满足60 mm,开发后的下凹绿地的渗蓄效率都可达到95％.但下凹深度超过100 mm后,随下凹深度继续增加而提高的渗蓄效率不足5％.考虑到建设成本和收益比等因素,建议天津市修建下凹绿地的深度范围为60 mm～100 mm.     

非饱和红壤土降雨入渗室内模拟试验

以江西省域范围内典型红壤土为研究对象,利用自行研制开发的降雨模拟试验设备与渗透试验装置,设计了大雨工况下土体初始含水率、干密度、降雨累积时间及降雨后土体静置时间等对其渗透性影响的室内试验。试验结果显示,土体渗透性随初始含水率的升高逐渐降低,给出的宏观渗透系数公式定量化描述了不同初始含水率的可渗透性强弱程度;在初始含水率相对固定的情况下,土体渗透性随干密度的增大逐渐减小,且干密度增大到一定程度后其渗透性锐减,各水平之间的差异性不再明显;累积降雨时间会显著影响深部土体的渗透性,降雨历时越长,深部土体的含水率越高;雨水的在降雨过程停止后继续沿土体纵深入渗,致使表层含水率降低,深部含水率提高,含水率特征曲线趋向竖直。     

Evaluating the Applicability of a Two‐dimensional Flow Model of a Highly Heterogeneous Domain to Flow and Environmental Management

Two‐dimensional simulation of highly heterogeneous domains, especially those with disparate length scales, roughness conditions, and geometries, often leads to challenges such as long computation times and numerical instability. Simulation of challenging domains is often needed to guide flood management and environmental regulation agencies in operation and potential domain modifications. This work evaluates the ability of a two‐dimensional unsteady hydrodynamic model to represent long‐duration transient flows over a domain with highly heterogeneous roughness, geometric characteristics, and length scales through bed roughness representation. The domain includes 13 km of Cache Creek and the 14.5 km² Cache Creek Settling Basin, which traps both sediment and mercury. Calibration under different bed roughness methods, validation, and modeling results of bathymetric modification scenarios are presented. The modeling approach's performance supports its application as a tool for management of similar domains, such as settling basins, leveed floodplains, and reservoirs. Accurate representation of flow dynamics can also inform environmental management that involves transport of sediments, nutrients, and heavy metals. This study found that a two‐dimensional unsteady flow model can accurately represent long‐duration transient flow in a large settling basin with highly heterogeneous characteristics without parsing of the domain or flow events simulated.     

DCCH型澄清池的性能试验研究

文章通过现场试验和分析分别考察了混凝剂加药量,活性泥渣浓度,助凝剂,澄清池进水流量和机械搅拌力度因素对DCCH型澄清池出水残余浊度的影响。试验表明增加混凝剂加药量可改善出水水质,但药量过量会使残余浊度上升;在一定范围内增加反应区活性泥渣沉降比澄清池残余浊度降低,且残余浊度与活性泥渣浓度符合一级反应动力学规律;助凝剂可改善絮体结构使残余浊度降低,但从经济环保角度出发应尽量减少使用量;增加进水流量使残余浊度上升,上升幅度主要取决于澄清池形成絮体的结构;适当增加机械搅拌力度能有效的降低澄清池残余浊度。     

太湖流域湖泊滩地资源及其开发利用

在调查和分析太湖流域湖泊滩地资源特征和开发利用状况的基础上,着重探讨了滩地围垦对流域生态环境的影响,并提出今后开发利用滩地资源的方向和对策。