硅藻土混凝剂在污染河水处理中的应用研究

以改性硅藻土为混疑剂，对具有不同污染特征的苏州河各支流污染水体进行了化学强化一级处理试验研究。结果表明，硅藻土混疑剂的最佳投药量随原水水质的不同而不同；硅藻土对C0Dcr和P有较高的去除效率，而对NH3-N的去除率不高；不同污染河水水质对硅藻土的混疑效果有比较显著的影响，表现为在混疑剂的最佳投药量条件下，C0Dcr去除量与原水CODcr之间存在着显著的线性关系。     

北江万古流

北江是珠江水系第二大支流，全长582km，流域面积有4.7×105km2。北江是晚第三纪以来形成发育的，塑造了著名的丹霞地貌峡谷。水力、矿产、动植物和旅游资源丰富。     

肇源县环境问题及其防治对策的研究

肇源江段是重要的水质监测段,是松花江干流水质监测的前哨.多年来黑龙江省政府高度重视肇源江段的水质污染.本文结合大量的以往监测结果,指出了肇源县环境问题主要是水环境污染,由于上游第二松花江大量石油化工企业工业废水及大庆市部分工业废水的流入及本地区各种废水的排放使其地表水和地下水,特别是松花江的水质受到严重污染,不仅是常规监测项目超标,而且存在严重的有机污染物的污染.这使松花江的水质及流域居民身体健康受到影响.依据松花江水质的污染特征提出保护松花江水环境的方法及对策,加强污染源的控制、加强流域污染防治的法制宣传教育.     

松花江水体中多环芳烃类污染物的污染研究

多环芳烃类污染物（PAHS）是化学性质比较稳定的一类污染物，具有“三致”作用，不仅难降解，而且生物毒性强，对水生态环境产生一定危害，研究表明，松花江江水以及松花江水补给的近江的浅层井水，包括水生生物及底质，均舍有多环芳烃类污染物，但暂不会对水生物和人体健康构成危胁.     

环渤海湾诸河口底质现状的调查研究

20 0 1年 6月实地采集了环渤海湾诸河口 19处土样 ,进行了汞、铜、锌、铅、砷、总氮、总磷和有机质含量分析 ,发现环渤海湾诸河口底泥中基本无重金属 (及砷 )污染 ,但与历史资料相比 ,近年来重金属含量普遍增加 ,特别是铅和锌含量增加幅度较大 .大多数河口底泥中的总氮和总磷含量较高 ,尤其是海河口附近的河口总氮和总磷含量高达 0 14%和 0 0 9%,通过与水体的交换 ,将对水体富营养化产生影响 .     

河流环境关心点的位置定量化

提出了河流环境关心点的概念，即指河流两岸或河中体现或影响河流环境功能的环境要素与河流某断面相互作用的点。阐述了河流环境关心点与位置定量化之间的关系及编制点位图时应遵循的功能原则、水质原则和边界原则，指出河流环境关心点位图能够比较直观、全观地反映各点位分布情况。以沅江为例，叙述了绘制各环境关心点位的方法。     

河流水质月报评价项目的选择

以三种评价项目选择法对国控河流断面水质评价的结果进行了比较。结合现阶段我国的经济技术条件选择了适用于河流水质月报的评价项目即pH、溶解氧、高锰酸盐指数、五日生化需氧量、氨氮、石油类、挥发酚、汞和铅等9项。     

Time Series Analysis to Monitor and Assess Water Resources: A Moving Average Approach

An understanding of the behavior of the groundwater body and its long-term trends are essential for making any management decision in a given watershed. Geostatistical methods can effectively be used to derive the long-term trends of the groundwater body. Here an attempt has been made to find out the long-term trends of the water table fluctuations of a river basin through a time series approach. The method was found to be useful for demarcating the zones of discharge and of recharge of an aquifer. The recharge of the aquifer is attributed to the return flow from applied irrigation. In the study area, farmers mainly depend on borewells for water and water is pumped from the deep aquifer indiscriminately. The recharge of the shallow aquifer implies excessive pumping of the deep aquifer. Necessary steps have to be taken immediately at appropriate levels to control the irrational pumping of deep aquifer groundwater, which is needed as a future water source. The study emphasizes the use of geostatistics for the better management of water resources and sustainable development of the area.     

马莲河水体中Cr+6来源调查

Cr+6是毒性最强的铬化合物.本文通过现场调查,对马莲河水体中Cr+6的来源进行了研究.结果表明,马莲河水体中Cr+6来自于地下泛水.     

How Hydrologic Connectivity Regulates Water Quality in River Corridors

Downstream flow in rivers is repeatedly delayed by hydrologic exchange with off‐channel storage zones where biogeochemical processing occurs. We present a dimensionless metric that quantifies river connectivity as the balance between downstream flow and the exchange of water with the bed, banks, and floodplains. The degree of connectivity directly influences downstream water quality — too little connectivity limits the amount of river water exchanged and leads to biogeochemically inactive water storage, while too much connectivity limits the contact time with sediments for reactions to proceed. Using a metric of reaction significance based on river connectivity, we provide evidence that intermediate levels of connectivity, rather than the highest or lowest levels, are the most efficient in removing nitrogen from Northeastern United States’ rivers. Intermediate connectivity balances the frequency, residence time, and contact volume with reactive sediments, which can maximize the reactive processing of dissolved contaminants and the protection of downstream water quality. Our simulations suggest denitrification dominantly occurs in riverbed hyporheic zones of streams and small rivers, whereas vertical turbulent mixing in contact with sediments dominates in mid‐size to large rivers. The metrics of connectivity and reaction significance presented here can facilitate scientifically based prioritizations of river management strategies to protect the values and functions of river corridors.