官厅流域农田地表径流磷流失初探

农田径流和侵蚀泥沙是磷进入官厅水库的主要非点污染源。针对该流域夏季农田暴雨径流发生的典型情景进行模拟降雨径流试验，对该流域农田地表径流泥沙和磷流失进行了初步的研究，结果表明，本降雨过程径流累积泥沙产量为30．5l～2493．34g／m^2，受雨强、坡度和作物覆盖的影响明显；径流溶解态磷(DP)中绝大部分是生物可利用性磷(DRP)，径流平均DP、DRP浓度都远大于水体允许临界值0．02mg／L，对官厅水体存在直接污染危害。径流累积全磷(TP)流失达O．0439～2．0798g/m^2；估算的流域农田径流全磷(TP)流失水平达2．67kg／(hm^2．a)以上，其颗粒态占969，0以上，可能成为官厅水库浮游生物长期丰富的潜在可利用磷源。降低农田土壤速效磷水平、减少水土侵蚀，是控制库区水华季节性发生和复原库区水体富营养化状态的关键。     

长江口柱状沉积物中有机质C/N比的研究

对长江口四个站位沉积物中有机质的C／N比在垂向上的分布进行了研究，在影响沉积物中有机质C／N比的环境因素中，上覆水体的水深、盐度、密度以及浊度对其有一定的影响．在研究沉积物中有机质C／N比的分布及其影响因素的基础上，进一步估算了陆源输入和海洋自生有机碳在这四个站位沉积物有机碳中所占的比例，结果表明，海洋自生组分占沉积物总有机碳的比例分别为：53．57％(8号站位)、20．34％(11号站位)，12．28％(17号站位)和32．73％(26号站位)．     

珠江广州河段底泥中汞铜铅的污染及其与有机质硫化物积累的关系

珠江广州河段底泥中有机质、硫化物和重金属汞、铜、铅的污染监测结果表明：各种污染物的含量范围分别为有机质２０．８—７４．４ｇ／ｋｇ，硫化物２８．７—５３８ｍｇ／ｋｇ，汞０．０７－０．７４ｍｇ／ｋｇ，铜２０．９—１０１ｍｇ／ｋｇ，铅１４．２—９１７ｍｇ／ｋｇ；它们在沿程各断面的分布表现为上游往中游递增，而中游向下游递减，基本上以猎德、广纸和黄沙三个断面的污染最严重；各种污染物的污染程度顺序是硫化物＞汞＞铜＞铅。相关分析表明：汞、铜与有机质和硫化物的相关关系均达到极显著水平。说明随着底泥中有机质和硫化物积累的增加，汞、铜的富集量相应增加，污染加重。     

底质中氨氮对沉水植物生长的影响

沉水植物的生长不但与水体营养盐浓度具有十分密切的关系,也受底泥中营养物质的影响,尤其是底泥中氨氮的含量对于植物生长具有重要的作用,因此研究底质中氨氮对高等沉水植物生长的影响,能够为沉水植被的重建及选种提供科学参考。作者在人工配制的7种含不同浓度铵态氮的底质条件下,通过测定苦草VallisnerianatansL.和伊乐藻Elodeanuttallii两种沉水植物的植株鲜物质量的变化、干物质量、根系的活力、过氧化物酶(POD)和过氧化氢酶(CAT)活性,以期明确这两种沉水植物与水体底质浓度之间的关系。试验结果表明,氨氮起始质量分数<50mg·kg-1和<500mg·kg-1时可以分别促进苦草和伊乐藻鲜物质量、干物质量和根系活力的增加,大于此范围则会抑制苦草VallisnerianatansL和伊乐藻Elodeanuttallii的生长。     

沉积物中腐殖质对铜毒性的影响

东湖沉积物中掺入腐殖质与铜 ,得到总有机碳 (TOC) 1.4 5 %～ 5 .72 %、总铜 (TCu) 12 0～ 2 70 0mg/kg的污染沉积物样品 ,离心法制取沉积物间隙水 .间隙水对大型溞 (Daphniamagna)进行 4 8h急性毒性试验 .沉积物及间隙水的化学分析表明 :间隙水中可溶性有机碳 (DOC)、铜 (Cu)、铁 (Fe)、锰 (Mn)、钙 (Ca)与沉积物中TOC和TCu含量关系呈现不同的变化规律 .多元分析表明 :间隙水中铜对大型溞的急性毒性 ,随沉积物中TOC含量的升高而减弱 ,随沉积物中总铜含量的增加而增强 ,多元回归方程为 :LC50 =- 0 .13179+0 .0 780 7[TOC]- 0 .0 0 0 12 [TCu]+0 .0 4 6 5 3[DOC]- 0 .0 80 4 5 [Cu]+0 .0 0 794 [Fe]+0 .0 36 6 [Ca],P =0 .0 0 0 0 相似文献   

淀山湖上覆水与沉积物孔隙水中重金属的分布特征

研究了淀山湖上覆水和沉积物孔隙水中Pb ,Cd,Cr,Cu ,Fe和Mn的浓度及Eh 分布 ,分析了孔隙水中重金属的扩散通量 .结果表明 ,淀山湖中重金属的浓度由高到低依次为 :Mn >Fe >Cr,Cu ,Pb >Cd ;Fe和Mn在孔隙水中的浓度远远大于它们在上覆水中的浓度 ,表层沉积物孔隙水中Pb ,Cd ,Cr,Cu的浓度稍大于它们在上覆水中的浓度 ;沉积物中的重金属可能按照浓度梯度经孔隙水从沉积物向上覆水中扩散而最终影响上覆水的水质     

Heavy Metals in the Bed and Suspended Sediments of Anyang River, Korea: Implications for Water Quality

The objective of this study is to compare Anyang River bed sediments with water chemical composition and to assess the anthropogenic chemical inputs into the river system. Eight sampling locations were chosen along the river channel. Bed and suspended river sediments and water samples were collected, and analyzed for their chemical and physical composition. Data revealed that trace element concentrations in the river water were generally below world average, except for As, Mn, Ni and Cr. Among the three phases: water, bed and suspended sediment, more than 99% of the trace elements was associated with the bed sediment. Concentrations of trace elements in the sediment were a function a particle size distribution and organic content. The calculated degrees of enrichment based on the least influenced sample (ASD 1) indicated the river sediments were enriched with respect to background. The enrichment factors for Pb, Zn and As were relatively lower than for Cr, Co, Ni and Zn. The difference in the enrichment seems to reflect the human activities influence in the basin, and specially for Cd. Speciation of the elements in the five different chemical forms in the sediment by sequential extraction indicated that the reducible fraction was predominant for Fe, Zinc and Cu showed an irregular variation among the different fractions; whereas, Cd and Pb were more regular. Zinc and Cu highly existed mostly in exchangeable forms. Acid soluble and reducible forms were also important for most metals. The speciation implies that the metals associated with the sediment are subject to release into water bodies as goechemical variables (pH and Eh) change. Currently, the introduced metals are deposited near the source area and are mostly associated with the sediment, implying that the river bed sediment acts mainly as a sink, rather than a pool. The accumulated and enriched toxic trace elements can pose a potential pollution of river water.     

无尾河下游湿地重金属污染评价

以无尾河下游漫流区———向海地区沼泽湿地为研究对象,通过对沼泽垂直剖面的精细采样,将放射性核素精确计年与重金属污染评价相结合,进行高分辨率剖析。在对其典型剖面沉积物重金属元素进行Al归一化的基础上,应用上下层比较法、富集系数法和地累积指数法3种评价方法对沉积物重金属污染富集水平及污染时序进行分析比较。结果表明,沼泽湿地沉积物表层已明显富集了重金属元素,达一定污染水平,这显示近20a霍林河流域上、中游人类活动对下游湿地的扰动增强。     

星湖沉积物特性研究

以肇庆星湖为研究对象，研究了其沉积物的各种特性。研究表明：(1)星湖沉积物的矿相(晶体物)主要为石英、伊利石、长石、绿泥石等；(2)沉积物中的TP、TN含量，基本随湖水交换和季节变化而变化，与交换量有着简单反比关系，其TP的含量在0．03％～0．06％之间，TN在0．19％～0．28％之间，内负荷较为严重；(3)沉积物的沉降存在很大的不均衡性；(4)沉积物营养物的释放受环境因子影响，其中溶解氧对N、P的释放都有较大的影响，温度对P的影响较N多一些，而保持水体中性，则有利于水体的稳定。     

EFFECTS OF BEST MANAGEMENT PRACTICES ON FOREST STREAMWATER QUALITY IN EASTERN KENTUCKY1

ABSTRACT: Forest land managers are concerned about the effects of logging on soil erosion, streamflow, and water quality and are promoting the use of Best Management Practices (BMPs) to control impacts. To compare the effects of BMP implementation on streamwater quality, two of three small watersheds in Kentucky were harvested in 1983 and 1984, one with BMPs, the other without BMPs. There was no effect of clearcutting on stream temperatures. Streamflow increased by 17.8 cm (123 percent) on the BMP watershed during the first 17 months after cutting and by 20.6 cm (138 percent) on the Non-BMP watershed. Water yields remained significantly elevated compared to the uncut watershed 8 years after harvesting. Suspended sediment flux was 14 and 30 times higher on the BMP and Non-BMP Watersheds, respectively, than on the uncut watershed during treatment, and 4 and 6.5 times higher in the 17 months after treatment was complete. Clearcutting resulted in increased concentrations of nitrate, and other nutrients compared to the uncut watershed, and concentrations were highest on the non-BMP watershed. Recovery of biotic control over nutrient losses occurred within three years of clearcutting. The streamside buffer strip was effective in reducing the impact of clearcutting on water yield and sediment flux.