Rapid manganese removal from mine waters using an aerated packed-bed bioreactor

In the UK, the Environmental Quality Standard for manganese has recently been lowered to 30 microg/L (annual average), which is less than the UK Drinking Water Inspectorate's Maximum Permitted Concentration Value (50 microg/L). Current passive treatment systems for manganese removal operate as open-air gravel-bed filters, designed to maximize either influent light and/or dissolved oxygen. This requires large areas of land. A novel enhanced bioremediation treatment system for manganese removal has been developed that consists of a passively aerated subsurface gravel bed. The provision of air at depth and the use of catalytic substrates help overcome the slow kinetics usually associated with manganese oxidation. With a residence time of only 8 h and an influent manganese concentration of approximately 20 mg/L, >95% of the manganese was removed. The treatment system also operates successfully at temperatures as low as 4 degrees C and in total darkness. These observations have positive implications for manganese treatment using this technique in both colder climates and where large areas of land are unavailable. Furthermore, as the operation of this passive treatment system continually generates fresh manganese oxyhydroxide, which is a powerful sorbent for most pollutant metals, it potentially has major ancillary benefits as a removal process for other metals, such as zinc.     

GEOMORPHOLOGY OF STEEPLAND HEADWATERS: THE TRANSITION FROM HILLSLOPES TO CHANNELS1

Headwater streams comprise 60 to 80 percent of the cumulative length of river networks. In hilly to mountainous terrain, they reflect a mix of hillslope and channel processes because of their close proximity to sediment source areas. Their morphology is an assemblage of residual soils, landslide deposits, wood, boulders, thin patches of poorly sorted alluvium, and stretches of bedrock. Longitudinal profiles of these channels are strongly influenced by steps created by sediment deposits, large wood, and boulders. Due to the combination of small drainage area, stepped shallow gradient, large roughness elements, and cohesive sediments, headwater streams typically transport little sediment or coarse wood debris by fluvial processes. Consequently, headwaters act as sediment reservoirs for periods spanning decades to centuries. The accumulated sediment and wood may be episodically evacuated by debris flows, debris floods, or gully erosion and transported to larger channels. In mountain environments, these processes deliver significant amounts of materials that form riverine habitats in larger channels. In managed steepland forests, accelerated rates of landslides and debris flows resulting from the harvest of headwater forests have the potential to seriously impact the morphology of headwater streams and downstream resources.     

BASE FLOW TRENDS IN URBANIZING WATERSHEDS OF THE DELAWARE RIVER BASIN1

Rapid land development is raising concern regarding the ability of urbanizing watersheds to sustain adequate base flow during periods of drought. Long term streamflow records from unregulated watersheds of the lower to middle Delaware River basin are examined to evaluate the impact of urbanization and imperviousness on base flow. Trends in annual base flow volumes, seven‐day low flows, and runoff ratios are determined for six urbanizing watersheds and four reference watersheds across three distinct physiographic regions. Hydrograph separation is used to determine annual base flow and stormflow volumes, and nonparametric trend tests are conducted on the resulting time series. Of the watersheds examined, the expected effects of declining base flow volumes and seven‐day low flows and increasing stormflows are seen in only one watershed that is approximately 20 percent impervious and has been subject to a net water export over the past 15 years. Both interbasin transfers and hydrologic mechanisms are invoked to explain these results. The results show that increases in impervious area may not result in measurable reductions in base flow at the watershed scale.     

2003～2004年大亚湾澳头养殖区水域浮游植物群落结构及数量变动特征

2003年4月至2004年4月对大亚湾赤潮高发区澳头海域进行了浮游植物群落周年调查和分析.共鉴定浮游植物57属118种.其中硅藻为优势类群,共42属84种,占总种类数的71.2%;甲藻11属27种.浮游植物数量分别在春末夏初,秋末冬初出现两个高峰值,年均值为5.68×105 /L.角毛藻属为全年优势属,平均占浮游植物数量的35.4%.Shannon-Weaver多样性指数和均匀度的年平均值分别为2.0和0.44.该海域共发现赤潮生物58种,锥状斯氏藻是最常见的甲藻赤潮生物,2003年8月该藻与海洋卡盾藻在澳头海域首次引发甲藻和针胞藻双相型赤潮.     

氮对酵母菌-SBR系统效能及酵母形态的影响研究

在酵母菌-SBR系统处理高含油废水中研究了氮添加对酵母细胞形态、沉降性、废水处理效果的影响及恢复能力.结果表明,氮添加量直接影响到系统中酵母菌的生物量,沉降性、pH和处理效果;氮缺乏诱发某些酵母菌菌株细胞由酵母形态向真菌丝形态转化,进而影响到酵母菌的沉降性;从系统运行效果和稳定性方面综合考虑,运行时最佳的进水BOD/N为20/1;恢复最佳氮添加能提高不同程度缺氮系统的处理效果,并可使轻度菌丝化系统快速恢复酵母形态为主,但在短期内对高度菌丝化系统的恢复效果不明显.     

Improved speciation of dissolved organic nitrogen in natural waters: amide hydrolysis with fluorescence derivatization

The objective of this study was to improve primary-amine nitrogen (1°-N) quantification in dissolved organic matter (DOM) originating from natural waters where inorganic forms of N, which may cause analytical interference, are commonly encountered. Efforts were targeted at elucidating organic-N structural criteria influencing the response of organic amines to known colorimetric and fluorescent reagents and exploring the use of divalent metal-assisted amide hydrolysis in combination with fluorescence analyse...     

混凝-A3-MBR处理餐厨垃圾发酵废液运行条件优化与特性

采用混凝-两级厌氧/缺氧/好氧-膜生物反应器（A3-MBR）处理实际餐厨垃圾发酵废液,通过对运行参数进行优化确定最优工况,并考察其在该条件下长期运行的处理效果。结果表明,混凝预处理的最适pH为8,最佳混凝剂投加量为1 000 mg·L-1。A3-MBR系统在最优运行条件：总HRT为110 h,回流比为200%,进水COD负荷控制在2.3~3.6 g·（L·d）-1下可稳定运行。当系统进水COD、TN、NH3-N和TP浓度分别为（10 984±383）、（335.9±16.2）、（209.1±6.7）和（37.2±2.3）mg·L-1时,系统进水有机负荷为2.3~3.5 g·（L·d）-1,在最优条件下处理系统出水的COD、TN、NH3-N和TP分别为（202±23）、（62.1±7.1）、（0.33±0.13）和（8.3±0.9）mg·L-1,其去除率分别为98.2%、81.5%、99.8%和77.8%。A3-MBR系统对有机物具有良好的去除效果,厌氧段未积累挥发性脂肪酸。最终出水中溶解性有机物主要为II区芳香族蛋白质类似物,残留的挥发性有机物以酯类物质为主。     

添加炭基材料对蔬菜废物好氧堆肥进程和腐熟度的影响

以蔬菜废弃物辣椒秸秆和树叶为堆肥原料(CK),采用密闭式好氧堆肥工艺,研究了添加5%木本泥炭(T1)、5%活性炭(T2)和10%木本泥炭(T3)等炭基材料对堆肥pH、EC、CO2累积量、物料损失率、T值、C/N和发芽率指数的影响。结果显示,T2处理的pH在60 d后维持在8~9之间;EC值随着堆肥进行呈现先下降后升高再下降的趋势,最终CK、T1、T2和T3处理的EC值(mS/cm)分别降低了1.02、0.76、0.33和0.48;T2和T3处理的CO2累积量一直高于其他处理;所有处理的物料损失率均在20%以上;4个处理堆肥产品的T值分别为0.56、0.65、0.68和0.69;堆肥产品的发芽率指数分别为63.2%、69.3%、93.5%和86.1%。T值和发芽率指数显示T2和T3处理达到了腐熟阶段。结果表明,在蔬菜堆肥处理中添加炭基材料可改善堆肥产品的理化性质,加速堆肥物料的分解,有效地缩短堆肥周期和提高堆肥产品的腐熟度。     

壳聚糖改性红壤去除铜绿微囊藻

研究了聚合氯化铝铁和壳聚糖改性对高岭土、海泡石和红壤去除水中铜绿微囊藻效果的影响。结果表明,壳聚糖改性的红壤对铜绿微囊藻的去除效果最好,其生成絮体密实度大,抗扰动能力强。当改性红壤的投加量为50 mg/L时,叶绿素a和铜绿微囊藻去除率分别达到98.0%、95.1%。该絮凝剂适应性好,在pH为3.0~6.0的范围内对铜绿微囊藻均可取得很好的去除效果,对叶绿素a和浊度的去除率可达90%以上。壳聚糖通过包裹红壤颗粒,借助壳聚糖的粘结架桥和电中和能力,大幅度提高了红壤的絮凝性能。该絮凝剂处理富藻水,具有絮凝效果明显、絮体密实度大、投加量少、绿色环保、经济等优点,在工程上具有较大的实用价值。     

助溶剂甲醇对化学物质紫外光解的影响

在研究微量有机化学污染物的光化学行为时,为了增加难溶于水的药品溶解度,往往采用甲醇作助溶剂.但对反应体系中助溶剂甲醇对光化学反应的影响缺乏系统研究.以高压汞灯为光源,以萘普生(NP)及其光解产物NP1和NP2为研究对象,通过对比纯水、1%甲醇和1%异丙醇反应体系中的实验结果发现,少量助溶剂甲醇在紫外光照下对羟基自由基的淬灭效果接近于异丙醇.结合检测到的中间产物,推导了NP的光解路径主要为光致脱羧、羟基自由基夺氢、自由基耦合等反应过程.在助溶剂甲醇存在的体系中,甲醇能与萘普生发生酯化反应,并通过淬灭羟基自由基,影响萘普生的光解反应,从而导致实验结果误读.因此,在光化学实验研究中,应该排除助溶剂甲醇对实验结果的影响.