佛山高明河水环境多环芳烃的分布特征与通量研究

利用液液萃取法和气相色谱-质谱方法对佛山境内高明河水环境多环芳烃（PAHs）进行了测定,并对PAHs的分布特征与通量进行了初步研究.结果表明高明河水环境中16种优控PAHs的浓度范围在41.6～375.6 ng/l之间,从上游到下游总体呈递增的趋势,其下游浓度偏高可能与荷城街道较为密集的工业和人口分布有关.高明河水环境PAHs的总含量高于欧美一些低污染水域,但低于国内一些主要河流.高明河PAHs年通量约为333.8 kg.     

不同养殖模式池塘沉降颗粒营养物质组成特征

2012年4~10月采用自制沉降颗粒收集装置收集主养草鱼和黄颡鱼池塘生态系统中沉降颗粒物,开展了颗粒物质的垂直沉降量以及沉降颗粒中碳氮磷等营养物质的组成及沉降通量的季节变化特征的研究。结果表明:养殖可以显著提高池塘颗粒物质的垂直沉降量,主养草鱼池塘中颗粒物质垂直沉降量显著高于主养黄颡鱼池塘(p0.01),且两种养殖模式池塘颗粒物质沉降量随着养殖时间推进有显著增加的趋势。主养草鱼的池塘中颗粒物质垂直沉降量在100.39~414.66g/(m2·d)之间变化,平均为224.46g/(m2·d),主养黄颡鱼池塘中沉降颗粒物质垂直沉降量在34.14~272.91g/(m2·d)之间变化,平均为155.18g/(m2·d)。两种养殖模式沉降颗粒的碳氮磷成分在养殖周期内的变化规律不明显但具有相似的变化趋势,主养黄颡鱼池塘沉降颗粒中TN、TC、TOC和TON的含量均比同时期主养草鱼高,且均随着养殖时间的推进,沉降颗粒中碳氮磷的总量呈增加趋势。两种养殖模式池塘沉降颗粒中的C/N比值与沉积物中的C/N比值较为接近,表明沉降颗粒与沉积物营养物质来源具有一定的相似性,同时养殖系统内养殖对象与其所处环境的相互依存和相互影响对颗粒物质的产生以及沉降具有重要作用。     

河口盐沼植物分布对有效光合辐射的响应

对东滩植被带光量子通量密度的调查研究表明:互花米草带与海三棱藨草带光量子通量密度没有显著性差异,其值分别为1 570和1 556μmol/(m2·s)。光照对两物种的生长、繁殖等植物行为的影响只取决于其对光照的利用能力和效率;在互花米草和海三棱藨草混生带,到达互花米草和海三棱藨草的光量子通量密度之间存在显著差异(P0.05),互花米草对海三棱藨草的遮荫效应达63%,表明互花米草对海三棱藨草具有强的遮荫作用。光照不足严重影响海三棱藨草的生长,在混生带,海三棱藨草生长速率降低,种群密度和生物量减少,植株高度增加。因此,互花米草对海三棱藨草的遮荫作用,抑制了海三棱藨草在中潮滩的更新过程,因而也是造成海三棱藨草生境丧失的重要原因之一。     

河流氧化亚氮产生和排放研究综述

氧化亚氮(N2O)是仅次于二氧化碳(CO2)和甲烷(CH4)的重要温室气体.由于人类活动对土地的影响导致河流系统中氮的可利用性增加,河流生态系统的N2O排放量正日益增长.本文对国内外河流水体N2O溶存浓度和饱和度、水-气界面排放通量及沉积物-水界面交换通量等数据进行了收集,并总结和分析了河流生态系统中N2O的产生机制及主要影响因子.     

生物强化/混凝沉淀工艺处理电镀园区物化出水的试验研究

试验采用生物强化/混凝沉淀工艺处理电镀工业园区的物化出水,重点考察了本工艺对进水COD、氨氮的去除效果.结果表明,生物强化工艺能有效降低废水中的COD、氨氮,混凝沉淀工艺能进一步去除废水中的污染物.当进水COD在200～ 350 mg/L、氨氮在20～35 mg/L时,出水水质能够达到《电镀污染物排放标准》(GB 21900-2008)中表2的标准,即COD≤80 mg/L、氨氮≤15 mg/L.     

水质安全的动态超声波强化混凝除藻水处理试验研究

超声波辐射能够破坏蓝藻气囊,在水处理工艺中达到强化蓝藻混凝沉淀的效果.然而不适当的超声处理会进一步破坏蓝藻细胞,导致胞内毒素大量释放,加重水质污染负荷.本研究为获得水质安全的超声波强化混凝沉淀蓝藻水处理方法,采用频率40~120 k Hz的超声波辐射蓝藻水,考察处理后蓝藻混凝沉淀去除效果及藻毒素释放情况.结果表明,频率68~120 k Hz、能量密度59.1~186.4 W·L-1的静态超声波作用10~15 s后进行混凝沉淀,藻类去除率达98%以上,且频率越高效果越好;然而各频率静态超声波作用5 s以上均会导致藻细胞内藻毒素释放.采用内衬吸声棉及动态超声方式,频率120 k Hz、能量密度38.5~196.6 W·L-1超声波作用7.5~30 s后,可避免胞内藻毒素释放,且能去除水中溶解性藻毒素18.7%~30.7%,混凝沉淀后藻类去除率97.0%以上,其它有机物也降低.     

MBR中水力条件对五孔中空纤维膜污染的研究

为了对五孔中空纤维膜在分置式膜生物反应器(MBR)处理模拟印染废水中膜污染特性进行研究,提出从水力学角度考察膜污染特性。在曝气强度分别为25,50,75,100 L/h,出水通量分别为9,12,15,18 L/(m2·h)的工况下考察膜污染表征系数跨膜压差(TMP)的变化情况。得出如下结论:出水通量稳定时,在一定范围内曝气强度的增加可使TMP的增长率降低,即延长膜稳定运行时间,有效缓解膜污染;在次临界通量下曝气量恒定时,出水通量越小,TMP的增长率越小,即膜的稳定运行时间越长。此实验结果对MBR中膜污染的有效控制和水力条件优化提供数据依据。     

微波-混凝处理高炉煤气洗涤水的实验研究

本文探索了微波作为辅助手段处理高炉煤气洗涤水过程中,微波辐射功率、微波辐射时间、聚合氯化铝(PAC)加入量、磷酸加入量对高炉煤气洗涤废水处理效果的影响。结果表明,微波和PAC混凝联用处理高炉煤气洗涤废水具有作用时间短、聚沉能力强等特点,可以有效去除废水中悬浮物,降低硬度及浊度。     

The Aging of America's Reservoirs: In‐Reservoir and Downstream Physical Changes and Habitat Implications

Reservoirs are important for various purposes including flood control, water supply, power generation, and recreation. The aging of America's reservoirs and progressive loss of water storage capacity resulting from ongoing sedimentation, coupled with increasing societal needs, will cause the social, economic, environmental, and political importance of reservoirs to continually increase. The short‐ and medium‐term (<50 years) environmental consequences of reservoir construction and operation are well known and include an altered flow regime, lost connectivity (longitudinal, floodplain), an altered sediment regime, substrate compositional change, and downstream channel degradation. In general, reservoir‐related changes have had adverse consequences for the natural ecosystem. Longer term (>50 years) environmental changes as reservoirs enter “old” age are less understood. Additional research is needed to help guide the future management of aging reservoir systems and support the difficult decisions that will have to be made. Important research directions include assessment of climate change effects on aging and determination of ecosystem response to ongoing aging and various management actions that may be taken with the intent of minimizing or reversing the physical effects of aging.     

Ozone concentrations, flux and potential effect on yield during wheat growth in the Northwest-Shandong Plain of China

Ozone (O₃) concentration and flux (F_o) were measured using the eddy covariance technique over a wheat field in the Northwest-Shandong Plain of China. The O₃-induced wheat yield loss was estimated by utilizing O₃ exposure-response models. The results showed that: (1) During the growing season (7 March to 7 June, 2012), the minimum (16.1 ppbV) and maximum (53.3 ppbV) mean O₃ concentrations occurred at approximately 6:30 and 16:00, respectively. The mean and maximum of all measured O₃ concentrations were 31.3 and 128.4 ppbV, respectively. The variation of O₃ concentration was mainly affected by solar radiation and temperature. (2) The mean diurnal variation of deposition velocity (V_d) can be divided into four phases, and the maximum occurred at noon (12:00). Averaged V_d during daytime (6:00–18:00) and nighttime (18:00–6:00) were 0.42 and 0.14 cm/sec, respectively. The maximum of measured V_d was about 1.5 cm/sec. The magnitude of V_d was influenced by the wheat growing stage, and its variation was significantly correlated with both global radiation and friction velocity. (3) The maximum mean F_o appeared at 14:00, and the maximum measured F_o was − 33.5 nmol/(m²·sec). Averaged F_o during daytime and nighttime were − 6.9 and − 1.5 nmol/(m²·sec), respectively. (4) Using O₃ exposure-response functions obtained from the USA, Europe, and China, the O₃-induced wheat yield reduction in the district was estimated as 12.9% on average (5.5%–23.3%). Large uncertainties were related to the statistical methods and environmental conditions involved in deriving the exposure-response functions.