东江流域水污染控制与水生态系统恢复技术与综合示范

归纳了水专项东江项目2008—2013年的主要研究成果:针对保护优质水源的国家需求,选择典型的东江流域开展前瞻性的水污染控制技术研发并进行工程示范,创建了由常规水质指标实时在线化,痕量污染物控制指标识别筛选全流域优化,生物毒性指标甄别多属性全程化等成套技术构成的水源流域水质风险识别技术体系;由各类工艺废水脱毒减害,同质污水区域集中强化处理,排水持续净化等成套技术构成的水环境风险控制工程技术体系;由水生物链各物种生长状况评级,生境恢复和物种受损关键环节恢复等成套技术构成的生态健康维护技术体系。集成以上3个技术体系形成成套的流域水环境风险控制技术体系集。基于上述技术创新提出了“控制风险、维护生态、保水甘甜、发展持续”的水源流域管理创新总体策略。研发的技术体系与策略在东江流域的示范与应用,实现了东江主干流水质常年优于Ⅱ类的污染控制目标。     

氯自由基介导的BDD电极选择性氧化脱氮

为实现氨氮的高效选择性转化,设计了一个氯自由基介导的电化学体系。该电化学体系以稳定性好、氧化能力强的掺硼金刚石(BDD)电极为阳极,以Pd-Cu修饰的泡沫镍材料(Pd-Cu/NF)为阴极,以氯化钠为电解质,对BDD电极选择性电催化氧化性能与机理进行了研究。结果表明：在4.0 V电压下,体系中的Cl⁻原位可转化成氯自由基(Cl·),Cl·可选择性地将氨氮转化为N₂和少量$ {\rm{NO}}_3^ - $,副产物$ {\rm{NO}}_3^ - $在Pd-Cu/NF阴极被高效还原为N₂;分别探究了阴极材料、电场强度、电极间距、溶液pH和电解质种类对氨氮转化性能的影响。通过电子顺磁共振和自由基捕获实验,证实了Cl·在氨氮转化过程中发挥了重要作用。在最优条件下,可实现40 min内100%的氨氮转化率和25 mg·L⁻¹的N₂生成量,以上研究结果可为解决水体中氨氮的污染问题提供参考。     

高氨废水自养半亚硝化过程N2O释放特性

接种普通活性污泥,以人工配制高氨废水为基质。在SBR中通过逐步提高进水氨氮浓度并控制低溶解氧的方法,经过58 d连续运行使出水NO2--N/NH4+-N维持在0.88~1.25,成功实现了半亚硝化的启动。通过对典型周期内氮素转化及N2O释放特性的考察表明:周期内DO浓度基本维持在0.4 mg/L以下,NH4+-N浓度由410.46 mg/L下降至257.26 mg/L。NO2--N浓度由162.90 mg/L升高至295.80 mg/L,NO3--N浓度由27.01 mg/L逐渐升高至50.16 mg/L。pH先由7.94升高到8.01后缓慢降至7.96,溶解性N2O浓度基本维持在0.07 mg/L。初期(0~20 min)气态N2O浓度由0.13 mg/L迅速升至1.13 mg/L后急剧下降到0.34 mg/L,随后缓慢升至0.54 mg/L。初期N2O的平均释放速率高达0.84 mg/min,这主要是上周期沉淀阶段产生并附着在污泥中的N2O受曝气吹脱所致。     

地铁多线换乘车站火灾模型实验研究—(1)模型装置设计

为研究地铁网络化运营枢纽车站火灾烟气扩散特征和防排烟技术,根据工程资料和标准规范对典型多线换乘车站进行1∶10火灾实验模型设计,并依据设计方案完成车站模型主体结构和通风排烟系统的搭建,同时在各个防烟分区设计安装温度、流速、烟气浓度和热辐射测量装置,可实现对“T”形、“十”形和“L”形换乘等不同换乘形式车站的火灾场景模拟和危险参数测量。研究结果表明:该模型装置能够开展一系列针对不同换乘形式和通风模式的火灾实验,对于全面揭示大型换乘车站火灾烟气运动规律、验证并优化火灾防排烟设计方法、支撑复杂结构枢纽车站火灾烟气控制技术具有重要意义。     

垃圾填埋场地下水污染修复技术优选研究

结合国内外地下水污染场地的修复经验,综合考虑当地社会经济条件、地下水脆弱性、污染物特征等因素,采用层次分析法建立了修复技术优化指标体系;在此基础上运用多准则决策分析模型(MCDA)进行地下水污染修复技术优选排序,构建垃圾填埋场地下水污染修复技术筛选模型;并以湖北省某简易垃圾填埋场为例进行应用研究。结果表明:在备选的5种场地地下水修复技术(监测自然衰减技术、渗透反应格栅、多相抽提技术、抽出-处理技术、原位微生物修复技术)中,抽出-处理技术、原位微生物修复技术较为理想。综合考虑该污染场地条件、地下水污染治理要求及附近受体分布情况,得到最佳修复方案为:高污染风险区域采用抽出-处理技术和原位微生物修复技术组合;低污染风险区域采用监测自然衰减技术。     

3种环保型淋洗剂对重金属污染土壤的淋洗效果

采用振荡淋洗法研究衣康酸(IA)、丙烯酸-2-丙烯酰胺-2-甲基丙磺酸共聚物(AA/AMPS)和衣康酸-丙烯酸共聚物(IA-AA)在不同因素影响下对污染土壤Cd、Pb和Zn的淋洗效率。结果表明：3种淋洗剂对土壤Cd、Pb和Zn的去除率随其浓度增加而快速上升,随pH增加呈迅速下降和先升高后降低2种趋势,随淋洗时间总体呈上升趋势;3种淋洗剂在浓度为0.15 mol·L-1且pH为3时,对Cd和Zn去除率最高（39.34%~65.65%）;在相同浓度和pH为5条件下对Pb的去除率最高（22.05%~50.62%）。其中IA-AA对Cd、Pb和Zn的去除率分别可达65.65%、50.62%和44.92%。它们去除的主要重金属组分为酸溶态、可还原态和部分可氧化态,且经IA和IA-AA淋洗的土壤养分损失相对较小。因此,IA-AA是修复Cd、Pb和Zn复合污染土壤有工程应用前景的淋洗剂。     

泡膜式介质阻挡放电等离子体去除模拟生产废水中的四溴双酚S

为了有效的降解生产废水中的四溴双酚S(TBBPS),采用泡膜式介质阻挡放电等离子体处理装置,研究了放电等离子体对TBBPS降解的影响。分别探讨了放电电压、空气流量、液体流量、活性物质抑制剂对TBBPS降解效果的影响;考察了降解过程中pH、电导率、COD和生物毒性的变化。结果表明,在放电电压为12.5 kV、空气流量为1.8 L·min⁻¹、液体流量为150 mL·min⁻¹时,处理9 min后其TBBPS去除率达到95 %以上;活性物质抑制剂对TBBPS的降解有一定的抑制作用,活性物质$ \cdot {\rm{O}}_2^ - $是反应体系中的主要活性物质;在降解过程中,pH不断下降,电导率不断上升,COD先升高后降低,生物毒性呈下降趋势。紫外-可见分光光度计全波扫描结果表明,TBBPS对应的特征吸收峰随处理时间变小,表明等离子体处理会破坏TBBPS的结构。以上研究结果可为TBBPS的有效降解提供参考。     

Pollution sources identification of polycyclic aromatic hydrocarbons of soils in Tianjin area, China

A total of 188 surface soil samples were collected from different types of utilization soils in Tianjin area. Factor analysis and scatter point surface tension spine function interpolation were used to analyze types and spatial distributions of PAH sources of surface soils in Tianjin area. The results showed that most pollution sources were mixed sources including coal burning and petroleum spill. Mixed sources occupied 56.12%, 58.96%, 46.45% and 59.50% in farmland of wastewater irrigation, common farmland, wild land and city greenbelt, respectively. Other pollution sources such as vehicle emission, biogenic conversion, wood burning and natural gas combustion were also significant. The spatial distributions of pollution sources were closely related to geographic location, geographic condition and living habit of indigenes.     

磁分离技术在我国废水处理中的研究进展

本文介绍了磁分离技术的基本原理、分离方法和设备，综述了该技术在某些特定废水处理中的应用现状。磁分离技术的实际应用具有分离效率高、分离速度快、选择性好、处理对象广、成本低廉、分离物系的粒度可达到很小，并且不受处理体系的温度、密度、酸碱度限制等优点，可以使某些采用传统分离方法较难或不能分离的物系得以顺利地分离，有较为广泛的应用前景。     

Reef coral reproduction in the eastern Pacific: Costa Rica, Panamá and Galápagos Islands (Ecuador). IV. Agariciidae, recruitment and recovery of Pavona varians and Pavona sp.a

The reproductive ecology of two eastern Pacific zooxanthellate coral species was examined as part of a continuing series of studies relating bleaching/mortality events caused by the El Niño–Southern Oscillation disturbance, and is described for study sites in Costa Rica, Panamá, and the Galápagos Islands (Ecuador). This study deals with the sibling agariciid species Pavona varians and Pavona sp.a over a 13?yr period (1985 to 1997). Both Pavona species are broadcast-spawners with some gonochoric, but mostly sequential hermaphroditic colonies. Minimum colony sizes (and ages) at first reproduction were 5?cm (5?yr) and 3?cm (2 to 3?yr), respectively, in P. varians and Pavona sp.a. In the Panamá and Galápagos populations, gonochoric colonies spawn eggs or sperm at least monthly. Six fecundity attributes were not significantly different in the two species, but the eggs of P. varians are white to beige and positively buoyant, and those of Pavona sp.a are dark green and neutrally to negatively buoyant. Eggs of both species lack zooxanthellae. Both species are reproductively active year-round, with maximum activity in the dry season in the nonupwelling Gulf of Chiriquí, and in the wet season in the upwelling Gulf of Panamá. Spawning is predominantly during full moon, and possibly also at new moon at most study sites. Spawning in P. varians and Pavona sp.a is 12?h out of phase, with the former species spawning ～1?h before sunrise and the latter about 1?h after sunset. The fecundity of Pavona spp. at Caño and the Galápagos Islands was much greater (19?900 to 27?900 eggs cm^?2?yr^?1) than at all Panamá sites (14?800 to 19?800 eggs cm^?2?yr^?1). Intraspecific crosses in both species resulted in swimming planula larvae after 25 to 36?h. Recruitment of P. varians was highest in Panamá, moderate in Costa Rica, and nil in the Galápagos Islands, matching, respectively, the contributions of P. varians to the pre-1982/1983 El Niño coral-population abundances in these areas. Recruitment success of P. varians at Uva Island was significantly related to maximum monthly positive sea surface-temperature (SST) anomalies that occurred in the year preceding recruitment over the period 1982 to 1996; recruitment failed when SST anomalies exceeded 1.6 to 1.9?C° during the severe ENSO events of 1982/1983 and 1997/1998.