Nitrifying population dynamics in a redox stratified membrane biofilm reactor (RSMBR) for treating ammonium-rich wastewater

Nitrogen removal performance and nitrifying population dynamics were investigated in a redox stratified membrane biofilm reactor (RSMBR) under oxygen limited condition to treat ammonium-rich wastewater. When the NH4+-N loading rate increased from 11.1±1.0 to 37.2±3.2 gNH4+-N·m-2·d-1, the nitrogen removal in the RSMBR system increased from 18.0±9.6 mgN·d^-1 to 128.9±61.7 mgN·d^-1. Shortcut nitrogen removal was achieved with nitrite accumulation of about 22.3±5.3 mgNO2--N·L-1. Confocal micrographs showed the stratified distributions of nitrifiers and denitrifiers in the membrane aerated biofilms (MABs) at day 120, i.e., ammonia and nitrite oxidizing bacteria (AOB and NOB) were dominant in the region adjacent to the membrane, while heterotrophic bacteria propagated at the top of the biofilm. Real-time qPCR results showed that the abundance of amoA gene was two orders of magnitude higher than the abundance of nxrA gene in the MABs. However, the nxrA gene was always detected during the operation time, which indicates the difficulty of complete washout of NOB in MABs. The growth of heterotrophic bacteria compromised the dominance of nitrifiers in biofilm communities, but it enhanced the denitrification performance of the RSMBR system. Applying a high ammonia loading together with oxygen limitation was found to be an effective way to start nitrite accumulation in MABs, but other approaches were needed to sustain or improve the extent of nitritation in nitrogen conversion in MABs.     

Toxicological impact of anilofos on some physiological processes of a rice field cyanobacterium Anabaena torulosa

This study deals with the toxicological impact of the herbicide anilofos on photosynthesis, respiration, nitrogen assimilation, and antioxidant system in a diazotrophic rice field cyanobacterium Anabaena torulosa. Treatment of anilofos (1.25, 2.5, and 5?mg?L^?1) affected growth, photosynthetic pigments, photosynthesis, and respiration of the cyanobacterium. Although all the photosynthetic pigments were affected, a maximum effect of the herbicide was observed on phycocyanin (51% reduction) followed by the carotenoids. The effect of the herbicide on photosynthetic pigments resulted in 57% decrease in photosynthetic O₂ evolution. Studies on the photochemical activity demonstrated that both photosystems (PS I and PS II) were affected by the herbicide. Decrease in the photosynthesis rate resulted in decreased nitrogen assimilation, as revealed by reduced nitrate (20%) and ammonium (26%) uptake and decreased activities of nitrogenase (63% decrease) and glutamine synthetase (22% decrease). This ultimately resulted in the reduced growth of the organism. Activities of superoxide dismutase, catalase, and peroxidase in the presence of anilofos increased by 1.8–3.5 times over control cultures. Proline content increased by 1.6 times, while the content of ascorbate decreased slightly. These results indicate that the organism was able to tolerate the herbicide stress by activating oxidative stress defense mechanism.     

1981~2010年深圳市不同等级霾天气特征分析

利用1981~2010年深圳市地面观测及空气质量监测资料,分析深圳不同等级霾天气的长期变化特征以及大气水平能见度、空气质量与霾的关系.结果表明:深圳霾日数总体呈增多趋势,强度增强,中度以上霾增多;各等级霾日数均呈增多态势,但不同等级霾日占年总霾日的比例变化趋势不同,轻微霾所占比例下降,轻度以上霾上升; 霾天气呈现冬季>秋季>春季>夏季的季节特征,但重度霾却是夏季最多; 霾导致大气水平能见度明显下降,霾日平均能见度较非霾日低6~7km,霾等级越高,能见度下降越明显,霾日能见度日变化幅度较非霾日小;霾日SO2、NO2浓度为非霾日的1.4~1.7倍,PM10是非霾日的2.2倍,大气颗粒物污染加剧可能是深圳能见度恶化、霾天气增多的一个重要原因;针对荔香站霾日SO2浓度日变化不明显,PM10 、NO2浓度呈双峰型分布,与上下班时段吻合,说明机动车的增加也是深圳霾天气增多的主因之一;霾等级越高,空气中PM10、SO2、NO2的浓度越高,从轻微到重度霾各级之间SO2、NO2和PM10浓度增幅大都在15%~20%.     

1980—2007年我国燃煤大气汞、铅、砷排放趋势分析

基于文献调研,对1980—2007年我国汞、铅、砷3种主要燃煤大气重金属排放清单进行归纳,计算了3种重金属的逐年平均排放量,并分析排放量与燃煤量的相关性、单位煤耗大气重金属污染物排放量的变化趋势及原因. 结果表明:1980—2007年我国燃煤大气汞、铅、砷排放量与燃煤量增长趋势基本一致,均呈显著正相关(R2分别为0.911、0.971、0.996),但燃煤大气汞排放量与燃煤量间的相关性却比铅、砷排放量与燃煤量的相关性小很多,这主要是燃煤电厂对汞协同脱除能力比对铅、砷强,以及电厂汞排放所占比例较大所致. 燃煤大气汞排放量在2005年后趋于稳定,而铅、砷排放量在2000年后快速增长,年均增速均超过10%,其中电厂和工业锅炉是重金属排放的重点行业. 在燃煤量不断增长的背景下,单位煤耗的大气汞、铅排放量均呈下降趋势,其中汞排放量在2005—2007年年均降低5.0%,铅排放量在1996—2007年年均降低1.7%. 这与我国主要燃煤行业除尘、脱硫、脱硝等大气污染控制装置对重金属的协同脱除能力不断增强有密切关系.      

洞庭湖沉积物不同形态氮赋存特征及其释放风险

为了揭示湖泊沉积物中氮的空间分布特征及其释放风险,采用连续分级提取法研究了洞庭湖表层沉积物中EN(可交换态氮)、HN(酸解态氮)及NHN(非酸解态氮)的赋存特征;同时,结合BN(生物可利用态氮)的含量和释放通量的大小,探讨了各形态氮对BN的贡献及与释放通量的相关关系. 结果表明,受水动力和湖盆地形的影响,沉积物中各形态氮含量空间差异较大. 全湖w(TN)在735.91~2846.51mg/kg之间,平均值为1371.85mg/kg,东洞庭湖、西洞庭湖、南洞庭湖、洞庭湖出口w(TN)的平均值分别为1513.43、1173.14、1262.76和1363.31mg/kg. 从各形态氮含量占w(TN)的比例来看,w(HN)最高,平均占66.74%;其次是w(NHN),平均占21.46%;w(EN)最小,仅占11.80%. 东洞庭湖、西洞庭湖、南洞庭湖、洞庭湖出口w(BN)的平均值分别为189.31、170.16、152.87和139.51mg/kg,其值大小主要受w(EN)和w(HN)的影响. 东洞庭湖、西洞庭湖、南洞庭湖、洞庭湖出口沉积物中NH₄+-N释放通量的平均值分别为6.32、7.03、7.78和146.96mg/(m2·d),沉积物中NH₄+-N释放通量主要受EN控制,其中尤其受可交换态NH₄+-N的控制,而沉积物中的HN和TN尚不是影响沉积物氮释放的主要因素.      

我国七个站点降雨和森林穿冠水中硝态氮同位素丰度

采集了我国7个站点的降雨和森林穿冠水样品,分析测定了水样中硝态氮和总氮的同位素丰度.降雨中硝态氮δ15N值范围为-9.00‰至9.71‰,其中北方站点冬季降雨中硝态氮δ15N值要远高于其他站点,可能是由于北方冬季燃煤供暖所致.穿冠水中硝态氮δ15N值范围为-16.59‰至-0.32‰,比降雨中的硝态氮δ15N值要低,其可能原因是林冠层中存在硝态氮的交换过程,从而产生了分馏作用.降雨和穿冠水中TN的δ15N值范围分别为-7.94‰至-3.07‰和-4.55‰至-1.73‰,其中穿冠水中TN的δ15N值要略高于降雨中的值.     

大气颗粒物吸湿性研究

大气颗粒物吸湿性是反映颗粒物理化性质的重要指标,吸湿性研究对深入了解颗粒物的环境和健康效应具有重要意义. 总结了国外近年来大气颗粒物吸湿性研究进展:①典型的大气颗粒物吸湿性分析方法为H-TDMA(吸湿性串联差分电迁移率粒径分析仪)系统及其优化方法. ②大气颗粒物吸湿性呈单峰、双峰甚至多峰分布;根据G_f(吸湿性生长因子)随粒径变化的模式,可将大气颗粒物分为强吸湿性和弱吸湿性2类,也可分为纯不溶性、混合不溶性、混合可溶性和纯可溶性4类. ③城市背景点颗粒物的G_f比城市观测点高;城市观测点的颗粒物G_f分布呈夏季高、冬季低,白天高、晚上低的特征. ④颗粒物吸湿性与其化学组成和形态密切相关,纯可溶性盐颗粒物的G_f通常较高. ⑤柴油燃烧源新排放的颗粒物属于弱吸湿性颗粒物,G_f非常小,但在其表面老化后或随燃料中硫含量的增加G_f会明显变大. ⑥生物质燃烧排放颗粒物的G_f相对较高,但存在区域差异性. 针对国内大气颗粒物吸湿性研究现状,提出了未来重点研究方向.      

洱海表层沉积物中总氮含量及氨氮的释放特征

通过现场调查和室内模拟试验,对洱海具有代表性的9个表层沉积物样品中w(TN)的分布特征以及沉积物中NH₄+-N释放动力学特征进行了研究. 结果表明,洱海表层沉积物中w(TN)在2.0844～6.5153g/kg之间,平均值为3.5378g/kg,北部西岸为高值区,南部(靠近大理市)为次高值区. 一级动力学模型可很好地拟合洱海表层沉积物NH₄+-N释放动力学特征,NH₄+-N最大释放量在0.1209～0.2810g/kg之间;释放主要集中在0~5min内,约占最大释放量的68%~83%;随后释放速率逐渐放缓,到120min后基本达到释放平衡.运用无限稀释法对沉积物NH₄+-N释放潜能进行测定表明,洱海沉积物NH₄+-N释放潜能在1.7001~3.5879 g/kg之间,在水土质量比约为2500时,NH₄+-N释放量达到最大,随后释放逐渐趋于平衡. 洱海沉积物NH₄+-N释放潜能及最大释放量均与其w(TN)呈显著正相关. 洱海沉积物中w(TN)与NH₄+-N释放潜能和最大释放量均高于长江中下游湖泊,具有较大的氮释放风险.      

液氮冻融破碎生物污泥制备生物絮凝剂

利用城市剩余生物污泥,采用液氮冻融破碎、提取液提取的方法制备了生物污泥絮凝剂。对絮凝剂的制备条件及其絮凝性能进行了研究,结果表明:采用液氮冻融破碎,pH为1.0的稀盐酸溶液作为提取液提取所制备的絮凝剂,对高岭土悬浮液的絮凝效率可达98.5%。液氮冻融破碎的次数对絮凝剂制备没有明显影响。同时考察了絮凝剂投加量以及絮凝体系的pH对絮凝剂絮凝活性的影响。