应用分子生物学与同位素示踪技术研究厌氧氨氧化菌活性及功效

厌氧氨氧化是一个新发现的氮循环途径,与反硝化作用都产生氮气,但准确衡量厌氧氨氧化活性及功效的相关方法还是个难题.本研究联合应用分子生物学与同位索示踪技术,以北京某污水处理厂的活性污泥为实验样品,研究其中厌氧氨氧化菌的存在、活性和功效.厌氧氨氧化菌的分子生物学分析是通过16S rRNA进行,选择两步引物分别为pla46-...     

猪粪秸秆高温堆肥过程中碳氮转化特征与堆肥周期探讨

将猪粪与秸秆以7：1（质量比,以鲜重计）的比例,在自制的强制通风静态堆肥反应箱中进行高温堆肥试验,研究了堆肥过程中碳氮转化特征及其腐熟时间.同时,在堆制的23d中,根据堆温变化采样6次,分析了堆肥样品中各种氮素和碳素含量及其它性质的变化情况.结果表明：堆肥结束时,硝态氮含量增加了103.0%,铵态氮、有机氮、总氮含量分...     

日本森林大气中过氧化物的浓度及其对森林植物的影响

为了研究森林衰退的原因,于2000,2001和2002年的8月,分别选择出现森林衰退的日本奥日光白根山落叶树森林和未出现森林衰退的长野县大芝高原红松森林设立监测点,对光化学氧化剂臭氧(O3)和过氧化物的浓度进行监测,同时利用人工气候室对森林植物山毛榉和白桦进行了50′10-9O3、100′10-9O3和50′10-9O3+2′10-9~3′10-9过氧化物(过氧化氢(H2O2)及甲基过氧化氢(MHP))的暴露实验.野外监测结果表明,监测期间奥日光和长野的O3平均浓度相同,奥日光的H2O2及MHP平均浓度均高于长野;大气中的H2O2和MHP总是与O3共存,并且其浓度随O3浓度的增加而增加.暴露实验结果表明,暴露于50′10-9O3+2′10-9~3′10-9过氧化物的山毛榉和白桦出现了不同于O3暴露的叶片伤害症状;与100′10-9O3相比,50′10-9O3+2′10-9~3′10-9过氧化物导致植物出现了严重的叶片伤害和显著的光合速率下降.研究结果表明,除O3外,大气中的过氧化物也是导致森林衰退的原因之一.     

钢铁行业大气环境影响评价方法与建议

按钢铁行业大气环评报告书的结构和顺序,结合HJ 2.2-2008《环境影响评价技术导则大气环境》中的相关技术要求,从评价因子、源强、评价等级、大气监测、大气预测、防护距离等方面出发,分析了钢铁行业大气环评中的评价等级确定、大气监测、大气预测等工作中存在的问题,并提出解决方案和建议对策。     

碳氮比对废水好氧脱氮中含氮气态产物的影响

针对目前人们对好氧脱氮中气态产物认识不清的问题,采用SBR反应器,以人工配制的NO3--N废水为处理对象,对影响好氧脱氮的COD/N进行了深入研究,测定了三种主要含氮气态产物(NO、NO2、N2O),揭示了好氧状态下生物脱氮的途径和机理。通过对COD/N分别为9、12、15、18的系统氮元素的全程跟踪测定,得到系统内各含氮化合物的变化规律。结果表明,三种气体的产生同COD/N有着密切的关系,低C/N会导致NO、NO2和N2O的积累,最多达总脱氮量的9%。研究结果还表明当进水COD/N为15时,既保证了良好的脱氮效果且抑制了NO、NO2、N2O三种有害气体的大量产生。     

供碳源载体及其在低碳氮比污水处理中的应用研究

为解决低C/N污水的脱氮问题,本实验自行研制开发了一种新型碳聚合物载体.对该载体进行低C/N污水的生物膜脱氮研究,考察了HRT、pH、DO、温度等因素对系统同步硝化反硝化脱氮效果的影响.结果表明:在C/N比为4、pH=8、DO=1 mg/L、HRT=6 h,T=24℃的条件下,氨氮及总氮的去除率分别可以达到90%和70...     

Seasonal and diurnal variations of atmospheric peroxyacetyl nitrate, peroxypropionyl nitrate, and carbon tetrachloride in Beijing

Atmospheric peroxyacetyl nitrate(PAN), peroxypropionyl nitrate(PPN), and carbon tetrachloride(CCl4) were measured from September 2010 to August 2011 in Beijing. PAN exhibited low values from mid-autumn to early spring(October to March) with monthly average concentrations ranging from 0.28 to 0.73 ppbV, and increased from early spring to summer(March to August), ranging from 1.37–3.79 ppbV. The monthly variation of PPN was similar to PAN, with low values(below detection limit to 0.18 ppbV) from mid-autumn to early spring, and a monthly maximum in September(1.14 ppbV). The monthly variation of CCl4was tightly related to the variation of temperature, exhibiting a minimum in winter(69.3 pptV) and a maximum of 180.6 pptV in summer. Due to weak solar intensity and short duration, PAN and O3showed no distinct diurnal patterns from morning to night during winter, whereas for other seasons, they both exhibited maximal values in the late afternoon(ca. 15:00 to 16:00 local time) and minimal values during early morning and midnight. Good linear correlations between PAN and PPN were found in autumn(R = 0.91), spring(R = 0.94), and summer(R = 0.81), with slopes of 0.130, 0.222, and 0.133, respectively, suggesting that anthropogenic hydrocarbons dominated the photochemical formation of PANs in Beijing. Positive correlation between PAN and O3 in summer with the low slopes( O3 / PAN) ranging from 9.92 to 18.0 indicated serious air pollution in Beijing, and strong negative correlation in winter reflected strong O3consumption by NO titration and less thermal decompositin of PAN.     

Characteristics of atmospheric particles and heavy metals in winter in Chang-Zhu-Tan city clusters, China

To understand the pollution characteristics of atmospheric particles and heavy metals in winter in Chang-Zhu-Tan city clusters, China, total suspended particulate(TSP) and PM10samples were collected in cities of Changsha, Zhuzhou and Xiangtan from December 2011 to January 2012, and heavy metals of Cd, Pb, Cr, and As were analyzed. It shows that the average TSP concentration in Changsha, Zhuzhou and Xiangtan were(183 ± 73),(201 ± 84) and(190 ± 66) μg/m3respectively, and the average PM10 were(171 ± 82),(178 ± 65) and(179 ± 55) μg/m3respectively. The lowest TSP and PM10concentrations occurred at the background Shaping site of Changsha. The average ratio of ρ(PM10)/ρ(TSP) was 91.9%, ranging from 81.3% to 98.9%. Concerning heavy metals, in TSP samples, the concentration of Cr, As, Cd and Pb were 28.8–56.5, 18.1–76.3, 3.9–26.1 and 148.0–460.9 ng/m3, respectively, while in PM10samples, were 16.4–42.1, 15.5–67.9, 3.3–22.2 and 127.9–389.3 ng/m3, respectively. The enrichment factor of Cd was the highest, followed by Pb and As, while that of Cr was the lowest.     

SBR法处理低C/N污水的工程应用——以某基地污水处理站改造工程为例

低C/N污水的生化处理过程中,由于碳源不足,不能满足硝化和反硝化的要求,造成出水NH3-N超标。采用SBR工艺对某基地污水处理站厌氧处理后的低C/N污水进行改造,处理后出水COD去除率达到97%以上,NH3-N去除率达到93%以上。     

汉江上游金水河流域氮湿沉降

汉江上游金水河流域是南水北调工程的重要水源涵养区,但是氮污染已成为该流域水质的主要威胁因素.该研究对汉江的金水河流域开展了为期1 a(2012-02~2013-02)的氮湿沉降观测,并利用氮输出模型估算了氮湿沉降对河流氮负荷的贡献量.结果表明雨水中总氮(DTN)的浓度在0.24~2.89 mg·L-1之间,铵态氮(NH+4-N)、硝态氮(NO-3N)及有机氮(DON)分别占42.8%、13.3%和43.9%;雨水氮浓度随降雨量增大而变小,明显受到降雨的稀释作用.流域内氮湿沉降主要来自人类活动,沉降负荷在4.97~7.00 kg·(hm2·a)-1之间,受降雨量的主要影响,上游地区的氮湿沉降负荷>下游地区>中游地区,春夏两季约占全年氮湿沉降的81%.流域氮湿沉降对河流氮负荷贡献量约为34 000~46 000 kg,只占流域氮肥贡献量的5.05%~6.78%,远小于流域内农业活动化肥氮的贡献量,不是河流氮的主要来源.