RPB-O3/H2O2法处理硝基苯模拟废水

在超重力场中,研究了硝基苯模拟废水的臭氧/双氧水(O3/H2O2)法处理效果,考察了超重力因子β、H2O2浓度、初始p H、液体流量及处理时间等因素对硝基苯去除率的影响。结果表明,硝基苯去除率随超重力因子β和处理时间的增加而增大,而随H2O2浓度、初始p H和液体流量的增加呈先增大后降低的趋势。当硝基苯初始浓度300 mg/L,工艺条件β=80、p H=10.0、臭氧质量浓度约为40 mg/L、H2O2浓度为4.9 mmol/L、液体流量为120 L/h时,循环处理35 min硝基苯去除率可达96.7%。处理时间60 min后,废水中硝基苯含量1.4 mg/L,COD为39 mg/L,达国家一级排放标准(GB 8978-1996)。在此条件下,硝基苯的降解过程符合准一级反应动力学。     

前置反硝化曝气生物滤池的挂膜启动研究

为了解前置反硝化曝气生物滤池(BAF)的启动规律,构建了小试规模的前置反硝化BAF,采用快速排泥、逐步增大水力负荷的策略考察了其启动过程中的污染物去除情况及启动特性。结果表明,在好氧柱水力负荷为2.04 m3/(m2·h),厌氧柱水力负荷为4.08 m3/(m2·h),回流比为100%,气水比为5.6∶1的情况下,前置反硝化BAF的启动需要49 d。启动过程中好氧池中硝化细菌的成熟是启动的关键。厌氧池中的反硝化细菌的成熟标志着启动的完成。启动完成后,前置反硝化BAF的出水COD、NH3-N及NO-3-N分别稳定在50、15和5 mg/L以下,满足国家一级A排放标准。     

煤粉炉掺烧干化污泥的污染物排放研究

结合某电厂420 t/h四角煤粉炉掺烧污泥项目的实验室分析测试,了解煤粉掺烧不同含水率不同比例的干化污泥条件下烟气中污染物和灰渣中重金属的排放特性。结果表明,在实验研究配比和燃烧的条件下,大部分重金属元素Pb、Cu、Cr和Ni残留在灰渣中,Zn、Cd部分残留在灰渣中,As、Hg和Se等易挥发元素释放到烟气中,在灰渣中的含量很小。掺烧污泥后,灰渣中的重金属含量较单烧单煤都有了一定幅度的升高,Zn的含量是单煤的2倍,其余重金属是单煤的1.1~1.2倍。3种不同的掺混比例之间的污染气体排放浓度基本相似。烟气中主要污染物及重金属浓度可以满足现行国家标准。与单烧单煤相比,CO、HCl以及其他有机气体排放浓度基本相同;NH3的排放浓度较单煤有所升高;SO2、NOx和CO2排放浓度略有降低;飞灰浓度有所升高。烟气中的重金属,Hg含量升高了30%,Pb含量约为单煤的4.3~4.8倍。以上研究结果可为环保达标和飞灰利用提供基础数据。     

中国春季降水与南印度洋偶极子的关系研究

利用美国国家海洋和大气管理局海温资料和1951~2010年中国160站月降水量资料,分析了前期冬季（12~2月）印度洋海表温度与中国160站春季降水的关系及其影响机制。研究表明：冬季印度洋海温异常的空间模态主要有两种：符号一致的单极和东、西符号相反的南印度偶极。将第2模态的时间系数定义为南印度洋偶极子指数。该指数与中国次年春季降水关系较好,并利用NCEP/NCAR再分析资料进行机制分析,发现主要南印度洋偶极子通过以下途径影响中国春季降水：中高纬,SIOD的影响主要引起低纬度的海温及对流异常,通过中低纬度间的相互作用,在中高纬产生较强的遥响应,从而影响同期冬季欧亚大陆的环流变化,这种扰动在西风气流的作用下引起后期春季北太平洋地区对流活动异常,通过中低纬度间的相互作用,加强中高纬地区的遥响应,表现为欧亚大陆EUP波列;低纬,SIOD的影响主要引起南海-海洋性大陆的海温及对流异常,引发经向环流异常,导致黄河至长江中下游地区垂直运动异常和气流辐合异常     

Estimating and comparing greenhouse gas emissions with their uncertainties using different methods: A case study for an energy supply utility

Energy supply utilities release significant amounts of greenhouse gases (GHGs) into the atmosphere. It is essential to accurately estimate GHG emissions with their uncertainties, for reducing GHG emissions and mitigating climate change. GHG emissions can be calculated by an activity-based method (i.e., fuel consumption) and continuous emission measurement (CEM). In this study, GHG emissions such as CO₂, CH₄, and N₂O are estimated for a heat generation utility, which uses bituminous coal as fuel, by applying both the activity-based method and CEM. CO₂ emissions by the activity-based method are 12–19% less than that by the CEM, while N₂O and CH₄ emissions by the activity-based method are two orders of magnitude and 60% less than those by the CEM, respectively. Comparing GHG emissions (as CO₂ equivalent) from both methods, total GHG emissions by the activity-based methods are 12–27% lower than that by the CEM, as CO₂ and N₂O emissions are lower than those by the CEM. Results from uncertainty estimation show that uncertainties in the GHG emissions by the activity-based methods range from 3.4% to about 20%, from 67% to 900%, and from about 70% to about 200% for CO₂, N₂O, and CH₄, respectively, while uncertainties in the GHG emissions by the CEM range from 4% to 4.5%. For the activity-based methods, an uncertainty in the Intergovernmental Panel on Climate Change (IPCC) default net calorific value (NCV) is the major uncertainty contributor to CO₂ emissions, while an uncertainty in the IPCC default emission factor is the major uncertainty contributor to CH₄ and N₂O emissions. For the CEM, an uncertainty in volumetric flow measurement, especially for the distribution of the volumetric flow rate in a stack, is the major uncertainty contributor to all GHG emissions, while uncertainties in concentration measurements contribute a little to uncertainties in the GHG emissions.

Implications:Energy supply utilities contribute a significant portion of the global greenhouse gas (GHG) emissions. It is important to accurately estimate GHG emissions with their uncertainties for reducing GHG emissions and mitigating climate change. GHG emissions can be estimated by an activity-based method and by continuous emission measurement (CEM), yet little study has been done to calculate GHG emissions with uncertainty analysis. This study estimates GHG emissions and their uncertainties, and also identifies major uncertainty contributors for each method.     

人工湿地基质对NH4＋-N吸附性能

为研究建筑废物红砖和工业废物煤渣用作人工湿地脱氮基质的可行性,分别通过静态吸附实验和动态NHf—N去除效果实验进行考察。结果表明,红砖和煤渣对NH4＋-N最大静态吸附量分别为0．2533mg／g和0．0533mg／g,其吸附等温曲线均符合Freundlich型吸附方程,吸附常数分别为0．0419和0．0091;红砖煤渣组合对污水中NH4＋-N平均动态脱除率达到41．18％,高于红砖的37．63％和煤渣的30．92％。     

添加天然沸石和石灰对土壤镉形态转化的影响

采用土壤培养实验,研究镉污染土壤中添加沸石、石灰及两者配施对土壤pH值和土壤镉形态变化的影响。结果表明,土壤pH值随沸石用量的增加而增加,随培养时间呈现先增加后下降并逐渐趋于稳定的趋势,但均高于对照。高剂量石灰的处理对土壤pH的影响最大,与对照相比土壤pH提高了3.33个单位。在土壤5~50 d培养过程中,石灰处理的土壤交换态镉含量呈现先逐渐降低而后略有升高的趋势,其余处理均呈下降趋势。培养50 d后,高剂量的沸石、石灰及高剂量沸石与石灰配施处理的土壤交换态镉含量从5 d时的67.54、61.95和55.56 mg/kg降低至54.65、49.93和45.96mg/kg。相关分析表明,不同培养时期交换态镉含量与土壤pH值呈负相关关系。在10个处理中,L2Z3(石灰2 g/kg土和沸石60 g/kg土)组合处理效果最好,使土壤交换态镉含量下降了34.68%,碳酸盐结合态镉含量上升了4.30%,铁锰氧化结合态镉含量上升了16.97%,有机结合态镉含量上升了1.31%,残渣态镉含量上升了12.11%。     

Comparison of lignin peroxidase and horseradish peroxidase for catalyzing the removal of nonylphenol from water

Concentrations of aqueous-phase nonylphenol (NP), a well-known endocrine-disrupting chemical, are shown to be reduced effectively via reaction with lignin peroxidase (LiP) or horseradish peroxidase (HRP) and hydrogen peroxide. We systematically assessed their reaction efficiencies at varying conditions, and the results have confirmed that the catalytic performance of LiP toward NP was more efficient than that of HRP under experimental conditions. Mass spectrum analysis demonstrated that polymerization through radical–radical coupling mechanism was the pathway leading to NP transformation. Our molecular modeling with the assistance of ab initio suggested the coupling of NP likely proceeded via covalent bonding between two NP radicals at their unsubstituted carbons in phenolic rings. Data from acute immobilization tests with Daphnia confirm that NP toxicity is effectively eliminated by LiP/HRP-catalyzed NP removal. The findings in this study provide useful information for understanding LiP/HRP-mediated NP reactions, and comparison of enzymatic performance can present their advantages for up-scale applications in water/wastewater treatment.     

中国陆上油藏CO2封存潜力评估

CO2捕集与封存是减缓气候变化的一种关键的碳减排选择方案。将CO2注入油藏作为一种碳埋存方式引起广泛关注。作为判断某一国家、某一区域或某一具体储层是否适合CO2地质封存开展的重要依据之一,有必要在规划碳捕集与封存(CCS)项目前,对潜在的封存库进行封存潜力评估。本文在已有可公开的地质资料的基础上,评估了中国陆上216个油田实施CO2地质封存的潜力,并与相关研究结果进行了比较。结果表明:在满足埋存深度大于800 m的筛选条件下,当假设我国陆上油田全部用于CO2-EOR时,CO2封存潜力约3.6 Gt;当陆上油田全部视为废弃油藏处理时,CO2理论封存潜力约4.6 Gt。其中,东北和华北地区油藏封存CO2潜力巨大,占陆上油田CO2封存总量的60%以上;同时这里CO2集中排放源分布密集,排放源和封存地间的匹配性良好,可以减少CO2运输和封存成本。在这两个地区可以优先考虑实施油藏封存CO2项目。     

基于WebGIS三峡干流水质模拟平台研究

三峡蓄水成库后仍属于典型的河道型水库,其总体水流、水质运动特性符合一维水流水质运动规律。针对三峡库区总体水流、水质运动特性,采用一维水流水质模型对三峡库区水流和水质进行了模拟。以该模型为核心,利用Web Services技术开发并在互联网上发布了模型服务,在此基础上采用成熟的WebGIS和富客户端Flex等技术构建了适用于三峡库区的干流水质模拟平台;能够实现包括各计算断面流速、流量、水位以及污染物浓度时空过程在内的三峡库区干流流速场和浓度场的数值模拟。以库区干流清溪场至十里铺断面内的江段作为模拟实例,利用该平台模拟计算江段内水流和水质状况,并以水文水质同步观测数据对模拟结果进行验证,结果表明其具有较好的模拟效果;为三峡库区污染物总体输移扩散特性研究提供了有利工具,同时也为国家和地方政府进行库区水环境决策提供了技术支持