徐州市气象因子与空气质量和PM_（10）浓度的相关性分析

通过对徐州市空气质量及其对应的气象因子进行统计分析,得出空气质量与相对湿度、风速,降水等气象因子的关系。分析特殊气象天气出现时空气中主要污染物PM10的变化规律.得到一些初步结果,为减轻和防止污染提供参考。     

基于形态与in vitro方法的铬污染土壤生物可给性研究

铬（Cr）是电镀类场地的主要污染物.开展土壤中Cr（III）和Cr（VI）的生物可给性研究对于准确评估Cr污染场地风险,克服污染场地过度修复问题十分关键.本研究采集我国栗钙土、红壤、潮土3种典型土壤,通过添加相同浓度污染物的方式制备成Cr（III）或Cr（VI）污染土壤.随后利用5种体外方法（in vitro）,对3种土壤经口摄入的Cr生物可给性进行比较与健康风险评估.进而从土壤理化性质、Cr赋存形态、土壤矿物组成方面,对不同土壤在溶解度生物可给性研究联盟（SBRC）方法中的生物可给性差异进行分析.结果表明,基于生物可给性的Cr污染土壤健康风险评估能够显著降低风险水平,提高风险控制值,其中,SBRC方法在评估中更具有保守性.3种土壤在相同的Cr（III）和Cr（VI）污染浓度下,栗钙土相较于红壤和潮土在肠期具有更高的生物可给性和健康风险.此外,土壤黏粒、有机质含量及迁移系数能够影响土壤Cr的生物可给性,土壤矿物种类赋存不同也是造成Cr（III）和Cr（VI）在不同土壤中生物可给性差异的重要因素.     

铜铈复合氧化物上石化行业典型VOCs的氧化行为与动力学

采用共沉淀法和等体积浸渍法制备了CuCeO x复合催化剂,对材料的物化性质进行了XRD、低温N2吸脱附、H2-TPR和O2-TPD表征.以石化行业典型VOCs(苯、甲苯和正己烷)为探针污染物,研究了污染物组成与浓度、反应空速、O2浓度、H2O浓度和催化剂种类对其氧化行为的影响,并对反应动力学参数进行了模型拟合.共沉淀得到的催化剂具有均匀的活性相、好的低温可还原性能和较多的活性表面氧物种.甲苯氧化率随着污染物浓度升高而降低,高转化率下苯浓度与其氧化率无相关性,正己烷的氧化率与入口浓度呈正比.苯能够显著抑制甲苯的氧化,而甲苯加入有利于苯的氧化.正己烷对苯氧化的影响较小,但能够促进甲苯的转化,苯系物对正己烷氧化有明显的抑制作用.低空速和高氧浓度都有利于污染物的氧化,氧浓度的变化对正己烷和苯的氧化影响较小.水汽对甲苯的氧化有明显的抑制作用,而对苯和正己烷氧化有明显的促进作用.共沉淀催化剂具有更好的甲苯和苯氧化性能,而无水条件下浸渍催化剂具有更好的正己烷氧化性能.拟一级动力学模型能够很好地模拟不同条件下污染物的氧化行为.     

呼伦湖自净功能及其在区域环境保护中的作用分析

在大量详实资料和调查基础上,论述了呼伦湖富营养化状况,找出了该湖富营养化的影响因素,以及其较强自净功能的成因。呼伦湖地处内陆区高纬度、半干旱气候地区,属牧业污染型,氮入湖量主要来源于点源污染(河流的输入),磷入湖量面源(主要是降尘)大于点源。经多年观测发现,氮和磷的变化并不明显,反映出湖体有较强的自净功能,这是和湖体特殊的地理位置分不开的:①该湖系构造湖与河流沟通的吞吐湖,面积大,水较深,使得湖体自净功能显著;②地处高纬度、半干旱地区,气温低,对湖体浮游生物有一定的抑制作用;③湖体构造特殊,露出30余个泉点,有大量地下水的补给。呼伦湖是一个较大的水体与其周围湿地构成的淡水湖泊生态系统,在维持生物多样性和丰富的生物资源方面发挥巨大作用,且有明显的调蓄洪水的功能,在区域环境保护中具有特殊的地位。     

绿地再生水灌溉土壤微生物量碳及酶活性效应研究

再生水灌溉引起了土壤理化性质的变化,其对土壤生物活性的影响备受关注.以再生水利用较典型的北京为研究区,分层采集了不同再生水灌溉历史的城区公园绿地与城郊农田表层土壤样品,测定并分析了一些常规理化指标、土壤微生物量碳及5种土壤酶（脲酶、碱性磷酸酶、蔗糖酶、脱氢酶和过氧化氢酶）活性,探讨长期再生水灌溉下土壤微生物量碳和酶活性的变化.结果表明,再生水灌溉下公园绿地土壤微生物量碳和酶活性均高于其自来水对照灌区,农田上升不明显.与对照相比,公园绿地与农田再生水灌区0～20 cm土层土壤微生物量碳平均含量分别上升了60.1%和14.2%,公园绿地再生水灌区0～20 cm土层中土壤酶活性平均增幅为36.7%,而农田为7.4%.调查区土壤微生物量碳及酶活性均随土壤深度的增加而降低,其中公园绿地0～10 cm与10～20 cm土层间差异极显著.因此,北京地区城市绿地使用再生水长期灌溉有助于提高土壤生物活性.     

Characteristics of plankton Hg bioaccumulations based on a global data set and the implications for aquatic systems with aggravating nutrient imbalance

• Hg bioaccumulation by phytoplankton varies among aquatic ecosystems. • Active Hg uptake may exist for the phytoplankton in aquatic ecosystems. • Impacts of nutrient imbalance on food chain Hg transfer should be addressed. The bioaccumulation of mercury (Hg) in aquatic ecosystem poses a potential health risk to human being and aquatic organism. Bioaccumulations by plankton represent a crucial process of Hg transfer from water to aquatic food chain. However, the current understanding of major factors affecting Hg accumulation by plankton is inadequate. In this study, a data set of 89 aquatic ecosystems worldwide, including inland water, nearshore water and open sea, was established. Key factors influencing plankton Hg bioaccumulation (i.e., plankton species, cell sizes and biomasses) were discussed. The results indicated that total Hg (THg) and methylmercury (MeHg) concentrations in plankton in inland waters were significantly higher than those in nearshore waters and open seas. Bioaccumulation factors for the logarithm of THg and MeHg of phytoplankton were 2.4–6.0 and 2.6–6.7 L/kg, respectively, in all aquatic ecosystems. They could be further biomagnified by a factor of 2.1–15.1 and 5.3–28.2 from phytoplankton to zooplankton. Higher MeHg concentrations were observed with the increases of cell size for both phyto- and zooplankton. A contrasting trend was observed between the plankton biomasses and BAF_MeHg, with a positive relationship for zooplankton and a negative relationship for phytoplankton. Plankton physiologic traits impose constraints on the rates of nutrients and contaminants obtaining process from water. Nowadays, many aquatic ecosystems are facing rapid shifts in nutrient compositions. We suggested that these potential influences on the growth and composition of plankton should be incorporated in future aquatic Hg modeling and ecological risk assessments.     

Cadmium (Cd) distribution and contamination in Chinese paddy soils on national scale

Rice is a staple food by an increasing number of people in China. As more issues have arisen in China due to rice contaminated by cadmium (Cd), Cd contamination in arable soils has become a severe problem. In China, many studies have examined Cd contamination in arable soils on a national scale, but little studies have focused on the distribution of Cd in paddy fields. This study explored the spatial pattern of Cd in paddy soils in China, made a preliminary evaluation of the potential risk, and identified the most critically contaminated regions based on the domestic rough rice trade flow. The results showed that Cd concentrations in paddy soils in China ranged from 0.01 to 5.50 mg/kg, with a median value of 0.23 mg/kg. On average, the highest Cd concentrations were in Hunan (0.73 mg/kg), Guangxi (0.70 mg/kg), and Sichuan (0.46 mg/kg) provinces. Cd concentrations in paddy soils in central and western regions were higher than those in eastern regions, especially the southeastern coastal regions. Of the administrative regions, Cd standard exceedance rate was 33.2 %, and the heavy pollution rate was 8.6 %. Regarding to Cd of paddy soil, soil environmental quality was better in Northeast China Plain than in Yangtze River Basin and southeastern coastal region. Mining activities were the main anthropogenic pollution source of Cd in Chinese paddy soil. Based on rice trade, more of the Chinese population would be exposed to Cd through intake of rice produced in Hunan province. Certain regions that output rice, especially Hunan province, should be given priority in the management and control of Cd contamination in paddy soil.     

一体化间歇曝气完全混合活性污泥法

一体化间歇曝气完全混合活性污泥法处理装置采取特殊的沉淀区构造,改变了活性污泥的循环流动方式,通过间歇曝气,反应区交替处于好氧/缺氧状态,达到了有机物高效去除、高效硝化反硝化及控制污泥膨胀的效果.该方法具有出水水质好、运行稳定、能耗低、流程简洁和操作管理方便的特点,是一种很有发展潜力的一体化中小型生活污水、城市污水处理系统.     

不同曝气方式下SBR亚硝化的实现及NO2--N积累效果

研究不同曝气方式下亚硝化的实现以及基质浓度、曝气频率和温度对NO-2-N积累效果的影响。以实际污泥脱水液为研究对象,控制进水NH+4-N浓度在50~80 mg/L范围内,温度为27℃,pH值为7.8~8.2,DO浓度为0.5~1.0mg/L,分别采用连续曝气和间歇曝气2种方式启动SBR亚硝化反应器,并考察了在不同基质浓度、曝气频率和温度条件下NO-2-N累积情况。实验研究结果表明,经过40 d左右的运行,在2种不同曝气方式下SBR均成功实现了亚硝化,稳定运行阶段,NO-2-N积累率分别达到95%和85%。经SEM扫描电镜观察发现,在驯化成熟的活性污泥中,亚硝化细菌多呈球状和杆状,大小不同,外形饱满。当进水氨氮浓度小于200 mg/L,曝气频率为曝气15 min/停曝15 min,温度为27℃时,NO-2-N积累效果最佳,平均积累率可达90%以上。间歇曝气可以有效促进亚硝化细菌富集,有利于实现较高浓度的NO-2-N积累。基质浓度、曝气频率和温度对NO-2-N积累效果的影响显著。     

中国主要城市土壤重金属累积特征与风险评价

我国快速城市化过程可能会导致重金属在城市土壤中累积,威胁居民健康.通过收集和整理最近15年间发表的文献数据,从整体上分析了我国52个主要城市土壤重金属含量特征及其健康风险.结果表明,我国城市土壤平均ω(Pb)、ω(Cd)、ω(Cu)和 ω(Zn)分别为:58.5、0.49、42.1 和 156.3 mg·kg-1,其I...