RBCA、CLEA及CalTOX模型在苯并[a]芘污染场地健康风险评估中的应用比较

为探讨不同模型对污染场地健康风险评估结果的影响,以苯并[a]芘为例,采用RBCA、CLEA和CalTOX模型对某工业污染场地表层土壤进行健康风险评估,分析了评估结果的差异和原因,同时对模型的主要暴露参数进行了敏感性分析,并推导出基于风险概率分布的土壤修复限值。结果表明,RBCA、CLEA和CalTOX模型计算的苯并[a]芘致癌总风险分别为2.40×10-4、6.32×10-4和7.04×10-6,且经口摄入和皮肤接触2个途径对人体健康造成的危害最大。降解作用是影响CalTOX模型风险评估结果不同于RBCA和CLEA模型的重要因素,3个模型间参数取值及方法学的差异也会导致风险评估结果不同。各模型暴露参数的敏感性排序也有差异。采用基于风险概率分布的方法推导土壤修复限值,RBCA、CLEA和CalTOX模型所得结果分别为0.18、0.08、0.13(不考虑降解作用CalTOX模型)和10.74(考虑降解作用CalTOX模型)mg·kg-1,为各模型直接推导值的1.5～2.6倍。基于风险概率分布的方法可有效降低风险评估过程中参数不确定性的影响,为工业污染场地土壤修复值的制定提供参考。     

钛对聚合硫酸铁制备与性能的影响

研究了由FeSO4制备聚合硫酸铁过程中,钛对聚铁聚合态分布和稳定性的影响,并进一步考察了含钛聚合硫酸铁的絮凝性能.应用络合比色法对聚铁中不同水解形态聚铁的含量进行了分析测定,并通过沉淀实验考察了不同钛含量对聚铁稳定性的影响;随后,通过出水浊度、TOC、金属离子残余量和出水pH等指标测试,研究了钛对聚合硫酸铁混凝性能的影响.结果表明,较低的钛含量(<0.025)在一定程度上有利于中聚态聚铁的形成,提高了聚铁絮凝剂的混凝效率;反之,钛含量超过0.025时不仅聚铁的稳定性显著下降,而且处理后出水的钛残留增加,pH降低.     

Threshold management in a coupled economic–ecological system

Economic analysis of optimal ecosystem management in the presence of a threshold has typically ignored the potential for induced behavioral responses. This paper contributes to the literature on non-convex ecosystem management by considering the implications of a particular behavioral response in a regional economy – that of amenity-led growth – to changes in ecosystem services generated by a lake ecosystem subject to a eutrophication threshold. The essential policy challenge is to achieve optimal levels of lake nutrients and urbanization given that improvements to water quality will induce additional migration and urbanization in the region with attendant ecological impacts. We show that policies that ignore the recursive relationship between urbanization and water quality unintentionally exacerbate boom-bust cycles of regional growth and decline and risk pushing the system towards long-run economic decline. In contrast, the optimal policy accounts for the behavioral feedbacks to improved ecosystem services, and balances regional growth and ecological degradation.     

Distribution characteristics of phosphorus forms in the sand-dust and the desert particles in Inner Mongolia and its environmental significance

根据我国中路沙尘暴的影响范围和移动路径,应用颗粒物中磷的连续浸提技术,选择研究了8个站位的颗粒物样品中磷的赋存形态和分布特征.研究结果表明,各粒级样品中无机磷（IP）含量范围在300.16—1916.99μg.g-1,占总磷（TP）比率86.11%—99.84%,TP含量主要受IP控制,有机磷（POrg）含量远低于IP,彼此之间表现为负相关关系;沙尘粒子Y1—Y4（呼和浩特,2005年—2010年沙尘暴期间收集）的TP、IP、生物可交换磷（BP）和可交换态磷（Pex）含量远高于沙尘暴源地及沿途地区地表颗粒物,这与沙尘暴源地及影响区域磷污染状况及地质环境条件关系密切;粒径小于57μm的颗粒物样品的TP、IP、PCa含量均高于自然粒径颗粒物样品.     

Characterization of soil low-molecular-weight organic acids in the Karst rocky desertification region of Guizhou Province, China

Soil low-molecular-weight (LMW) organic acids play important roles in the soil-forming process and the cycling of nutrients in Karst regions. In this study, we quantified the contents of LMW organic acids (including lactate, acetate, formate, malate, and oxalate) in soil solution over the Karst region of Guizhou Province, China using ion chromatography. The concentration of total LMW organic acids in topsoil solution ranged from 0.358 to 1.823 μmol·g^-1, with an average of 0.912 μmol·g^-1. The mean concentrations of lactate, acetate, formate, malate, and oxalate were 0.212±0.089, 0.302±0.228, 0.301±0.214, 0.014±0.018 and 0.086±0.118 μmol·g^-1, respectively. There were also significant difference in the contents of these acids among four phases of rocky desertification, and their concentrations decreased with the aggravation of rocky desertification. The concentrations of the LMW organic acids were significantly positive correlated each other. Significant positive correlations were also observed among individual LMW organic acids in soil solution, and between them and soil available P, available K, exchangeable Ca, respectively. Furthermore, the concentrations of LMW organic acids were significantly positively correlated with inorganic anions (chlorides, nitrates, and sulfates) in Karst topsoil solution. Therefore, the concentrations of soil LMW organic acids might be one of driving force in the Karst rock desertification process in Guizhou Province.     

Optimal locations of monitoring stations in water distribution systems under multiple demand patterns: a flaw of demand coverage method and modification

A flaw of demand coverage method in solving optimal monitoring stations problem under multiple demand patterns was identified in this paper. In the demand coverage method, the demand coverage of each set of monitoring stations is calculated by accumulating their demand coverage under each demand pattern, and the impact of temporal distribution between different time periods or demand patterns is ignored. This could lead to miscalculation of the optimal locations of the monitoring stations. To overcome this flaw, this paper presents a Demand Coverage Index (DCI) based method. The optimization considers extended period unsteady hydraulics due to the change of nodal demands with time. The method is cast in a genetic algorithm framework for integration with Environmental Protection Agency Net (EPANET) and is demonstrated through example applications. Results show that the set of optimal locations of monitoring stations obtained using the DCI method can represent the water quality of water distribution systems under multiple demand patterns better than the one obtained using previous methods.     

石家庄地区雾霾天气下云滴和云凝结核的分布特征

2009年5~10月在石家庄地区对雾霾天气下的近地面到高空的云雾滴和云凝结核(CCN)进行了7架次飞机探测.利用PMS云粒子测量仪器、机载温湿仪和连续气流纵向热梯度云凝结核仪获得的云雾粒子和云凝结核(CCN)探测资料,分析了层积云(Sc)和高积云(Ac)中云粒子浓度、液态含水量、粒子算术平均直径和粒子有效平均直径的垂直分布特征;分析了CCN垂直和水平分布特征以及谱分布.结果表明雾霾天气状况下,云滴数浓度在102个/cm3量级上.高云粒子粒径总体大于低云粒子.云含水量平均值范围为0.03~0.14g/m3;地面到600 m高度内, CCN值的平均值为3034cm-3(过饱和度S=0.3%).对CCN的活化谱进行拟合表明石家庄属于典型大陆性核谱,云对CCN有消耗作用,逆温层的存在使得该区CCN浓度累积增加.     

洋河水库微囊藻空间分布特征及其影响因素分析

通过野外调查及现场风速实时监测,对2010年夏季我国河北洋河水库微囊藻的空间分布特征及其影响因素进行了研究.结果表明,在水平空间上,西洋河口(主要入湖河口)微囊藻细胞密度最高,库心、北库心、坝前西、东洋河口等位置次之,坝前东(取水口)处微囊藻细胞密度最低,整体呈由水库西北向东南方向降低的趋势.Pearson相关性检验表明,洋河水库微囊藻细胞密度与ρ(TP)显著相关(P<0.05),但与ρ(DTP)、ρ(TN)及ρ(NO3--N)相关性不显著(P>0.05).风场分析表明,洋河水库水华发生季节东南风风频明显大于西北风,说明洋河水库微囊藻水平空间分布主要受入湖河流氮、磷污染及风场分布共同影响.西洋河口和库心的微囊藻昼夜垂向分布特征表现为早晨主要集中在水体的表层(10 cm),中午主要分布在水体0～3.5 m的水层,而傍晚时则可能下沉至底层,昼夜变化规律明显,并且其垂向分布特征主要受藻细胞的光合作用和风浪的混匀作用共同影响.      

2006─2010年环保重点城市主要污染物浓度变化特征

利用2006─2010年全国环保重点城市的空气质量日报数据,分析了大气ρ(SO2)、ρ(NO2)和ρ(PM10)的变化特征. 结果表明:从年际变化看,ρ(SO2)和ρ(PM10)呈下降趋势,ρ(NO2)变化不显著.从季节变化看,ρ(SO2)、ρ(NO2)和ρ(PM10)均呈冬季高、夏季低的特征.从浓度谱分布看,全国大气中ρ(SO2)、ρ(NO2)和ρ(PM10)分别集中在0～0.150、0～0.100和0～0.250 mg/m3范围内,ρ(SO2)和ρ(PM10)谱峰区间逐渐向低浓度范围偏移,高浓度事件逐渐减少,表明SO2和PM10污染得到较明显的控制,而ρ(NO2)谱峰变化不大.从浓度变化看,山西ρ(SO2)、ρ(NO2)和ρ(PM10)下降最明显,年变化率分别为-11.2、-3.6和-14.2 μg/m3;青海ρ(SO2)、山东ρ(NO2)和ρ(PM10)的上升趋势最明显,年变化率分别为4.4、2.7和4.5 μg/m3.      

中国大气NH3和NOx排放的时空分布特征

根据我国不同氨源的数量、燃料消费量和相应的氨与氮氧化物排放因子,计算了我国大陆地区1995~2004年历年的氨(NH3)排放量与1985~2005年历年的氮氧化物(NOx)排放量,在此基础上模拟了2006~2010年的NOx排放量,并分析了NH3和NOx排放强度的空间分布.结果表明:2004年,我国NH3排放量为12.0Tg,比1995年的10.6Tg增加了大约13.2%;2004年的NOx排放量为20.6Tg,比1995年的12.2Tg增加了大约68.9%,比1985年的6.2Tg增加了大约2.3倍.在1996年以前,我国NH3和NOx的排放量基本相当,但是此后NH3的年排放量在经历了1997~1999年的下降之后,变化比较平稳,而NOx的排放量自2000年之后呈逐年迅速增加的趋势.2004年全国NH3的排放总量中,畜禽排泄、氮肥施用、人类粪便、氮肥与合成氨生产的贡献率分别为69.2%、15.2%、13.9%和1.9%;2004年全国NOx的排放总量中,由于受到我国能源消费结构的制约,煤炭来源的NOx占到了排放总量的77.4%.NH3和NOx的排放强度都具有明显的空间差异,表现在中东部地区的排放强度明显高于西部地区,这与中东部地区人口多、能源消费量大以及畜禽养殖数量大有关.