白洋淀地区的多氯联苯污染研究

对白洋淀地区不同类型纸厂排水口底泥及保定市排污渠底泥进行了ＧＣ／ＥＣＤ分析，可萃取有机氯（ＥＯＣｌ）含量测定，检出了多氯联苯和有机氯农药。用截止分子量为１０００道尔顿的透析袋方法对相应地区的水体进行了检测，发现水体中可检出含氯农药六六六，但多氯联苯等由于水中存在浓度低未能检出，同样样品的ＧＣ／ＭＳ／ＣＯＭ结果表明，水体中主要存在的亲脂性有机污染物为：蒽酮、蒽二酮、苯胺、氯代烃、邻苯二甲酸酯类和苯系物。     

One-step preparation of a novel graphitic biochar/Cu0/Fe3O4 composite using CO2-ambiance pyrolysis to activate peroxydisulfate for dye degradation

Herein,a one-step co-pyrolysis protocol was adopted for the first time to prepare a novel pyrogenic carbon-Cu⁰/Fe₃O₄ heteroatoms (FCBC) in CO₂ ambiance to discern the roles of each component in PDS activation.During co-pyrolysis,CO₂ catalyzed formation of reducing gases by biomass which facilitated reductive transformation of Fe³⁺ and Cu²⁺ to Cu⁰ and Fe₃O₄,respectively.According to the a...     

博斯腾湖矿化度遥感反演及空间分布特征研究

以我国最大的内陆淡水湖——博斯腾湖为研究对象,利用Terra/MODIS L1B空间分辨率为250 m和500 m的遥感反射率数据及湖水矿化度实测数据建立线性回归模型,分析湖表面矿化度的空间分布特征。结果表明:空间分辨率为500 m的1~7个波段组合建立的多元线性回归模型相关性最高(R~2=0.70),模型验证结果显示,实测值和反演值的相关系数(R~2)为0.82,均方根误差(RMSE)为0.12。利用最优模型对博斯腾湖湖面矿化度进行反演,其分布存在明显的空间梯度,西北、东北和东南湖区矿化度较高,而西南湖区和湖区南部矿化度较低。     

长期饲喂钬对鲤鱼非特异性免疫酶活性的影响

以鲤鱼为研究对象,进行为期60 d的饲喂试验,研究了硝酸钬对其非特异性免疫的影响。结果表明:与对照组相比,在实验剂量范围内,超氧化物歧化酶(SOD)、过氧化氢酶(CAT)、谷胱甘肽过氧化物酶(GSH-Px)在肝脏中呈先升高后降低的趋势,SOD、GSH-Px酶活性在20 mg·kg~(-1)时,升高显著(P0.05),三者在65 mg·kg~(-1)时都被显著抑制(P0.05);在肾中都被诱导,在65 mg·kg~(-1)升高显著(P0.05)。肝肾中丙二醛(MDA)含量都变化不显著(P0.05)。抗超氧阴离子自由基、抑制羟自由基能力和单胺氧化酶(MAO)活性都降低,且在65 mg·kg~(-1)时降低显著(P0.05或P0.01)。因此,在饲料中添加稀土元素钬20、42、65 mg·kg~(-1),能够影响非特异性免疫力,且鲤鱼肝组织比肾脏反应更敏感。     

基于仿生防护技术的海底管线悬空治理研究

针对海底管线悬空对海洋油气田安全生产的严重威胁及其对海洋环境构成的重大隐患,文章以海底管线周围的局部冲刷及其冲刷防护与控制技术为研究对象,从海底管线冲刷机理入手,分析了管线一次悬空和二次悬空的原因,从模型实验和工程实践两方面开展仿生防护技术治理海底管线悬空研究,利用高分子材料仿生草叶片的柔性黏滞阻尼作用,减缓流速,降低水流的携沙能力,最终达到固沙、填沙、保护管线的目的。     

基于神经网络的碳排放预测及影响因素分析

基于新疆1995—2014年农业生产碳排放源,建立碳排放关系数据库。应用广义神经网络(generalized regression neural network,GRNN)构建了排放量预测模型,结合平均影响值(mean impact value,MIV)方法对碳排放影响因素进行量化。结果表明:1)GRNN模型预测碳排放的平均绝对百分误差和拟合优度分别为2.7860%和0.8720;2)新疆人口、人均GDP、农业贡献值、农机总动力和农户固定资产投资等因素对农业生产碳排放的影响程度分别为0.6210、0.2377、0.3698、0.8500和0.1000。该成果可为新疆碳排放总量分析和影响因素量化方面提供参考。     

和田绿洲沙尘暴物质输送路径及其对大气环境质量的影响

为了研究来自不同方向的沙尘暴对和田绿洲大气环境质量的影响，本文利用HYSPLIT后向轨迹模型和NCEP的GDAS全球气象要素数据，将和田绿洲西北部的墨玉县城作为模拟受点（37.26°N，79.72°E），计算2016年1月1日—2018年12月31日发生的每一次沙尘天气期间逐日18：00（世界时）36 h后向气流轨迹，轨迹计算起始高度设置为500 m，并结合相应的PM_2.5、PM₁₀、SO₂、NO₂、CO、O₃浓度监测数据进行聚类分析，研究抵达该地区的沙尘暴的主要移动轨迹和污染物输送路径.同时，运用潜在源贡献因子分析法（PSCF）和权重污染轨迹分析法，分析了沙尘暴期间不同气流轨迹对墨玉县污染物浓度的影响，识别大气污染物的潜在源区，揭示不同源区对污染物浓度的贡献差异.结果表明，影响和田绿洲（墨玉县）的沙尘暴主要来自西北（WN）、北（N）、东北（EN）和东（E）4个方向；其中，来自东部的沙尘天气频率最高（60.2%），但主要以浮尘天气为主；扬沙和强沙尘暴主要来自西部方向，54.48%的强沙尘暴和38.53%的扬沙来自西和西北方向.不同沙尘源区和不同传输路径上的沙尘气溶胶对和田绿洲大气环境的影响不一样.沙尘天气期间，大气PM_2.5和PM₁₀的平均浓度相当于无沙尘天气期间的3~5倍，但对SO₂、NO₂、CO、O₃质量浓度的影响不大；由西向东和由北向南的沙尘暴对墨玉县PM_2.5和PM₁₀质量浓度的贡献率最大；由东向西的沙尘暴由于路过和田市和洛浦县等工业污染源区，此簇沙尘暴气团将该区域SO₂、NO₂、CO等污染颗粒携带到墨玉县，因此，东-东南（E-ES）方向的沙尘暴对SO₂、NO₂、CO的贡献率分别为15.56%、20.55%和21.57%.本文定量印证了沙尘暴对和田绿洲大气环境质量的影响，可为绿洲区沙尘暴研究提供参考.     

黄龙自然保护区喀斯特湖泊水色特征及其影响因素

湖泊颜色是黄龙自然保护区喀斯特景观的核心美景.以黄龙自然保护区喀斯特湖泊和高原非喀斯特湖泊(措琼海、夏茹措)为研究对象,通过高光谱设备测定离水辐亮度量化湖泊水色,对比分析黄龙自然保护区与其他高原非喀斯特湖泊水色特征及其水环境因子,进而探究黄龙自然保护区湖泊水色特征及其影响因素.结果显示：(1)黄龙自然保护区喀斯特湖泊水体呈现蓝绿色,湖泊归一化离水辐亮度反射波长主要集中在420-570 nm.(2)黄龙喀斯特湖泊水化学类型为Ca²⁺-HCO₃^-和Mg²⁺-HCO₃^-型,具有高透明度和贫营养化等独特的水环境特征,对可见光的吸收、反射和散射具有强烈的波长选择性,而非喀斯特湖泊光谱曲线的变化没有黄龙喀斯特湖泊明显.(3)对黄龙喀斯特湖泊水色成因分析,黄龙喀斯特湖泊含有丰富的Ca²⁺、Mg²⁺、HCO₃^-,钙华沉积是喀斯特湖泊水色形成的核心过程.冗余分析和相关性分析中,不同的水环...     

Contribution of precursor compounds to the release of per- and polyfluoroalkyl substances (PFASs) from waste water treatment plants (WWTPs)

Per-and polyfluoroalkyl substances(PFASs) are ubiquitous in sludge and water from waste water treatment plants, as a result of their incorporation in everyday products and industrial processes. In this study, we measured several classes of persistent PFASs,precursors, transformation intermediates, and newly identified PFASs in influent and effluent sewage water and sludge from three municipal waste water treatment plants in Sweden, sampled in 2015. For sludge, samples from 2012 and 2014 were analyzed as well.Levels of precursors in sludge exceeded those of perfluoroalkyl acids and sulfonic acids(PFCAs and PFSAs), in 2015 the sum of polyfluoroalkyl phosphoric acid esters(PAPs) were 15–20 ng/g dry weight, the sum of fluorotelomer sulfonic acids(FTSAs) was 0.8–1.3 ng/g,and the sum of perfluorooctane sulfonamides and ethanols ranged from non-detected to 3.2 ng/g. Persistent PFSAs and PFCAs were detected at 1.9–3.9 ng/g and 2.4–7.3 ng/g dry weight, respectively. The influence of precursor compounds was further demonstrated by an observed substantial increase for a majority of the persistent PFCAs and PFSAs in water after waste water treatment. Perfluorohexanoic acid(PFHxA), perfluorooctanoic acid(PFOA), perfluorohexane sulfonic acid(PFHxS), and perfluorooctane sulfonic acid(PFOS)had a net mass increase in all WWTPs, with mean values of 83%, 28%, 37% and 58%,respectively. The load of precursors and intermediates in influent water and sludge combined with net mass increase support the hypothesis that degradation of precursor compounds is a significant contributor to PFAS contamination in the environment.     

Transport and fate of mercury under different hydrologic regimes in polluted stream in mining area

Seepage from Hg mine wastes and calcines contains high concentrations of mercury (Hg). Hg pollution is a major environmental problem in areas with abandoned mercury mines and retorting units. This study evaluates factors, especially the hydrological and sedimentary variables, governing temporal and spatial variation in levels and state of mercury in streams impacted by Hg contaminated runo . Samples were taken during di erent flow regimes in theWanshan Hg mining area in Guizhou Province, China. In its headwaters the sampled streams/rivers pass by several mine wastes and calcines with high concentration of Hg. Seepage causes serious Hg contamination to the downstream area. Concentrations of Hg in water samples showed significant seasonal variations. Periods of higher flow showed high concentrations of total Hg (THg) in water due to more particles being re-suspended and transported. The concentrations of major anions (e.g., Cl??, F??, NO3?? and SO4 2??) were lower during higher flow due to dilution. Due to both sedimentation of particles and dilution from tributaries the concentration of THg decreased from 2100 ng/L to background levels (< 50 ng/L) within 10 km distance downstream. Sedimentation is the main reason for the fast decrease of the concentration, it accounts for 69% and 60% for higher flow and lower flow regimes respectively in the upper part of the stream. Speciation calculation of the dissolved Hg fraction (DHg) (using Visual MINTEQ) showed that Hg(OH)2 associated with dissolved organic matter is the main form of Hg in dissolved phase in surface waters in Wanshan (over 95%).