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1.
The emission of the dioxin-like compounds from on-site waste incinerators of seven schools in Kyonggi Province of Korea was evaluated by determination of the cytochrome P4501A(CYP1A) catalytic activity and antiestrogenic activity using cell culturemicrobioassay. The residue samples were extracted in a Soxhlet apparatus using toluene for 20 hr. The concentrated crude extractswere fractionated with a basic alumina column. Dioxin-like compounds were then extracted. Induction of CYP1A activity in a rat(H4IIE) hepatoma cell line was used as indicator of biologicaleffect of incinerator residues and measured as 7-ethoxyresorufin-O-deethylase(EROD) activities. The EROD activities of fraction II extracts (one of the two extracts) in the H4IIE cells were from 0.044±0.002 to 4.424±0.351 ng-TEQ g-1 (TCDD Toxicity equivalent), showing relatively high inducing capacity. Antisetrogenicity of the extracts was measured as decrease in E2-induced cell proliferation. Most of the extracts showed antiestrogenic activity in MCF7-BUS cell.The TEQ levels of the incinerator residues and the antiestrogenicactivities were in good correlation, strongly suggesting that thepotent toxic emissions were indeed produced from the on-site school waste semi-incinerators and could cause the antiestrogenicity. 相似文献
2.
Wong MY Sauser KR Chung KT Wong TY Liu JK 《Environmental monitoring and assessment》2001,67(3):361-378
The green alga Selenastrum capricornutum expresses a uniqueascorbate peroxidase, that responds to copper and lead. Attemptswere made to test if this peroxidase could be used to monitor thelevels of copper and lead in natural waters. When S.capricornutum was exposed to a stormwater sample, the specificactivity of the peroxidase in the cell extract was commensuratewith the combined copper and lead contents in the sample. Theperoxidase responses were also correlated with the 96 hr biomasstoxicity assay of S. capricornutum. However, unlike thebiomass toxicity assay, the peroxidase activity was not affectedby the anions in the samples. The use of this peroxidase can beused as a marker for testing heavy metal toxicity in the water. 相似文献
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介绍多目标决策-理想点法,并将其改进运用于评价湖泊的营养化,该方法与属性识别理论方法,模糊隶属函数法进行比较,评价结果令人满意. 相似文献
6.
草坪作为城市绿地的重要组成部分,其温室气体的吸收或排放不容忽视.然而当前对亚热带城市草坪温室气体通量的研究相对匮乏.采用静态箱-气相色谱法,对杭州市城区典型城市草坪的多种温室气体(CO2、CH4、N2O和CO)地气交换通量进行了连续观测研究.结果表明,城市草坪的温室气体月平均通量变化明显,而其日变化特征并不明显.城市草地和土壤(无植被生长的裸土)是大气N2O的源,平均通量分别为(0.66±0.17)μg·(m2·min)-1和(0.58±0.20)μg·(m2·min)-1;是CH4和CO的汇,其中CH4平均通量分别为(-0.21±0.078)μg·(m2·min)-1和(-0.26±0.10)μg·(m2·min)-1,CO分别为(-6.36±1.28)μg·(m2·min)-1和(-6.55±1.69)μg·(m2·min)-1.城市草地和土壤CO2平均通量分别为(5.28±0.75) mg·(m2·min)-1和(4.83±0.91) mg·(m2·min)-1.基于相关性分析研究发现,草地和土壤的CO2和N2O通量均与降水量呈显著的负相关,而CH4和CO通量与降水量呈显著的正相关;除草地CH4通量与土壤温度无显著相关、草地N2O通量与土壤温度呈显著负相关外,其余各温室气体通量与土壤温度均呈显著正相关.另外,城市草坪的草地和土壤CO2(R2为0.371和0.314)和N2O (R2为0.371和0.284)通量季节变化受降水量的影响要大于其它温室气体,而土壤温度对CO通量的影响(R2为0.290和0.234)要显著于其它温室气体. 相似文献
7.
利用大流量颗粒物采样器分昼夜采集了2007年春节前后大气气溶胶中PM10和PM2.5样品,并采用气相色谱-质谱技术对PM2.5样品中的多环芳烃进行了检测.春节期间大气颗粒物中PM10和PM2.5夜间平均质量浓度为232 μg·m-3和132 μg·m-3,分别高于白天的PM10(194 μg·m-3)和PM2.5(107 μg·m-3);除夕后颗粒物日平均质量浓度为252.3 μg·m-3 (PM10)和123.8 μg·m-3 (PM2.5),分别高于除夕前的166.7 μg·m-3(PM10)和106.8 μg·m-3(PM2.5);同时夜间PM2.5中多17种多环芳烃(PAHs)的总浓度都高于相应白天的总浓度,且除夕前多环芳烃日均总浓度为95.9 ng·m-3,高于除夕后的58.9 ng·m-3.结果表明,除了受一定的气象条件的影响外,大量燃放烟花爆竹会对大气颗粒物浓度有影响,但对大气中的多环芳烃影响不大,而春节期间工业及交通污染排放的减少削减了排放到大气中的PAHs.根据荧蒽/芘等比值指标判别北京PAHs主要以燃煤为主、交通为次的混合局地源污染. 相似文献
8.
Jiang Xue-Gong Shen Jian-Guo Liu Jing-Tao Chung Yong-Seung 《Water, Air, & Soil Pollution: Focus》2003,3(2):191-212
By using observational data and MM5, an observational analysisand numerical study was conducted on the synoptic condition of a severe dust storm that was caused by a Mongolian cyclone whichoccurred from 6 to 8 April 2001. Results illustrated thatthe cyclogenesis was due to the isentropic potential vorticity (IPV) advection in the upper troposphere and the terrain modifiedbaroclinicity in the mid-lower troposphere. The Altai-Sayan complex of mountains blocked the lower level cold air and made the isentropic surface sharply steep. When the air slid down along the isentropic surface the increasing of baroclinicity anddecreasing of stability blew up the vertical vorticity development.The formation of the dust storm was a result of a cyclonic cold front passing across the area. The occurrence of this dust stormwas closely related to the strong surface wind, which was accompanied by a cold front passing, rather than the cyclogenesis, itself. Hence, the reason for the pre-front dust storm formulation was the formation of heating convection. Reasons behind the formation of a black storm (visibilitylower than 50 m), which occurred in the mid-north part ofInner Mongolia, lay in several aspects. Firstly, in thisarea the surface wind was strong, a direct result of thedownward transport in mid-lower troposphere. Secondly,the cold front passed over the effected area near sunsetso the air obtained much more surface heating to form adeeper mixed layer (ML). Thirdly, cooperation between thelower level wind and the terrain made the atmosphere inthis area and acquired the maximum advective contributionnecessary to form a deep post-front ML. The sensitivityexperiment revealed that surface heat flux was important to the frontal lifting. In addition, the forcing of surface heating wasalso seen as the primary forcing mechanism of frontogenesis. Meanwhile, removal of the surface heat flux made the atmosphericstratification became stable and the pre-storm ML very shallow,which weakened the strength of the dust storm. 相似文献
9.
Wang Xu Ma Yu Chen Hongwu Wen Gang Chen Shoujun Tao Zuyu Chung Yong-Seung 《Water, Air, & Soil Pollution: Focus》2003,3(2):67-79
With observational data spanning 1961–1999 from 90 meteorological stations in Xinjiang, China, the spatial and temporal characteristics of sandstorms and strong winds, and the contribution of strong winds to the occurrence of sandstormsare analyzed. Moreover, the dominant wind direction and minimumwind speeds during sandstorm periods are discussed. The research shows that although possessing similar climatic trends, sandstorms and strong winds in Xinjiang have opposite geographical distributions, i.e. places with more sandstorms show fewer strong winds. The contribution of strongwinds to sandstorms in northern Xinjiang is larger than that insouthern Xinjiang. The dominant wind directions clearly indicatethe paths of the weather systems that introduced the sandstorms.The minimum wind speeds in the sandstorms were over 10 ms-1in northern and eastern Xinjiang and in the Turpan and Yanqi Basins of southern Xinjiang. In Tarim Basin of southern Xinjiang,however, the minimum wind speed was about 6–8 ms-1, and even 6 ms-1 at its southern edge. 相似文献
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