Measurements of Ozone Concentrations in Zagreb

Ozone concentrations were measured in Zagreb at four sites from May 1999 to April 2001 in order to categorize the air quality with respect to ozone. In the summer of 2000, the ozone measurements were also extended to four sites in the suburbs of Zagreb. Methods of active and passive sampling with nitrite ion as a reagent were used. In the northern part of the town ozone was analyzed by an automatic device. Automatic device measurements in the years 1999 and 2000 showed that hourly averages of ozone concentrations did not exceed the Croatian recommended value of the 98th percentile (180 g m^–3). Over the two-year period, 24-h averages occasionally exceed 110 g m^–3 in city center and in the northern part of the town. Regardless of these isolated examples, ozone was well within acceptable concentrations. Ozone concentrations measured in summer 2000 were higher in the suburbs of Zagreb than in the city. The 98th percentile values higher than 110 g m^–3 were recorded at three sites.     

Determination of arsenic in grain and soil by hydride nondispersive atomic fluorescence method

Quantity of trace arsenic in grain and soil was determined by hydride nondispersive atomic fluorescence method.Optimum conditions of measurement were selected in the experiment including the pH of the medium, reductive agent, the concentration and flowing velocity of KBH4, rate of carrier gas and atomized temperature. The reference sample of rice C was determined and the linear relationship of the calibration curve was plotted, indicating that the method was highly precise. In the experiment of recovery rate, the method was quite satisfactory.Based on the determination of hundreds of samples, it is proved that atomic fluorescence method is rapid, sensitive and low in interference. It is very efficient on determination of trace arsenic in soils and grains, especially in grains.     

淮北煤中12种有害微量元素在煤及其灰中的分布特征

为了解有害微量元素在各煤层中的分布与变化规律,以及在煤燃烧后的煤灰中所发生的迁移与富集情况,采集了淮北煤田不同煤层、不同深度的15个煤样,采用中子活化法对其原煤及灰分中的12 种微量元素(Ag, As,Ba, Co, Cr, Cu, Mn, Mo, Sb, Th, U, V)进行了测试。结果显示:绝大部分有害微量元素的含量都处于n×10 6到n×10 5数量级范围内,不同煤层或同一煤层不同部位中微量元素的含量分布不同;与全国和华北煤中有害微量元素的(平均)含量相比,除Mn低于全国和华北的平均值外,As、Co、Mo、Sb、Th、U与之相近,而Ag、Ba、Cr、Cu、V高于全国和华北煤中的平均值;12种微量元素均在灰分中有所富集,而且富集能力序列为:Cu>Cr>Mn>Mo>Co>Ba>V>Th>As>U>Sb。     

恐龙骨骼化石与其它脊椎动物骨骼的微量元素的对比研究

采用中子活化分析 (INAA)技术 ,对比分析恐龙骨骼化石及其它脊椎动物 (乌龟、鱼和大量哺乳动物 )骨骼中微量元素的含量组合 ,结果表明稀土、砷、钡、铀元素在恐龙骨骼化石中的含量远高于其它脊椎动物骨骼 ,而锌元素的含量情况却与之相反 ;同时进一步分析推测得出 :这种砷、钡元素含量的高异常和锌元素的低异常 ,极可能是导致四川盆地恐龙动物群集群死亡的原因之一。     

正己烷萃取—此外分光光度法测定矿井水中微量油

在进行矿井水中油类分析时，用正己烷作为萃取剂，以工作曲线代替标准曲线，从而使油平均回收率增加到96％以上。并在正己烷用量、水样预处理等测试参数选择上做了条件试验。     

祁连—柴达木盆地北缘地区石炭系泥岩沉积地球化学特征

详细研究了祁连—柴达木盆地北缘地区石炭系泥岩的微量元素和稀土元素地球化学特征。各微量元素在各剖面及不同层位变化相当复杂 ,但仍有一定规律 ,这种变化与其物源供应和沉积成岩环境有关。各样品稀土总量变化较大 ,以甘肃永昌煤山子剖面总量最高 ;各泥岩样品轻稀土富集 ,Eu负异常 ,δEu介于 0 .4 4～0 .90之间。微量、稀土元素组合及比值的变化 ,显示物源区母岩为花岗岩和玄武岩的混合 ,稀土分布模式显示源岩为粘土岩、花岗岩和中性岩的混合 ,两者示物源一致。元素的丰度及其比值 ,反映当时水介质环境大部分为海相 ,亦有部分为陆相 ,与其它相标志所表征的结果是一致的。     

水质特性和NOM在臭氧氧化和PAC吸附去除MIB、GEOSMIN上的作用

介绍了臭氧氧化、活性炭吸附去除MIB、GEOSMIN时的主要影响因素，分析了各因素对去除率的影响程度及原因。还介绍了臭氧、PAC去除痕量异味物质的机理。     

电极旋转放电条件下O3合成效率的理论研究

根据低温等离子体理论和电磁场理论，在实验的基础上研究了电极旋转条件下低温等离子体的产生机制和臭氧的合成机制，分析了放电过程中二次放电重叠对臭氧合成的影响，建立了旋转放电与二次放电的理论模型，并根据这一理论模型导出电极旋转条件下的臭氧合成效率与二次放电重叠概率以及电极旋转速度间的理论关系．这一理论结果表明：二次放电重叠使得臭氧合成效率降低，而电极以适当地速度旋转则可以有效地避免二次放电的重叠，从而提高臭氧的合成效率．理论值和实验结果能够较好地吻合．     

重庆某发电厂煤中微量元素的初步研究

重庆市是一个以煤为主要能源的城市，煤在能源消耗中占的比例长期保持在2／3左右。煤在燃烧过程中会释放出有毒有害物质，对环境和人体健康造成危害。为了保护重庆市民的身体健康，制定更加科学的有毒有害物质污染控制对策，本文以某电厂用煤为研究对象，分析了24个煤样中Hg、As、Se、Pb、Cd、Zn、Ba、Co、Cr、Cu、Li、Ni、V、Zr等微量元素的含量水平。结果表明：Hg、As、Se、Cd和Li等元素的浓度克拉克值大于l，说明这些元素在煤中呈富集状态：其余元素的浓度克拉克值小于1，在煤中这些元素呈分散状态。该发电厂然煤中的Hg、As、Pb和Se的含量更高，而其余元素的含量则比北方煤中的低。     

The spatial and temporal distribution of total ozone over China

In this paper the grid data of total ozone mapping spectrograph (TOMS) installed on Nimbus-7 satellite (1978 to 1994) was used and the spatial and temporal distribution of total ozone over China was analyzed. The research indicates that the Qinghai-Tibet Plateau destroyed the latitudinal distribution of total ozone of China and the low value closed center emerged over Qinghai-Tibet Plateau. Long time change trends of seasonal total ozone of Qinghai-Tibet plateau are provided. It shows that the most obvious decrease of total ozone occurs in winter (Jan.), then in summer (Jul.), the relevant slow change occurs in autumn (Oct.) and spring (Apr.).