固定污染源烟尘监测质量的探讨

固定污染源烟尘是大气污染的重要来源之一。测试烟尘浓度是检查污染源排放的尘粒是否符合排放标准的重要手段；是为大气质量管理与评价提供依据的重要手段。监测烟尘的一般方法是滤筒重量法。现在通常用的仪器(特别是四级站)是JYP-Ⅱ型静压平衡烟尘浓度测定仪。     

沈阳市大气微生物的研究

用ＡＮＤＥＲＳＥＮ生物粒子采样器在沈阳市对大气细菌粒子浓度和革兰氏染色形态特征进行了一年的观测．结果表明，细菌粒子的种类年平均浓度分布，是随着地区的季节、时间、场所和人群活动的变化而变化．     

土壤重金属污染的酶学诊断——紫色土中的镉、铜、铅、砷对水稻根系过氧化物酶的影响

通过四川酸性紫色土、中性紫色土,石灰性紫色土中不同浓度的Cd、Cu、Pb、As对水稻根系过氧化物酶的影响研究,揭示了过氧化物酶受抑制与产生抗性的过程.在低浓度时,上述元素对过氧化物酶的影响能反映土壤类型影响的差别.确定了三种紫色土中Cd、Cu、Pb、As的临界浓度.     

多边形源下风方向的污染物浓度

面源下风方向空气颗粒物或气体浓度计算涉及到二重积分。当面源是圆形或多边形时,文中给出了高斯烟流模型降解为一重积分的形式。文中还给出了当下风距离超过窄烟流近似法应用极限距离2到3倍时的近似计算方法,精确度达到了10％,计算速度提高了5倍。     

渭北黄土高原苹果优质气候层带分析

本文利用元帅系苹果定位试验的品质测定资料,分析研究了苹果品质(含糖量、含酸量、硬度等)与海拔高度及其垂直气候层带的关系,认为我国渭北黄土高原海拔1000—1500m 范围的半湿润、半干旱地区,是全国苹果品质最佳的优质气候区。这一层带的气候-土壤生态条件,适宜于发展优质苹果生产和建立商品生产基地。     

下行流人工湿地去除生活污水中氮磷的研究

用下行流人工湿地处理生活污水,分析了系统对TP,TN的处理效果,并将有无植物2种系统对污染物的去除效果进行对比.研究结果表明:下行流人工湿地对N,P都有很高的去除率;进水中TN,TP的浓度变化对出水中N,P含量影响不大,系统对N,P有一定的抗冲击能力;植物在污染物去除过程中起了一定的作用.     

低DO浓度下短程硝化试验研究

进水氨氮浓度不变，低DO下启动并运行了短程硝化试验，考察了反应器内的氨氮氧化和亚硝酸盐积累情况。试验结果表明反应器内氨氮几乎全部被氧化，污泥浓度从4500mg／L下降到870mg／L，此时亚硝酸盐的积累率为55％，说明只控制DO的浓度很难实现高的积累率，同时受到温度和污泥龄等的较大影响。     

Spatial variations in daily average CO2 concentrations above wetland surface of Xianghai National Nature Reserve, China

Horizontal and vertical variations of daily average CO2 concentration above the wetland surface were studied in Xianghai National Nature Reserve of China in August, 2000. The primary purpose was to study spatial distribution characteristics of CO2 concentration on the four levels of height(0.1 m, 0.6 m, 1.2 m and 2 m) and compare the differences of CO2 concentration under different land covers. Results showed that daily average CO2 concentration above wetland surface in Xianghai National Natural Reserve was lower than that above other wetlands in northeast China as well as the worldwide average, suggesting that Xianghai wetland absorbed CO2 in August and acted as“sink” of CO2. The horizontal variations on the four levels of height along the latitude were distinct, and had the changing tendency of“decreasing after increasing” with the increase of height. The areas with obvious variations were consistent on different levels of height,and those with the highest variations appeared above surface of shore, sloping field, Typha wetland and Phragmites wetland; the vertical variations were greatly different, with the higher variations in Phragmites wetland and Typha wetland, and the lands near the shore and the sloping field with the lower variations. Spatial variations of daily average CO2 concentrations above wet!and surface were affected by surface qualities and land covers.