气相色谱法测定长江水体悬浮物和沉积物中有机氯农药的残留量

采用GC/MS定性 ,GC/ECD定量 ,对长江南京段悬浮物和沉积物中 8种有机氯农药 (OCPs)进行了分离测定 ,结果表明悬浮物中OCPs的含量分布按DDTs>HCB HCHs的顺序减小 ,DDTs的含量为 0 5 2— 1 15ng·L-1,HCB及HCHs的含量分别为 0 11— 0 48ng·L-1和 0 14— 0 47ng·L-1.沉积物中OCPs的含量分布按DDTs >HCB >HCHs的顺序减小 ,DDTs的含量为 0 2 1— 4 5 0ng·g-1,HCB及HCHs的含量分别为 0 14— 3 96ng·g-1和 0 18— 1 6 7ng·g-1.但总的来说 ,长江悬浮物和沉积物中有机氯农药在各采样点的分布特征较相似 .     

室内空气中多环芳烃污染的测量和特征性研究

本文就室内空气中多环芳烃典型污染源－室内燃煤和室内吸烟排放的多环芳烃组成和含量进行了测定，并同室外大气（对照）中多环芳烃组成含量进行了对比，研究了室内环境不同污染源排放多环烃组成和含量的特征性，结果表明，室内燃煤污染同燃煤型室外大气源排放多环芳烃具有相似组成含量特征，而室朵烟草烟雾污染源的多环芳烃组成含量特征，则与室外煤型和交通型均有显著区别。     

从武汉印染厂废水淤泥中分离出的趋磁细菌的生长与磁小体形成过程

对从武汉印染厂污泥中分离出的趋磁细菌YN-1,分别进行了5 d,10 d,20 d,25 d和30 d的纯培养与透射电镜的观察,并对30 d释放出的磁小体进行了能谱分析.结果表明:培养5 d的趋磁细菌,其体内的细胞质相对均匀,可见到铁质在细胞内输送的痕迹.随后细胞质变为不均匀,菌体内泡状物和磁小体增多;20 d后菌体膜出现自溶,可见磁小体从破裂的菌膜排出体外的现象,25 d后可见到具有鞭毛、细胞质分布均匀的“营养体”.培养30 d,菌膜基本自溶,除见有营养体外,残存大量的细胞膜碎片和磁小体,对它们的能谱分析显示,磁小体的主要无机成分为Fe.由此判断,25 d可能为该菌在培养条件下的趋磁细菌生长与磁小体形成周期.图3表1参15     

动态顶空-气相色谱/离子阱质谱法测定土壤中苯系物

采用动态顶空进样,气相色谱/离子阱质谱法测定土壤中的苯系物。对样品的吹扫温度、吹扫时间和解析时间进行了优化,各组分的方法检出限：苯为0.43 μg/kg,甲苯为1.13 μg/kg,对、间二甲苯均为1.74 μg/kg,邻二甲苯为0.37 μg/kg;对5种苯系物的低、中质量浓度标液进行加标,回收率为82.0%～115%,重复测定7次的RSD为4.8%～15.1%。对某造纸厂周边土壤样品中苯系物进行测定,结果固废堆存处周边土壤中苯和甲苯检出。     

SPE-GC/MS法测定水中对硝基氯苯和2,4-二硝基氯苯

采用SPE-GC/MS法测定水中对硝基氯苯和2,4-二硝基氯苯,优化了试验条件.对硝基氯苯在1.00 mg/L～80.0 mg/L之间线性关系良好,2,4-二硝基氯苯在1.00 mg/L～50.0 mg/L之间线性关系良好,方法检出限对硝基氯苯为0.6 μg/L,2,4-二硝基氯苯为2.1 μg/L,回收率对硝基氯苯为86.2%～94.7%,2,4-二硝基氯苯为87.3%～95.4%.     

机动车排放尾气中挥发性有机污染物对环境空气质量影响初探

采用气相色谱/质谱检测技术,对汽油和柴油、汽油车和柴油车排放气体以及天津市环境空气中主要挥发性有机污染物(VOCs)的组成种类及比例进行探析.结果表明,机动车排放的尾气中主要有机污染物为芳香烃类、烷烃类和烯烃类化合物,其中芳香烃类含量最高;汽油车排放的芳香烃类化合物浓度高于柴油车排放的浓度;机动车尾气对交通区域空气质量的影响高于工厂区(非化工区)、生活小区和公园.     

气相色谱法直接进样测定环境空气中的卤代烃

用100mL玻璃注射器采集气样，直接进入气相色谱仪，卤代烃经HP—101毛细管柱分离、ECD测定。方法检出限为0.007mg／m^3-0．05mg／m^3，相对标准偏差为3．4％-7．6％，加标回收率为94％-106％。     

加速溶剂提取气-质联用分析土壤中的多环芳烃

建立了加速溶剂提取-凝胶渗透色谱净化和气相色谱-质谱联用快速分析土壤中16种多环芳烃的新方法。方法的检出限、定量限分别为1.1~12μg/kg、3.7~40μg/kg。16种PAHs的回收率为76.6%~96.8%,相对标准偏差为2.9%~9.5%。应用于多个环境样品的分析测试,结果满意。     

固相萃取-UPLC-MS/MS法测定水中全氟化合物

水样中全氟辛酸、全氟辛烷磺酸钾、全氟丁酸、全氟丁烷磺酸经弱阴离子交换固相萃取柱富集净化后,用超高效液相色谱-串联质谱法测定。通过优化样品前处理条件和仪器条件,使4种全氟化合物在0.05μg/L~10.0μg/L范围内线性良好,相关系数为0.998 9~0.999 9,方法检出限为0.27 ng/L~0.96 ng/L。空白水样3个质量浓度水平的加标回收率为73.1%~91.3%,6次测定结果的RSD为7.4%~14.3%。     

Molecular characterization of transformation and halogenation of natural organic matter during the UV/chlorine AOP using FT-ICR mass spectrometry

UV/chlorine process, as an emerging advanced oxidation process (AOP), was effective for removing micro-pollutants via various reactive radicals, but it also led to the changes of natural organic matter (NOM) and formation of disinfection byproducts (DBPs). By using negative ion electrospray ionization coupled with Fourier transform ion cyclotron resonance mass spectrometry (ESI FT-ICR MS), the transformation of Suwannee River NOM (SRNOM) and the formation of chlorinated DBPs (Cl-DBPs) in the UV/chlorine AOP and subsequent post-chlorination were tracked and compared with dark chlorination. In comparison to dark chlorination, the involvement of ClO^?, Cl^?, and HO^? in the UV/chlorine AOP promoted the transformation of NOM by removing the compounds owning higher aromaticity (AI_mod) value and DBE (double-bond equivalence)/C ratio and causing the decrease in the proportion of aromatic compounds. Meanwhile, more compounds which contained only C, H, O, N atoms (CHON) were observed after the UV/chlorine AOP compared with dark chlorination via photolysis of organic chloramines or radical reactions. A total of 833 compounds contained C, H, O, Cl atoms (CHOCl) were observed after the UV/chlorine AOP, higher than 789 CHOCl compounds in dark chlorination, and one-chlorine-containing components were the dominant species. The different products from chlorine substitution reactions (SR) and addition reactions (AR) suggested that SR often occurred in the precursors owning higher H/C ratio and AR often occurred in the precursors owning higher aromaticity. Post-chlorination further caused the cleavages of NOM structures into small molecular weight compounds, removed CHON compounds and enhanced the formation of Cl-DBPs. The results provide information about NOM transformation and Cl-DBPs formation at molecular levels in the UV/chlorine AOP.