色谱质谱联用技术在一起农药污染事故应急监测中的应用

在一起污染源应急事故中,色谱质谱联用技术在确定污染源类型,并快速做出准确定性定量分析中发挥了重要作用。通过气相色谱-质谱联用技术,首先确定可能污染物类型为三嗪类化合物;之后,通过液相色谱-串连质谱全扫描,推断可能为三嗪类除草剂——甲磺隆。正、负ESI子离子全扫描后图谱与甲磺隆标准物质图谱相对照,完全吻合。最后,通过SRM模式下对380.0→139.0的母、子离子选择反应监测,测定了农田灌溉水源和土壤中甲磺隆的含量。     

Phototransformation of herbicide metsulfuron methyl

Phototransformation of the herbicide metsulfuron methyl was investigated on glass surface under sunlight and ultraviolet (UV) light and compared with dark condition. The half-lives of metsulfuron methyl under UV light and sunlight were found to be 0.5 and 7.8 days respectively. Rate of phototransformation followed first order kinetics with significant correlation coefficient. The major photoproducts were identified as methyl-2-sulfonyl-amino-benzoate, 2-amino-6-methoxy-4-methyltriazine and saccharin (O-sulfobenzoimide). Various metabolites from this study were identified by high performance liquid chromatography (HPLC). Authentic samples required for HPLC comparison were prepared in laboratory and characterized on the basis of nuclear magnetic resonance (NMR) and infra red (IR) spectral data. These metabolites were also identified from metsulfuron methyl treated wheat field soil.     

Combined effects of two sulfonylurea herbicides on soil microbial biomass and N-mineralization

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绿黄隆、甲黄隆在江苏省农区5种土壤中残留活性的研究

采用改进的玉米主根长土培生测法，研究绿黄隆、甲黄隆在江苏省典型农区土壤中残留活性。结果表明，两种除草剂在５种土壤中剂量与玉米主根长抑制率之间皆达极显著相关，土壤ｐＨ和有机质含量是主要影响因素，碱性轻质土壤中活性较高，酸性重质土壤中活性较低，活性大小顺序为：黄潮土＞高沙土＞砂姜黑土＞滨海盐土＞太湖水稻土。     

Persistence of metsulfuron‐methyl in two soils

Abstract

The persistence of metsulfuron‐methyl in sandy loam and clay soil incubated at different temperatures and moistures contents was investigated under laboratory conditions using longbean (Vigna sesquipedalis L.) as bioassay species. A significant degradation of metsulfuron‐methyl was observed in non‐autoclaved soil rather than the autoclaved soil sample. At higher temperature, the degradation rate in non‐autoclaved soil improved with increasing soil moisture content. In non‐autoclaved sandy loam and clay soil, the half‐life was reduced from 9.0 to 5.7 and from 11.2 to 4.6 days, respectively when moisture level of sandy loam increased from 20 to 80% field capacity at 35°C. In the autoclaved soil, herbicide residue seems to have been broken down by non‐biological process. The rate of dissipation was slightly increased after the second application of the herbicide to non‐autoclaved soils but not in autoclaved soil, indicating the importance of microorganisms in the breakdown process.     

Effects of metsulfuron‐methyl on microbial biomass and populations in soils

Abstract

Effects of the herbicide metsulfuron‐methyl on soil microorganisms and their activities in two soils were evaluated under laboratory conditions. Measurements included their populations, soil respiration, and microbial biomass. In the clay soil, bacterial populations decreased with increasing concentration of metsulfuron‐methyl during the first 9 days of incubation but exceeded that of the control soil from day 27 onward. In the sandy loam soil, the herbicide reduced bacterial populations during the first 3 days after application, but these increased to the level of untreated controls after 9 days’ incubation. Fungal populations in both soils increased with increasing metsulfuron‐methyl concentrations, especially in the sandy loam soil. CO₂ evolution was stimulated in both soils in the presence of the herbicide initially, but decreased during days 3 to 9 of the incubation period before increasing again afterward. The presence of metsulfuron‐methyl in the soil increased microbial biomass, except in sandy loam soil at the first day of incubation.     

江苏省主要水稻品种对甲磺隆的敏感性研究

在用土培方法探索水稻土培生物测定条件的基础上，研究了甲磺隆残留对水稻秧苗根系生长的影响。结果表明，采用高沙土，添加法加入甲磺隆，培养时调节土壤含水量３５％左右，恒温培养６ｄ，将获得满意的甲磺隆残留土培生物测定结果；用此方法测得的江苏主要水稻品种对甲磺隆残留的敏感程度呈现：常规粳稻＞糯稻、杂交粳稻＞常规籼稻＞杂交籼稻之趋势；土壤中甲磺隆残留量达０５μｇ／ｋｇ对江苏大多数水稻品种秧苗根系生长有着强烈的抑制作用。     

甲磺隆在土壤腐殖物质中结合残留的动态变化

土壤中14 C 甲磺隆的可提取态残留物随时间延长不断降低 ,而其结合态残留率第 2 8天达最高 .14 C 甲磺隆结合态残留物在土壤腐殖物质中的分布是 :富啡酸 胡敏素 >胡敏酸 .在处理最初 2 8天 ,富啡酸中14 C 甲磺隆结合态残留物不断增大 ,随后减少 ;胡敏素中的结合态残留量在 2 8— 2 2 4天变化不大 .14 C残留物在不同土壤之间的结合及其分布都是有差异的 ,与土壤pH值、粘粒矿物类型等都有密切关系