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Survival and Activity of an Atrazine-Mineralizing Bacterial Consortium in Rhizosphere Soil

机译:阿特拉津矿化细菌财团在根际土壤中的存活和活性

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摘要

Plant rhizosphere effects on atrazine degradation were examined in soil inoculated with an atrazine-mineralizing bacterial consortium. The consortium, consisting of three bacterial species, was isolated from an agricultural soil having previous long-term exposure to the herbicide. Atrazine mineralization and metabolite formation were monitored by measuring ~(14)CO_2 evolution from microcosms amended with radiolabeled atrazine and by HPLC of soil extracts. In noninoculated soil, ca. 11% of ~(14)C-chain-labeled atrazine was N-dealkylated, while only 2.4% of the ring-labeled atrazine was mineralized after 5 weeks. Corn plants had no effect on atrazine mineralization or ethyl-side-chain N-dealkylation in noninoculated soils, but the formation of hydroxyatrazine was significantly enhanced in planted soil. Growth of corn in sterilized soil suggested that hydroxyatrazine formation was caused by plant metabolism of atrazine. Introduction of the atrazine-mineralizing consortium into the soil significantly increased the rate of atrazine mineralization in comparison to noninoculated soil. After 4 weeks, 71% of the atrazine was mineralized in nonplanted soil, whereas 84% of the atrazine was mineralized in soil with corn plants. There was no significant difference in the rate of atrazine mineralization by the consortium in nonplanted and planted soil. However, atrazine-mineralizing populations at the end of the incubation were higher in the planted soil, which contained 8.1 x 10~4 degraders g~(-1) of soil versus 2.7 x 10~3 degraders g~(-1) in soil without plants. The results demonstrated that bioaugmentation with the atrazine-mineralizing consortium greatly enhanced the rate of atrazine mineralization. Long-term survival of the consortium and degradation of atrazine to hydroxyatrazine were both enhanced in rhizosphere soil, but corn seedlings had no significant effect on the rate of atrazine mineralization, either by the indigenous microflora or in soil inoculated with atrazine-mineralizing bacteria.
机译:在接种了at去津矿化细菌财团的土壤中检查了植物根际对at去津降解的影响。该财团由三个细菌物种组成,是从以前长期接触除草剂的农业土壤中分离出来的。通过测量〜(14)CO_2从放射性标记的r去津修饰的微观世界中的演变以及土壤提取物的HPLC监测monitored去津的矿化和代谢产物的形成。在未接种的土壤中, 〜(14)C链标记的r去津11%被N-去烷基化,而5周后只有2.4%的环标记的r去津矿化。玉米植物对未接种土壤中的r去津矿化或乙基侧链N-脱烷基化没有影响,但在种植后的土壤中羟基azine去津的形成显着增强。灭菌土壤中玉米的生长表明羟基阿特拉津的形成是由阿特拉津的植物代谢引起的。与未接种土壤相比,将阿特拉津矿化联合体引入土壤显着提高了阿特拉津矿化速率。 4周后,71%的阿特拉津在未种植的土壤中矿化,而84%的阿特拉津在玉米植物的土壤中矿化。在非种植和种植的土壤中,财团对at去津矿化的速率没有显着差异。然而,在培养结束时,阿特拉津矿化的人口在种植的土壤中更高,其土壤含量为8.1 x 10〜4降解物g〜(-1),而土壤中的含量为2.7 x 10〜3降解物g〜(-1)。没有植物。结果表明,用阿特拉津矿化联合体进行生物强化大大提高了阿特拉津矿化的速率。在根际土壤中,财团的长期存活和阿特拉津降解为羟基阿特拉津都得到了增强,但是玉米幼苗对阿特拉津矿化速率的影响不显着,无论是本地菌群还是接种了阿特拉津矿化细菌的土壤。

著录项

  • 来源
    《Environmental Science & Technology》 |1996年第5期|p.1596-1603|共8页
  • 作者

    S. ALVEY; D. E. CROWLEY;

  • 作者单位

    Department of Soil and Environmental Sciences, University of California, Riverside, California 92521;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 环境化学;
  • 关键词

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