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Biodegradation of Atrazine by Agrobacterium radiobacter J14a and Use of This Strain in Bioremediation of Contaminated Soil

机译:农杆菌J14a对阿特拉津的生物降解及其在污染土壤生物修复中的应用

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摘要

We examined the ability of a soil bacterium, Agrobacterium radiobacter J14a, to degrade the herbicide atrazine under a variety of cultural conditions, and we used this bacterium to increase the biodegradation of atrazine in soils from agricultural chemical distribution sites. J14a cells grown in nitrogen-free medium with citrate and sucrose as carbon sources mineralized 94% of 50 μg of [14C-U-ring]atrazine ml−1 in 72 h with a concurrent increase in the population size from 7.9 × 105 to 5.0 × 107 cells ml−1. Under these conditions cells mineralized the [ethyl-14C]atrazine and incorporated approximately 30% of the 14C into the J14a biomass. Cells grown in medium without additional carbon and nitrogen sources degraded atrazine, but the cell numbers did not increase. Metabolites produced by J14a during atrazine degradation include hydroxyatrazine, deethylatrazine, and deethyl-hydroxyatrazine. The addition of 105 J14a cells g−1 into soil with a low indigenous population of atrazine degraders treated with 50 and 200 μg of atrazine g−1 soil resulted in two to five times higher mineralization than in the noninoculated soil. Sucrose addition did not result in significantly faster mineralization rates or shorten degradation lag times. However, J14a introduction (105 cells g−1) into another soil with a larger indigenous atrazine-mineralizing population reduced the atrazine degradation lag times below those in noninoculated treatments but did not generally increase total atrazine mineralization.
机译:我们检查了土壤细菌,土壤杆菌属细菌J14a在多种文化条件下降解除草剂r去津的能力,并使用该细菌增加了农业化学分布场所土壤中at去津的生物降解能力。在无氮培养基中以柠檬酸盐和蔗糖为碳源生长的J14a细胞在72 h内矿化了50μg[ 14 CU-ring] at去津ml -1 的94%。同时人口数量从7.9×10 5 增加到5.0×10 7 个细胞ml -1 。在这些条件下,细胞使[ethyl- 14 C] r去津矿化,并将大约30%的 14 C掺入J14a生物质中。在没有其他碳和氮源的培养基中生长的细胞降解了at去津,但细胞数量并未增加。 J14a在at去津降解期间产生的代谢产物包括羟基去津,脱乙基at去津和脱乙基羟基-去津。将10 5 J14a细胞g −1 添加到土壤中具有低原生indigenous去津降解剂的土壤中,分别用50和200μg的at去津g −1 土壤导致的矿化度比未接种土壤高2至5倍。蔗糖的添加不会导致显着更快的矿化速率或缩短降解滞后时间。但是,将J14a引入(10 5 细胞g −1 )到另一种具有大量天然阿特拉津矿化人口的土壤中,可降低阿特拉津降解的滞后时间,低于未接种处理的时间,但确实如此通常不会增加总at去津的矿化度。

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