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Effects of planting Phragmites australis on nitrogen removal, microbial nitrogen cycling, and abundance of ammonia-oxidizing and denitrifying microorganisms in sediments

机译:种植芦苇对沉积物中氮的去除,微生物氮循环以及氨氧化反硝化微生物的丰度的影响

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We examined the effect of planting an emergent aquatic plant (Phragmites australis) on nitrogen removal from sediments using a 42-d pot experiment. The experimental pot systems comprised two types of sediments planted with and without young P. australis. Total nitrogen (total N), total dissolved N, and NH4-N in the sediments decreased markedly after planting. In contrast, those levels decreased only slightly in the unplanted sediments. The decrease in total N in the P. australis-planted sediments was 7-20 times those in the unplanted sediments. Abundances of bacterial 16S rRNA, archaeal 16S rRNA, ammonia-oxidizing bacterial ammonia monooxygenase (amoA), ammonia-oxidizing archaeal amoA, and denitrifying bacterial nitrite reductase (nirK) genes increased significantly in sediments after planting. Phragmites australis appears to have released oxygen and created a repeating cycle of oxidizing and reducing conditions in the sediments. These conditions should promote mineralization of organic N, nitrification, and denitrification in the sediments. Phragmites australis absorbed bioavailable nitrogen generated by microbial nitrogen metabolism. During the 42-d period after planting, 31-44% of total N was removed by microbial nitrogen cycling, and 56-69% was removed via absorption by P. australis. These results suggest that planting P. australis can increase microbial populations and their activities, and that nitrogen removal can be accelerated by the combined functions of P. australis and microorganisms in the sediment. Thus, planting P. australis has considerable potential as an effective remediation technology for eutrophic sediments.
机译:我们使用42天盆栽试验研究了种植紧急水生植物(Phragmites australis)对沉积物中氮去除的影响。实验盆栽系统包括两种类型的沉积物,有或没有幼小的P. australis。种植后,沉积物中的总氮(总氮),总溶解氮和NH4-N显着下降。相反,这些水平在未种植的沉积物中仅略有下降。南极假山种植的沉积物中总氮的减少是未种植的沉积物中的总氮的7-20倍。种植后,沉积物中的细菌16S rRNA,古细菌16S rRNA,氨氧化细菌氨单加氧酶(amoA),氨氧化细菌古细菌amoA和反硝化细菌亚硝酸还原酶(nirK)基因的丰度显着增加。芦苇似乎释放了氧气,并在沉积物中形成了氧化和还原条件的重复循环。这些条件应促进沉积物中有机氮的矿化,硝化作用和反硝化作用。芦苇吸收微生物氮代谢产生的生物利用氮。在播种后的42 d期间,通过微生物氮循环去除了总氮的31-44%,并通过澳大利亚假单胞菌的吸收去除了56-69%。这些结果表明,种植澳洲假单胞菌可以增加微生物种群及其活性,并且可以通过澳洲假单胞菌和沉积物中微生物的联合功能来加速脱氮。因此,作为一种对富营养化沉积物的有效修复技术,种植澳大利亚假单胞菌具有巨大潜力。

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