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辽河口湿地沉积物硝化细菌及硝化作用研究
引用本文:白洁,陈春涛,赵阳国,田伟君,董晓,尹宁宁.辽河口湿地沉积物硝化细菌及硝化作用研究[J].环境科学,2010,31(12):3011-3017.
作者姓名:白洁  陈春涛  赵阳国  田伟君  董晓  尹宁宁
作者单位:1. 中国海洋大学环境科学与工程学院,青岛,266100;海洋环境与生态教育部重点实验室,青岛,266100
2. 中国海洋大学环境科学与工程学院,青岛,266100
基金项目:国家水体污染控制与治理科技重大专项(2008ZX07208-009);国家重点基础研究发展规划(973)项目(2006CB400602)
摘    要:2009年6月和8月,采用现场培养和实验室模拟培养相结合的方法对辽河口湿地表层沉积物硝化细菌数量、硝化速率及影响因素进行了研究.结果表明,辽河口湿地表层沉积物氨氧化细菌(ammonia-oxidizing bacteria,AOB)数量6月在0.54×104~5.69×104个.g-1之间,平均值为(2.21±2.32)×104个.g-1,8月在1.90×104~7.90×104个.g-1之间,平均值为(3.61±2.87)×104个.g-1;沉积物潜在硝化速率6月在9.72~16.45 mmol.(m2.h)-1之间,平均值为(12.54±3.14)mmol.(m2.h)-1,8月在14.66~24.62 mmol.(m2.h)-1之间,平均值为(18.71±4.21)mmol.(m2.h)-1;净硝化作用速率6月(S1站)为0.41 mmol.(m2.h)-1,8月在0.20~0.53 mmol.(m2.h)-1之间,平均值为(0.35±0.16)mmol.(m2.h)-1.潜在硝化速率显著高于净硝化速率,AOB数量、净硝化作用速率和潜在硝化作用速率均表现为8月高于6月,芦苇根际效应对硝化作用有促进作用.通过SPSS 13.0软件统计分析,表明影响辽河口湿地表层沉积物硝化作用的主要环境因子有上覆水NH 4+-N浓度和沉积物pH、有机质、总氮(TN)、总磷(TP)、NH 4+-N含量以及AOB数量(p0.05),其中上覆水NH 4+-N浓度和沉积物总磷(TP)、NH 4+-N含量对硝化作用影响较大,是辽河口湿地硝化作用影响的关键因素.根据研究结果估算辽河口湿地沉积物硝化作用每天可以将1.14×105kg的NH 4+-N转化为NO 3--N,对河口湿地氮的循环具有重要意义.

关 键 词:辽河口湿地  沉积物  硝化作用  氨氧化细菌(AOB)  影响因素
收稿时间:2010/1/15 0:00:00
修稿时间:2010/3/17 0:00:00

Studies on Nitrobacteria and Nitrification in Liaohe Estuary Wetland Sediments
BAI Jie,CHEN Chun-tao,ZHAO Yang-guo,TIAN Wei-jun,DONG Xiao and YIN Ning-ning.Studies on Nitrobacteria and Nitrification in Liaohe Estuary Wetland Sediments[J].Chinese Journal of Environmental Science,2010,31(12):3011-3017.
Authors:BAI Jie  CHEN Chun-tao  ZHAO Yang-guo  TIAN Wei-jun  DONG Xiao and YIN Ning-ning
Institution:College of Environmental Science and Engineering, Ocean University of China, Qingdao 266100, China. baijie@ouc.edu.cn
Abstract:Nitrobacteria, nitrification and its impact factors were discussed based on the method of on-site incubation and laboratory simulation in Liaohe estuary wetland sediments in June and August 2009, respectively. The results showed that the number of ammonia-oxidizing bacteria (AOB) ranged from 0.54×104 to 5.69×104 cells·g-1 with an average of (2.21±2.32)×104 cells·g-1 in June and ranged from 1.90×104 to 7.90×104 cells·g-1 with an average of (3.61±2.87)×104 cells·g-1 in August. The potential nitrification rates ranged from 9.72 to 16.45 mmol·(m2·h)-1 with an average of (12.54±3.14) mmol·(m2·h)-1 in June and ranged from 14.66 to 24.62 mmol·(m2·h)-1 with an average of (18.71±4.21) mmol·(m2·h)-1 in August. The net nitrification rates were 0.41 mmol·(m2·h)-1 in June and ranged from 0.20 to 0.53 mmol·(m2·h)-1 with an average of (0.35±0.16) mmol·(m2·h)-1 in August. The potential nitrification rates were apparently higher than the net nitrification rates. The AOB abundance and nitrification rates were all higher in August than in June. Ammonia concentration in the overlying water, pH, organic matter, total nitrogen content, total phosphorus content, ammonia nitrogen content and the number of AOB in sediments were the main environmental impact factors on nitrification by SPSS 13.0 statistical analysis (p<0.05), and it also showed ammonia concentration in the overlying water, total phosphorus content and ammonia nitrogen content in sediments were key impact factors on nitrification by partial correlation analysis. The flux of transformed ammonium into nitrate by nitrification process was 1.14×105 kg per day, suggesting that nitrification was important on nitrogen cycle in Liaohe estuary wetland sediments.
Keywords:Liaohe estuary wetland  sediments  nitrification  ammonia-oxidizing bacteria(AOB)  impact factors
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