Liang Bin, Kang Lingyun, Ren Tao, Junliang Li, Chen Qing, Wang Jingguo
College of Resources and Environmental Sciences, Qingdao Agriculture University, Qingdao 266109, China.
College of Resources and Environmental Sciences, China Agricultural University, Beijing 100193, China.
J Environ Manage. 2015 May 1;154:351-7. doi: 10.1016/j.jenvman.2015.02.045. Epub 2015 Mar 9.
A long-term greenhouse experiment (2004-2012) was conducted with continuous tomato (Lycopersicum esculentum Mill.) plantings to understand the influence of an exogenous nitrogen supply from irrigation water, chemical fertilizer, or organic amendment on the N balance and soluble organic nitrogen (SON). The results from 16 tomato growing seasons indicated that the application of organic amendment (manure and straw) alone (Or-N) resulted in the same yield as the conventional chemical N with organic amendment (Co-N) and the reduced chemical N with organic amendment (Re-N) treatments. The annual apparent N loss was >1000 and 438 kg N ha(-1) in the Co-N and Re-N treatments, respectively. Over the study period, the SON in the 1.8 m soil profile was 1449 and 1978 kg N ha(-1) in the Re-N and Co-N treatments, respectively, it was 1.7- and 2.3-fold higher than that observed in the Or-N treatment, which indicated that SON increased with the chemical N application. The percentage of SON in the cumulative soluble N (SON plus mineral N) ranged from 28% to 44%, and there were no significant differences across the 0-0.6, 0.6-1.2, and 1.2-1.8 m soil profile, which indicated that the leaching and distribution of SON was similar to those of the mineral N in the 0-1.8 m soil profile. We conclude that the mobility of soluble organic N in the 0-1.8 m of the soil was synchronous with the mineral N under a greenhouse production system, and the risk of soluble organic N leaching increased with inorganic N application rate. Therefore, leaching of SON in the intensive agriculture should not be ignored when evaluating the risk of N leaching.
进行了一项长期温室试验(2004 - 2012年),连续种植番茄(Lycopersicum esculentum Mill.),以了解灌溉水、化肥或有机改良剂提供的外源氮供应对氮平衡和可溶性有机氮(SON)的影响。16个番茄生长季的结果表明,单独施用有机改良剂(粪肥和秸秆)(Or - N)的产量与传统化学氮肥配施有机改良剂(Co - N)以及减量化化学氮肥配施有机改良剂(Re - N)处理的产量相同。Co - N和Re - N处理的年表观氮损失分别>1000和438 kg N ha(-1)。在研究期间,Re - N和Co - N处理中1.8 m土壤剖面中的SON分别为1449和1978 kg N ha(-1),比Or - N处理中观察到的SON分别高1.7倍和2.3倍,这表明SON随着化学氮肥施用量的增加而增加。SON在累积可溶性氮(SON加矿质氮)中的百分比范围为28%至44%,在0 - 0.6、0.6 - 1.2和1.2 - 1.8 m土壤剖面中没有显著差异,这表明SON在0 - 1.8 m土壤剖面中的淋溶和分布与矿质氮相似。我们得出结论,在温室生产系统下,0 - 1.8 m土壤中可溶性有机氮的迁移与矿质氮同步,并且可溶性有机氮淋溶风险随着无机氮施用量的增加而增加。因此,在评估氮淋溶风险时,集约化农业中SON的淋溶不容忽视。