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配施有机肥减少太湖地区稻田土壤硝态氮淋失的机理研究
引用本文:张 敏,姚元林,曾 科,李冰洋,田玉华,尹 斌.配施有机肥减少太湖地区稻田土壤硝态氮淋失的机理研究[J].土壤,2020,52(4):766-772.
作者姓名:张 敏  姚元林  曾 科  李冰洋  田玉华  尹 斌
作者单位:洛阳师范学院,南京信息工程大学,土壤与农业可持续发展国家重点实验室中国科学院南京土壤研究所,土壤与农业可持续发展国家重点实验室中国科学院南京土壤研究所,土壤与农业可持续发展国家重点实验室中国科学院南京土壤研究所
基金项目:国家重点重点研究开发项目
摘    要:采用田间小区试验,设计两种无机氮肥梯度,研究配施有机肥对太湖地区水稻季土壤氮素淋失的影响,并从水/土NO_3~-–N迁移研究其对土壤NO_3~-–N淋失的影响机制。设置的处理有:对照(CK)、常规施氮(CT)、减氮施肥(RT)、常规施氮下配施有机肥(CT+M)、减氮施肥下配施有机肥(RT+M)。结果发现:①除去2015年的CT处理,两年里30 cm处配施有机肥和单施无机肥处理之间的土壤NO_3~-–N淋失均没有显著差异;80 cm处,CT+M处理的NO_3~-–N淋失较CT处理减少41%,RT+M处理较RT处理减少12%。②无机肥处理的田面水NO_3~-–N和土壤淋溶水NO_3~-–N之间存在极显著线性相关,但是有机肥的参与会削弱二者之间的相关性。③配施有机肥有利于土壤有机质含量的提高,CT+M处理的有机质含量较CT处理提高6.7%。0~20 cm土层,配施有机肥处理土壤NO_3~-–N含量明显高于无机肥处理;而20~40 cm土层,二者之间的土壤NO_3~-–N含量差异很小。这表明配施有机肥是通过提高土壤有机质含量,增强土壤表层对NO_3~-–N的吸附固持,从而抑制土壤NO_3~-–N的向下迁移,而不是通过减少田面水NO_3~-–N浓度来实现的。此外,配施有机肥还可以提高土壤质量和水稻产量,促进作物对土壤氮素的吸收,这也是稻田土壤NO_3~-–N淋失减少的一个原因。研究结果为减少农田土壤NO_3~-–N淋失提供了科学依据。

关 键 词:水稻  有机肥  淋溶  机制  太湖地区
收稿时间:2019/4/15 0:00:00
修稿时间:2019/5/23 0:00:00

Study on Mechanism of Reducing Nitrate Leaching with Organic Addition from Paddy Field in Taihu Lake Region
ZHANG Min,YAO Yuanlin,ZENG Ke,LI Bingyang,TIAN Yuhu,YIN Bin.Study on Mechanism of Reducing Nitrate Leaching with Organic Addition from Paddy Field in Taihu Lake Region[J].Soils,2020,52(4):766-772.
Authors:ZHANG Min  YAO Yuanlin  ZENG Ke  LI Bingyang  TIAN Yuhu  YIN Bin
Institution:Luoyang normal university,Luoyang,Nanjing university of information technology,Nanjing,State Key Laboratory of Soil and Sustainable Agriculture,Institute of Soil Science,Chinese Academy of Sciences,State Key Laboratory of Soil and Sustainable Agriculture,Institute of Soil Science,Chinese Academy of Sciences,State Key Laboratory of Soil and Sustainable Agriculture,Institute of Soil Science,Chinese Academy of Sciences
Abstract:Field plot experiment with two N rates was adopted to study the effect of organic addition on nitrogen (N) leaching in rice season of Taihu Lake Region, and the mechanism was also studied through nitrate (NO3--N) migration of water and soil. The results showed that: (1) There was no significant difference of soil NO3--N leaching between organic addition and inorganic fertilizer treatments at 30 cm depth during the two seasons except CT treatment in 2015. NO3--N leaching at 80 cm depth in CT+M was 41% lower than in CT, and RT+M produced 12% lower NO3--N leaching loss compared to RT. (2) Floodwater NO3--N under chemical N treatments was in significant relationship with soil NO3--N leaching, while the involvement of organic fertilizer would weaken the relationship between floodwater NO3--N and soil NO3--N leaching. (3) Organic addition could increase soil organic matter content, and CT+M achieved 6.7% higher SOM than CT. Organic N treatments showed higher soil NO3--N content at 0-20 cm compared to chemical N treatments. And soil NO3--N content at 20-40 cm differed little between organic N and chemical N treatments. These indicated that organic addition enhanced the absorption and fixation of NO3--N by soil through the improved SOM and thus inhibited the migration of NO3--N to deep soil. The reduced NO3--N leaching under organic addition was not achieved by reducing floodwater NO3--N concentration. Additionally, organic addition improved soil quality and rice yield, promoted crop N uptake, and thus could also explain the reduced NO3--N leaching loss. The results provided scientific basis for decreasing NO3--N leaching in farmland.
Keywords:Rice  Organic addition  N leaching  Mechanism  Taihu Lake region
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