中国农业科学 ›› 2019, Vol. 52 ›› Issue (14): 2468-2483.doi: 10.3864/j.issn.0578-1752.2019.14.007

• 土壤肥料·节水灌溉·农业生态环境 • 上一篇    下一篇

典型红壤不同形态氮素迁移对长期施肥制度的响应

申凤敏1,姜桂英1(),张玉军1,2,刘芳1,刘世亮1(),柳开楼3   

  1. 1河南农业大学资源与环境学院,郑州 450002
    2郑州市城市园林科学研究所,郑州 450051
    3江西省红壤研究所,江西进贤 331717
  • 收稿日期:2019-01-22 接受日期:2019-04-11 出版日期:2019-07-16 发布日期:2019-07-26
  • 通讯作者: 姜桂英,刘世亮
  • 作者简介:申凤敏,E-mail: shenfengmin@henau.edu.cn。
  • 基金资助:
    国家重点研发计划重点专项(2016YFD0300803);国家自然科学基金(41401327);河南省教育厅基金(14B210024)

Response of Different Forms of Nitrogen Migration in Typical Red Soil to Long-Term Different Fertilization Systems

SHEN FengMin1,JIANG GuiYing1(),ZHANG YuJun1,2,LIU Fang1,LIU ShiLiang1(),LIU KaiLou3   

  1. 1College of Resources and Environmental Sciences, Henan Agricultural University, Zhengzhou 450002
    2Zhengzhou Institute of Urban Landscape and Architecture, Zhengzhou 450051
    3Jiangxi Institute of Red Soil, Jinxian 331717, Jiangxi
  • Received:2019-01-22 Accepted:2019-04-11 Online:2019-07-16 Published:2019-07-26
  • Contact: GuiYing JIANG,ShiLiang LIU

摘要:

【目的】基于长期定位试验,探讨典型红壤水稻土不同施肥制度下不同形态土壤氮素迁移特征,为红壤水稻土氮肥合理施用提供理论依据。【方法】选取始于1981年的进贤红壤长期定位试验站4个典型施肥处理,分别为不施肥对照(CK)、施氮磷钾肥(NPK)、氮磷钾配施秸秆(NPKS)、氮磷钾配施有机肥(NPKSM),测定并分析0—10 cm、10—20 cm、20—40 cm和40—60 cm土层土壤全氮(TN)、碱解氮(AN)、硝态氮(NO3 --N)、铵态氮(NH4 +-N)、可溶性有机氮(DON)和微生物生物量氮(SMBN)变化特征。 【结果】不同处理不同形态氮素基本均随土层加深呈下降趋势,但不同形态氮素在不同层次下降特征不同。其中有效态氮,如AN、NO3 --N、NH4 +-N、DON和SMBN主要集中分布在0—20 cm土层,且20—60 cm土层含量较0—20 cm明显降低;而TN在表层0—40 cm土层变化不明显。与CK相比,施肥处理可不同程度地提高0—60 cm各土层各形态氮素含量。其中NPKSM处理显著提高各形态氮素含量,其次为NPKS和NPK处理。相同处理下,TN在0—40 cm土层变化不明显;但在0—60 cm土层TN含量均表现为NPKSM>NPKS>NPK>CK。各处理AN含量随土层深度增加降低幅度显著,其中,20—40 cm土层AN含量相比10—20 cm土层分别降低了42%(CK)、50%(NPK)、44%(NPKS)、44%(NPKSM)。各处理不同土层NO3 --N和NH4 +-N含量均以NPKSM处理显著高于其他处理;其中40—60 cm土层中NO3 --N和NH4 +-N与0—10 cm土层相比,NH4 +-N含量下降幅度更大,分别为51%(CK)、48%(NPK)、54%(NPKS)、36%(NPKSM),且NO3 --N和NH4 +-N均以NPKS处理下降幅度最大,NPKSM处理最小。各处理DON含量在0—20 cm土层差异显著,且均以化肥与有机肥配施处理显著高于其他处理;CK和NPK处理40—60 cm土层的DON含量较20—40 cm略有增加,但NPKS和NPKSM处理则显著降低。各处理SMBN在10—20 cm土层差异最大,表现为NPKSM>NPKS>NPK>CK。相同处理下各形态氮素占TN的比例随土层深度的增加而下降,其中在0—20 cm土层各比例变化较明显;整体上NPKS与NPKSM处理的SMBN占TN比例较高,为2%—4%。耕层土壤(0—20 cm)的TN、AN、NO3 --N、DON和SMBN两两之间均存在显著的正相关关系(P≤0.05),其中TN、DON、AN与SMBN之间存在极显著正相关关系(P≤0.01)。施肥处理(NPK、NPKS、NPKSM)较不施肥处理(CK)可显著提高早、晚稻稻谷、稻草产量和总生物量及其相应的氮吸收量,其中以NPKSM处理最高;但NPKSM处理的无机氮残留量及氮表观损失也显著高于其他处理。 【结论】不同施肥处理对各形态氮素的影响主要集中在土壤耕层(0—20 cm),且各形态氮素含量整体上随土层深度的增加而降低,化肥与有机肥配施可以更好改善红壤区各土层氮素的供应情况;同时化肥与有机肥配施能显著提高作物产量及其氮吸收量,但也增加了其无机氮残留量及氮表观损失量。

关键词: 长期施肥, 红壤, 不同形态氮素, 迁移, 水稻

Abstract:

【Objective】 This study was aimed to explore the characteristics of different nitrogen forms migration under different fertilizations in typical red soil, so as to provide theoretical basis for rational amount of applied nitrogen in red soil region. 【Method】 Based on the long-term experiment site located at Jinxian, Jiangxi province, four typical treatments were chosen as: (1) no fertilization (CK); (2) mineral nitrogen, phosphorus, potassium (NPK); (3) NPK combined with straw (NPKS); (4) NPK combined with pig manure and straw (NPKSM). Four levels of soil samples of 0-10 cm, 10-20 cm, 20-40 cm and 40-60cm were collected from each treatment. Soil total nitrogen (TN), alkali-hydrolyzable nitrogen (AN), nitrate nitrogen (NO3 --N), ammonium nitrogen (NH4 +-N), dissolved organic nitrogen (DON) and microbial biomass nitrogen (SMBN) were measured and analyzed. 【Result】 The results showed that the content of nitrogen forms under different treatments decreased with soil depth, while the different nitrogen forms demonstrated different characteristics in different soil layers. The available nitrogen forms (e.g. AN, NO3 --N, NH4 +-N, DON and SMBN) were concentrated at 0-20 cm soil layers, and their content obviously decreased in 20-60 cm compared with 0-20 cm under all treatments. The TN content in 0-40 cm layers was no significantly change. The fertilizer treatments (i.e. NPK, NPKS and NPKSM) could improve all nitrogen forms content compared with CK, which was the highest under NPKSM treatment. The TN content was little change under the same treatment in 0-40 cm, while the TN content was ordered as NPKSM>NPKS>NPK>CK in 0-60 cm. The AN content under the same treatment was obviously decreased with soil depths. Therein, compared with the AN content in 10-20 cm, which in 20-40 cm was decreased by 42% (CK), 50% (NPK), and 44% (NPKS, NPKSM), respectively. The NO3 --N and NH4 +-N content were highest under NPKSM treatment in each soil layers. Therein, the drop of NH4 +-N between 40-60 cm and 0-10 cm was higher than that of NO3 --N, which ordered as 54% (NPKS)>51% (CK)>48% (NPK)>36% (NPKSM). The DON content was significantly different among the treatments in 0-20 cm, and which was higher under the treatment with mineral fertilizer combined with organic fertilizer. The DON content under CK and NPK treatments in 40-60 cm was increased slightly, while significantly decreased under NPKS and NPKSM treatments. The SMBN was significantly different among treatments in 10-20 cm layer compared with other soil layers, and ordered as NPKSM>NPKS>NPK>CK. The proportion of each form of nitrogen to total nitrogen was decreased with soil depth. There was significantly positive correlation between TN, AN, NO3 --N, DON and SMBN at 0-20 cm (P≤0.05), among which TN, DON, AN and SMBN existed very significant positive correlation (P≤0.01). The early, late rice grain yield, straw yield, total biomass, and their nitrogen accumulation were significantly higher under fertilization treatments (i.e. NPK, NPKS, and NPKSM) than that under CK treatment, which was the highest under NPKSM treatment. Moreover, the residual mineral nitrogen and apparent nitrogen loss were also highest under NPKSM treatment. 【Conclusion】 In red soil, the effect of fertilization on nitrogen form focused on the upper layer (e.g. 0-20 cm). All the nitrogen forms content under all treatments decreased with soil depths. All forms of nitrogen content at 0-60 cm was improved under NPKSM. Meanwhile, the crop yield and their nitrogen accumulation were significantly increased under NPKSM treatment, so did with the residual mineral nitrogen and apparent nitrogen loss.

Key words: long-term fertilization, red soil, various forms of nitrogen, migration, rice