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应用生态学报 ›› 2023, Vol. 34 ›› Issue (2): 405-414.doi: 10.13287/j.1001-9332.202302.012

• 研究论文 • 上一篇    下一篇

氮输入对罗时江湿地沉积物N2O生成过程及酶活性的影响

李佳琛, 侯磊, 王艳霞, 梁启斌*   

  1. 西南林业大学生态与环境学院, 昆明 650224
  • 收稿日期:2022-06-06 接受日期:2022-11-17 出版日期:2023-02-15 发布日期:2023-08-15
  • 通讯作者: *E-mail: qbliang@swfu.edu.cn
  • 作者简介:李佳琛, 女, 1998年生, 硕士研究生。主要从事氮的地球化学循环过程研究。E-mail: lijiachen0411@126.com
  • 基金资助:
    国家自然科学基金项目(41663016,22066023)和云南省教育厅科学研究基金项目(2021Y233)

Effects of nitrogen input on N2O production and enzyme activity in Luoshijiang Wetland sediments, China

LI Jiachen, HOU Lei, WANG Yanxia, LIANG Qibin*   

  1. College of Ecology and Environment, Southwest Forestry University, Kunming 650224, China
  • Received:2022-06-06 Accepted:2022-11-17 Online:2023-02-15 Published:2023-08-15

摘要: 以洱海上游的罗时江湿地表层沉积物(0~5 cm)为研究对象,设置不同浓度(0、1、5和25 mg·kg-1)的硝态氮(NO3--N)和铵态氮(NH4+-N)输入,采用抑制剂法研究沉积物中硝化作用、反硝化作用、硝化细菌反硝化作用和其他作用对N2O产生率的贡献,探讨N2O生成与沉积物中羟胺还原酶(HyR)、硝酸还原酶(NAR)、一氧化氮还原酶(NOR)和氧化亚氮还原酶(NOS)活性的关系。结果表明: NO3--N输入显著增加了沉积物N2O总产生率(1.51~11.35 nmol·kg-1·h-1),表现为N2O释放;NH4+-N输入降低了沉积物N2O总产生率(-0.80~-0.54 nmol·kg-1·h-1),N2O由释放转为吸收。NO3--N输入未改变硝化作用和硝化细菌反硝化作用对N2O生成贡献的主导地位,其贡献率分别提高至69.5%和56.5%;NH4+-N输入明显改变了沉积物中N2O生成过程,硝化作用和硝化细菌反硝化作用由N2O释放转为吸收。沉积物中N2O总产生率与NO3--N输入量呈正相关,NO3--N输入显著增加了沉积物中NOR活性,降低了NOS活性,进而促进了N2O生成;沉积物中N2O总产生率与NH4+-N输入量呈负相关,NH4+-N输入显著增加了HyR和NOR活性,降低了NAR活性,进而抑制了N2O生成。不同形态、浓度的氮输入通过影响沉积物中的酶活性,进而改变了N2O生成的贡献程度及贡献模式,NO3--N输入显著促进N2O生成,表现为N2O“源”,NH4+-N输入抑制N2O生成,由N2O“源”转为“汇”。

关键词: N2O, 氮输入, 酶活性, 湿地沉积物

Abstract: We examined the effects of nitrate (NO3--N) and ammonium (NH4+-N) input at different concentrations (0, 1, 5 and 25 mg·kg-1) on N2O production rate from the surface sediment (0-5 cm) of Luoshijiang Wetland, located upstream from Lake Erhai. The contribution of nitrification, denitrification, nitrifier denitrification, and other factors to the N2O production rate in sediments was studied by the inhibitor method. The relationships between N2O production and the activities of hydroxylamine (HyR), nitrate (NAR), nitric oxide (NOR), and nitrous oxide (NOS) reductases in sediments were analyzed. We found that NO3--N input significantly increased total N2O production rate (1.51-11.35 nmol·kg-1·h-1), which led to N2O release, whereas NH4+-N input decreased that (-0.80 to -0.54 nmol·kg-1·h-1), causing N2O absorption. NO3--N input did not change the dominant roles of nitrification and nitrifier denitrification in N2O production in sediments, but increased the contributions of these two factors to 69.5% and 56.5%, respectively. The NH4+-N input significantly changed N2O gene-ration process, and the nitrification and nitrifier denitrification changed from N2O release to uptake. There was a positive correlation between total N2O production rate and NO3--N input. NO3--N input significantly increased NOR activity and decreased NOS activity, thereby promoting N2O production. The total N2O production rate in sediments was negatively correlated with NH4+-N input. NH4+-N input significantly increased the activities of HyR and NOR, decreased NAR activity, and inhibited N2O production. Nitrogen inputs with different forms and concentrations changed the degree of contribution and mode of N2O production by affecting enzyme activities in sediments. NO3--N input significantly promoted N2O production, acting as a source of N2O, while NH4+-N input inhibited N2O production, resulting in an N2O sink.

Key words: N2O, nitrogen input, enzyme activity, wetland sediment