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Effects of three years of simulated nitrogen deposition on soil nitrogen dynamics and greenhouse gas emissions in a Korean pine plantation of northeast China

机译:三年模拟氮沉降对中国东北红松人工林土壤氮动态和温室气体排放的影响

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摘要

Continuously enhanced nitrogen (N) deposition alters the pattern of N and carbon (C) transformations, and thus influences greenhouse gas emissions. It is necessary to clarify the effect of N deposition on greenhouse gas emissions and soil N dynamics for an accurate assessment of C and N budgets under increasing N deposition. In this study, four simulated N deposition treatments (control [CK: no N addition], low-N [L: 20 kg N ha~(-1) yr~(-1)], medi-um-N [M: 40 kg N ha~(-1) yr~(-1)], and high-N [H: 80 kg N ha~(-1) yr~(-1)]) were operated from 2014. Carbon dioxide, methane and nitrous oxide fluxes were monitored semimonthly, as were soil variables such as temperature, moisture and the concentrations of total dissolved N (TDN), NO_3~-, NO_2~-, NH_4~+, and dissolved organic N (DON) in soil solutions. The simulated N deposition resulted in a significant increase in TDN, NOf and DON concentrations in soil solutions. The average CO_2 emission rate ranged from 222.6 mg CO_2 m~2 h~(-1) in CK to 233.7 mg CO_2 m~2 h~(-1) in the high-N treatment Three years of simulated N deposition had no effect on soil CO_2 emission, which was mainly controlled by soil temperature. The mean N_2O emission rate during the whole 3 years was 0.02 mg N_2O m~2 h~(-1) for CK, which increased significantly to 0.05 mg N_2O m~2 h~(-1) in the high-N treatment. The N_2O emission rate positively correlated with NH_4~+ concentrations, and negatively correlated with soil moisture. The average CH_4 flux during the whole 3 years was -0.74 ug CH_4 m~2 h~(-1) in CK, which increased to 1.41 μg CH_4 m~(-2) h~(-1) in the low-N treatment CH_4 flux positively correlated with NO3 concentrations. These results indicate that short-term N deposition did not affect soil CO_2 emissions, while CH_4 and N_2O emissions were sensitive to N deposition.
机译:不断增加的氮(N)沉积会改变氮和碳(C)转化的方式,从而影响温室气体排放。有必要弄清楚氮沉降对温室气体排放和土壤氮动力学的影响,以便在氮沉降增加的情况下准确评估碳和氮的预算。在这项研究中,进行了四种模拟的N沉积处理(对照[CK:不添加N],低氮[L:20 kg N ha〜(-1)yr〜(-1)],med-um-N [M:从2014年开始运行40 kg N ha〜(-1)yr〜(-1)]和高氮[H:80 kg N ha〜(-1)yr〜(-1)]。二氧化碳,甲烷每半个月监测一次和一氧化二氮通量,以及土壤变量,例如温度,湿度和土壤溶液中总溶解氮(TDN),NO_3〜-,NO_2〜-,NH_4〜+和溶解有机氮(DON)的浓度。模拟的氮沉降导致土壤溶液中TDN,NOf和DON浓度显着增加。在高氮处理中,平均CO_2排放速率从CK的222.6 mg CO_2 m〜2 h〜(-1)到高氮处理中的233.7 mg CO_2 m〜2 h〜(-1)不等。土壤CO_2的排放主要受土壤温度控制。 CK的3年平均N_2O排放量为0.02 mg N_2O m〜2 h〜(-1),高氮处理显着增加至0.05 mg N_2O m〜2 h〜(-1)。 N_2O排放速率与NH_4〜+浓度呈正相关,与土壤水分呈负相关。 CK整个3年的平均CH_4通量为-0.74 ug CH_4 m〜2 h〜(-1),低氮处理时增加到1.41μgCH_4 m〜(-2)h〜(-1)。 CH_4通量与NO3浓度呈正相关。这些结果表明,短期氮沉降对土壤CO_2排放没有影响,而CH_4和N_2O排放对氮沉降敏感。

著录项

  • 来源
    《The Science of the Total Environment》 |2017年第31期|1303-1311|共9页
  • 作者单位

    Center for Ecological Research, Northeast Forestry University, Harbin 150040, China;

    Center for Ecological Research, Northeast Forestry University, Harbin 150040, China;

    School of Geography Sciences, Nanjing Normal University, Nanjing 210023, China,Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing210023, China;

    Center for Ecological Research, Northeast Forestry University, Harbin 150040, China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Nitrogen deposition; Nitrogen dynamics; Greenhouse gas; Soil variables;

    机译:氮沉积;氮动力学;温室气体;土壤变量;

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