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Atmospheric wet deposition of nitrogen and sulfur to a typical red soil agroecosystem in Southeast China during the ten-year monsoon seasons (2003-2012)

机译:十年季风季节期间(2003-2012),大气和氮和硫在中国东南典型的红壤农业生态系统中的大气湿沉降

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摘要

Biological processes in agroecosystems have been affected by atmospheric nitrogen (N) and sulfur (S) deposition, but there is uncertainty about their deposition characteristics in the monsoon season. We collected rain samples using an ASP-2 sampler, recorded rainfall and rain frequency by an auto-meteorological experiment sub-station, and determined total N, NO_3~- - N and NH_4~+ - N levels in precipitation with an AutoAnalyzer 3 and SO_4~(2-) - S with a chromatography, in order to characterize the wet deposition of N and S to a typical red soil agroecosystem by a ten-year monitoring experiment in Southeast China. The results indicated that N and S wet deposition had an increased trend with the flux of total N (3.34-65.17 kg ha~(-1) N) and total S (SO_4~(2-) - S) (7.17-23.44 kg ha~(-1) S) during the monsoon seasons. The additional applications of pig mature in 2006 and 2007 led to the peaks of DON (dissolved organic nitrogen) and total N wet deposition. On average, NH_4~+ - N was the major N form, accounting for 48.5% of total N wet deposition and DON was not a negligible N form, accounting for 20.8% during the ten-year monsoon seasons (except 2006 and 2007). Wet deposition of N and S has been intensively influenced by human activities in the monsoon season, and would increase the potential ecological risk in the red soil agricultural ecosystem.
机译:农业生态系统中的生物过程已受到大气中氮(N)和硫(S)沉积的影响,但是在季风季节中它们的沉积特征尚不确定。我们使用ASP-2采样器收集降雨样本,通过自动气象实验分站记录降雨和降雨频率,并使用AutoAnalyzer 3和3确定了降水中的总N,NO_3〜--N和NH_4〜+-N水平。 SO_4〜(2-)-S色谱法,旨在通过在中国东南部进行的十年监测试验,将N和S湿沉降到典型的红壤农业生态系统中。结果表明,随着总氮通量(3.34-65.17 kg ha〜(-1)N)和总硫通量(SO_4〜(2-)-S)(7.17-23.44 kg)的通量,N和S的湿沉降呈增加趋势。 ha〜(-1)S)在季风季节。猪在2006年和2007年成熟的额外应用导致DON(溶解的有机氮)和总氮湿沉降达到峰值。平均而言,NH_4〜+-N是主要的N形态,占总N湿沉降的48.5%,DON是不可忽略的N形态,在十年季风季节(2006和2007年除外)占20.8%。季风季节人类活动强烈地影响了氮和硫的湿沉降,这将增加红壤农业生态系统的潜在生态风险。

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  • 来源
    《Atmospheric environment》 |2014年第1期|121-129|共9页
  • 作者单位

    Institute of Soil Science, Chinese Academy of Sciences, 71st East Beijing Road, Nanjing 210008, PR China,Red Soil Ecological Experiment Station, Chinese Academy of Sciences, Liujiazhan Plantation, Yingtan 335211, PR China,Institute of Soil Science, Chinese Academy of Sciences, 71 East Beijing Road, Nanjing 210008, PR China;

    Institute of Soil Science, Chinese Academy of Sciences, 71st East Beijing Road, Nanjing 210008, PR China,Red Soil Ecological Experiment Station, Chinese Academy of Sciences, Liujiazhan Plantation, Yingtan 335211, PR China,National Engineering and Technology Research Center for Red Soil Improvement, 602nd Nanlian Road, Nanchang 330200, PR China,Institute of Soil Science, Chinese Academy of Sciences, 71 East Beijing Road, Nanjing 210008, PR China;

    Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, 73rd East Beijing Road, Nanjing 210008, PR China;

    Institute of Soil Science, Chinese Academy of Sciences, 71st East Beijing Road, Nanjing 210008, PR China,Red Soil Ecological Experiment Station, Chinese Academy of Sciences, Liujiazhan Plantation, Yingtan 335211, PR China;

    College of Geography Science, Nanjing Normal University, 1st Wenyuan Road, Nanjing 210046, PR China;

    Department of Chemistry and Biochemistry, Old Dominion University, Norfolk 23529, VA, United States;

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

    N and S deposition; Wet deposition; Monsoon season; Red soil farmland; Southeast China;

    机译:氮和硫沉积;湿沉降;季风季节;红壤农田;中国东南;

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