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Monitoring nitrogen deposition in typical forest ecosystems along a large transect in China

机译:监测中国大型样带典型森林生态系统中的氮沉降

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摘要

The nitrogen (N) deposition fluxes were investigated in eight typical forest ecosystems along the North-South Transect of Eastern China (NSTEC; based on the ChinaFLUX network) by ion-exchange resin (IER) columns from May 2008 to April 2009. Our results demonstrated that the method of IER columns was both labor cost saving and reliable for measuring dissolved inorganic nitrogen (DIN) deposition at the remote forest stations. The deposition of DIN in the throughfall ranged from 1.3 to 29.5 kg N ha~(-1) a~(-1), increasing from north to south along NSTEC. The relatively high average ratio of ammonium to nitrate in deposition (1.83) indicated that the N deposition along the NSTEC in China mostly originated in farming and animal husbandry rather than in industry and vehicle activities. For seasonal variability, the DIN deposition showed a single peak in the growing season in the northern part of NSTEC, while, in the southern part, it exhibited double-peaks in the early spring and the mid-summer, respectively. On the annual scale, the DIN deposition variations of the eight sites could be mainly explained by precipitation and the distances from forest stations to provincial capital cities. Dissolved inorganic nitrogen (DIN) ? Ion-exchange resin (IER) ? Forest ecosystem ? North-South Transect
机译:用离子交换树脂(IER)柱研究了华东地区南北样带(NSTEC;基于ChinaFLUX网络)的八个典型森林生态系统中的氮(N)沉积通量,时间为2008年5月至2009年4月。我们的结果证明IER柱的方法既节省人工成本,又可用于测量偏远森林站的溶解无机氮(DIN)沉积的可靠性。 DIN在穿透物中的沉积量为1.3至29.5 kg N ha〜(-1)a〜(-1),沿着NSTEC从北向南增加。沉积物中铵与硝酸盐的平均比率较高(1.83),表明中国沿NSTEC的氮沉积主要起源于农业和畜牧业,而不是工业和车辆活动。对于季节变化,在NSTEC的北部,DIN沉积物在生长季节显示出一个高峰,而在南部,早期的春季和仲夏则表现出双峰。在年尺度上,这八个地点的DIN沉积变化主要可以通过降水和从林站到省会城市的距离来解释。溶解的无机氮(DIN)离子交换树脂(IER)森林生态系统?南北样带

著录项

  • 来源
    《Environmental Monitoring and Assessment》 |2013年第1期|833-844|共12页
  • 作者单位

    Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, People's Republic of China;

    Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, People's Republic of China;

    Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, People's Republic of China;

    South China Botany Garden, Chinese Academy of Science, Guangzhou 510650, People's Republic of China;

    Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, People's Republic of China;

    Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, People's Republic of China;

    Institute of Forest Ecology Environment and Protection,Chinese Academy of Forestry,Beijing 100091, People's Republic of China;

    Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, People's Republic of China;

    College of Forestry, Northeast Forestry University,Harbin 150040, People's Republic of China;

    College of Ecology and Environmental Science,Inner Mongolia Agricultural University,Hohhot 010019,People's Republic of China;

    Institute of Botany, Chinese Academy of Sciences,Beijing 100093, People's Republic of China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    dissolved inorganic nitrogen (DIN); ion-exchange resin (IER); forest ecosystem; north-south transect of eastern China (NSTEC); ChinaFLUX;

    机译:溶解的无机氮(DIN);离子交换树脂(IER);森林生态系统;中国东部的南北向样带(NSTEC);中国通量;

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