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Monitoring nitrogen deposition in typical forest ecosystems along a large transect in China
Authors:Wenping Sheng  Guirui Yu  Chunming Jiang  Junhua Yan  Yunfen Liu  Silong Wang  Bing Wang  Junhui Zhang  Chuankuan Wang  Mei Zhou  Bingrui Jia
Institution:1. 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
2. Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang, 110016, People’s Republic of China
3. South China Botany Garden, Chinese Academy of Science, Guangzhou, 510650, People’s Republic of China
4. Institute of Forest Ecology Environment and Protection, Chinese Academy of Forestry, Beijing, 100091, People’s Republic of China
5. College of Forestry, Northeast Forestry University, Harbin, 150040, People’s Republic of China
6. College of Ecology and Environmental Science, Inner Mongolia Agricultural University, Hohhot, 010019, People’s Republic of China
7. Institute of Botany, Chinese Academy of Sciences, Beijing, 100093, People’s Republic of China
Abstract: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.
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