Quantification of N2O fluxes from soil–plant systems may be biased by the applied gas chromatograph methodology

Author:

Zheng Xunhua,Mei Baoling,Wang Yinghong,Xie Baohua,Wang Yuesi,Dong Haibo,Xu Hui,Chen Guanxiong,Cai Zucong,Yue Jin,Gu Jiangxin,Su Fang,Zou Jianwen,Zhu Jianguo

Publisher

Springer Science and Business Media LLC

Subject

Plant Science,Soil Science

Reference61 articles.

1. Arah JRM, Crichton IJ, Smith KA, Clayton H, Skiba U (1994) Automated gas chromatographic analysis system for micrometeorological measurements of trace gas fluxes. J Geophys Res 99:16593–16598

2. Breuer L, Papen H, Butterbach-Bahl K (2000) N2O emission from tropical forest soils of Australia. J Geophys Res 105:26353–26367

3. Butterbach-Bahl K, Gasche R, Breuer L, Papen H (1997) Fluxes of NO and N2O from temperate forest soils: impact of forest type, N deposition and of liming on the NO and N2O emissions. Nutr Cycl Agroecosys 48:79–90

4. Chen GX, Shang SH, Yu KW, Yu AD, Wu J, Wang YJ (1990) Investigation on the emission of N2O by plant. Chinese J Appl Ecol 1:94–96 (in Chinese)

5. Chen GX, Huang GH, Shang SH, Li N, Wu J, Yu KW, Xu H, Wang YJ, Li L (1992) Measurement of N2O emission from soil, plants and soil–plant systems. In Ghazi A (ed) Proceedings of CEC and P. R. China workshop of contribution to global change. Biosphere atmosphere interactions. Brussels Belgium pp 109–114

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