4.7 Article

Tea plantation destroys soil retention of NO3- and increases N2O emissions in subtropical China

Journal

SOIL BIOLOGY & BIOCHEMISTRY
Volume 73, Issue -, Pages 106-114

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2014.02.016

Keywords

Tea plantation; N-15 tracing; Model; Gross N transformation; NO3- retention; N2O emission

Categories

Funding

  1. National Natural Science Foundation of China [41330744, 41301313, 41301238]
  2. Research Fund of State Key Laboratory of Soil and Sustainable Agriculture
  3. Nanjing Institute of Soil Science
  4. Chinese Academy of Science [0812201211]
  5. Natural Science Foundation of Jiangsu Province [BK20131045]
  6. China Postdoctoral Science Foundation [2013T60550]
  7. Priority Academic Program Development of Jiangsu Higher Education Institutions

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The intensive conversion from woodland to tea plantation in subtropical China might significantly change the potential supply processes and cycling of inorganic Nitrogen (N). However, few studies have been conducted to investigate the internal N transformations involved in the production and consumption of inorganic N and N2O emissions in subtropical soils under tea plantations. In a N-15 tracing experiment, nine tea fields with different plantation ages (1-y, 5-y and 30-y) and three adjacent woodlands were sampled to investigate changes in soil gross N transformation rates in humid subtropical China. Conversion of woodland to tea plantation significantly altered soil gross N transformation rates. The mineralization rate (M-Norg) was much lower in soils under tea plantation (0.53 0.75 mg N kg(-1) d(-1)) than in soil sampled from woodland (1.71 mg N kg(-1), d-1), while the biological inorganic N supply (INS), defined as the sum of organic N mineralized into NH4+ (MNorg) and heterotrophic nitrification (O-Nrec), was not significantly different between soils under woodland and tea plantation, apart from soil under 30-y tea plantation which had the largest INS. Interestingly, the contribution of O-Nrec to INS increased from 19.6% in soil under woodland to 65.0-82.4% in tea-planted soils, suggesting O-Nrec is the dominant process producing inorganic N in tea-planted soils. Meanwhile, the conversion from woodland to tea plantation destroyed soil NO3- retention by increasing O-Nrec, autotrophic nitrification (O-NH4) and abiotic release of stored NOT while decreasing microbial NOT immobilization (I-NO3), resulting in greater NOT production in soil. In addition, long-term tea plantation significantly enhanced the potential release of N2O. Soil C/N was positively correlated with M-Norg and I-NO3, suggesting that an increase in soil C/N from added organic materials (e.g. rice hull) is likely to reduce the increased production of NO3- in the soils under tea plantation. (C) 2014 Elsevier Ltd. All rights reserved.

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