4.7 Article

Nitrogen fertilization alters the distribution and fates of photosynthesized carbon in rice-soil systems: a 13C-CO2 pulse labeling study

期刊

PLANT AND SOIL
卷 445, 期 1-2, 页码 101-112

出版社

SPRINGER
DOI: 10.1007/s11104-019-04030-z

关键词

Paddy soil; Rhizodeposition; C flow; C-13-CO2 pulse labeling; N fertilization

资金

  1. National Key Research and Development Program [2016YFE0101100]
  2. Australia-China Joint Research Centre-Healthy Soils for Sustainable Food Production and Environmental Quality [ACSRF48165]
  3. National Natural Science Foundation of China [41671292, 41771337]
  4. Hunan Province Base for Scientific and Technological Innovation Cooperation [2018WK4012]
  5. Open Fund of Key Laboratory of Agroecological Processes in Subtropical Region, Chinese Academy of Sciences [ISA2017301]
  6. Innovation Groups of Natural Science Foundation of Hunan Province [2019JJ10003]
  7. Youth Innovation Team Project of ISA, CAS [2017QNCXTD_GTD]

向作者/读者索取更多资源

Aims Although nitrogen (N) fertilization is widely used to increase rice yield, its impact on the distribution, transformation, and fates of photosynthetic carbon (C) in rice-soil systems is poorly understood. To address this, we quantified the C flows into various pools in a rice-soil system. Methods Rice (Oryza sativa L.) was pulse-labeled with (CO2)-C-13 at the tillering stage. Samples were collected six times during the 26 days following labeling. We quantified the partitioned photosynthesized C into various pools using stable isotopic techniques and estimated C flows. Results Although the net distribution of assimilated C to belowground pools did not change, N fertilization promoted C assimilation in aboveground biomass. C allocation into soil was enhanced by N fertilization during early growth, but decreased during late growth. N fertilization induced higher mass-specific rhizodeposition (per unit root dry weight) and its turnover rate compared with the unfertilized system. However, with higher microbial turnover, the daily C allocation from roots to soil was similar at both fertilization levels. Conclusions Although total C input into soil is enhanced by N fertilization, its further fate is N fertilization independent, thus leading to a net accumulation of C input in rice paddy soil similar to that observed unfertilized soil.

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