Journal
PLANT AND SOIL
Volume 445, Issue 1-2, Pages 101-112Publisher
SPRINGER
DOI: 10.1007/s11104-019-04030-z
Keywords
Paddy soil; Rhizodeposition; C flow; C-13-CO2 pulse labeling; N fertilization
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Funding
- National Key Research and Development Program [2016YFE0101100]
- Australia-China Joint Research Centre-Healthy Soils for Sustainable Food Production and Environmental Quality [ACSRF48165]
- National Natural Science Foundation of China [41671292, 41771337]
- Hunan Province Base for Scientific and Technological Innovation Cooperation [2018WK4012]
- Open Fund of Key Laboratory of Agroecological Processes in Subtropical Region, Chinese Academy of Sciences [ISA2017301]
- Innovation Groups of Natural Science Foundation of Hunan Province [2019JJ10003]
- Youth Innovation Team Project of ISA, CAS [2017QNCXTD_GTD]
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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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