Mineralization Patterns of Maize Straw in Fluvio-Aquatic Soil as Determined by Isotopic Traces
Lixia Zhu,
Jutian Chen,
Lili Li,
Fuli Zhang and
Tianxue Liu
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Lixia Zhu: College of Life Science and Agronomy, Zhoukou Normal University, Zhoukou 466001, China
Jutian Chen: College of Life Science and Agronomy, Zhoukou Normal University, Zhoukou 466001, China
Lili Li: College of Life Science and Agronomy, Zhoukou Normal University, Zhoukou 466001, China
Fuli Zhang: College of Life Science and Agronomy, Zhoukou Normal University, Zhoukou 466001, China
Tianxue Liu: National Key Laboratory of Wheat and Maize Crop Science, Agricultural College of Henan Agricultural University, Zhengzhou 450002, China
Sustainability, 2020, vol. 12, issue 2, 1-13
Abstract:
The mineralization of plant residues results in changes in soil C and N. However, it is difficult to determine the origins of C and N from either soil organic matter mineralization or residue decomposition using traditional methods. An incubation experiment containing two treatments (blank soil (BS) and soil with 6% maize straw (MS)) was conducted to assess the contributions of maize straw to gas emissions, and to soil organic carbon (SOC) and total nitrogen (TN) using isotopic tracers. About 11.5% of maize straw C was sequestered in soil, the cumulative amount of C emitted from MS was 2.5-fold higher than that in BS treatment. A positive priming effect of maize straw on native SOC in the first 14 days was observed, and then became negative, indicating the potential for a positive balance of SOC storage. Cumulative N 2 O emissions in MS markedly decreased by 22.4% compared with BS, and the loss of N via N 2 O in MS was approximately 3.3%. Maize straw significantly increased soil TN and contributed 15.8% to TN at day 120. Our study clearly demonstrated that the different dynamics of 13 C and 15 N in the soils and gases indicated differences of maize straw C and N during decomposition. Maize straw C preferred to contribute to CO 2 emissions, while maize straw N contributed more to soil TN.
Keywords: CO 2 emissions; isotopic signature; N 2 O emissions; priming effect; soil organic matter (search for similar items in EconPapers)
JEL-codes: O13 Q Q0 Q2 Q3 Q5 Q56 (search for similar items in EconPapers)
Date: 2020
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Persistent link: https://EconPapers.repec.org/RePEc:gam:jsusta:v:12:y:2020:i:2:p:621-:d:308794
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