Evaluation of long-term organic carbon dynamics and organic matter stability in a cultivated paddy soil using a carbon and nitrogen stable isotopes-based model

• Published in: Soil & tillage research Vol. 239; p. 106040
• Main Authors: Samson, Victor Manna, Wei, Yuanhui, Guo, Liming, Liu, Dongming, Heiling, Maria, Dercon, Gerd, Guo, Yuxuan, Mao, Yanling
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-06-2024
• Subjects: Fertilizer; Soil organic matter; Stability; Stable isotopes; Soil organic matter; Stability; Stable isotopes; Fertilizer
• ISSN: 0167-1987; 1879-3444
• DOI: 10.1016/j.still.2024.106040

Understanding soil organic matter (SOM) stability and carbon storage under long-term intensive land management systems is vital for estimating the C sequestration potentials of agricultural lands. Available methods currently used for measuring the stability of SOM, such as radiocarbon dating, are expensive. However, a cost-effective and reliable stable isotope-based model was developed for grasslands which utilizes the C/N ratio and δ15N of soils to determine the stability of SOM. We applied this model to test for the first time its usefulness for evaluating SOM stability in the top and subsoils of a subtropical paddy field cultivated for 37 years. We also compared paddy soil's SOM stability and carbon storage under different fertilizer treatments. Treatments evaluated were a control (CK), inorganic fertilizer (NPK), NPK+cattle manure (NPKM), and NPK+rice straw (NPKS). Results showed that the C/N ratios and δ15N signatures of POM and mOM proved effective in predicting SOM stability as predicted by the model. SOM stability increased with depth across the treatments, especially in NPKM and NPKS in the deeper soil layer compared to CK and NPK. Introducing δ13 C as an indicator further strengthened the model, revealing higher δ13 C accumulation in the subsoils, indicating higher C sequestration. Further insights showed that unlike in the CK treatment, the use of NPKM and NPKS significantly increased SOC accumulation by increasing the proportion of mineral-protected organic matter (mOM) compared to the microbial-accessible particulate organic matter (POM). The abundance of mOM associated with a lower rate of decomposition in the paddy fields and the incorporation of higher 13 C in the subsoils under NPKM and NPKS were key factors that enhanced the long-term increase in organic C and SOM stability. Thus, the stable isotope-based model proved a reliable proxy for estimating SOM stability in paddy fields.
•CN ratio and δ15N is a reliable proxy for estimating soil organic matter stability.•Soil organic matter relative stability increases with depth.•Addition of manure and straw with NPK fertilizer increased organic matter stability.•δ13C enrichment correlates positively with soil organic matter stability.