Effect of 9-year water and nitrogen additions on microbial necromass carbon content at different soil depths and its main influencing factors
Microbial necromass carbon (MNC) is a major source of soil organic carbon (SOC) pool, significantly influencing soil carbon sequestration. The effects of long-term water and nitrogen addition on MNC in soils at different depths, as well as their interactions, remain poorly understood. In this study,...
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Veröffentlicht in: | The Science of the total environment 2024-12, Vol.954, p.176825, Article 176825 |
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Zusammenfassung: | Microbial necromass carbon (MNC) is a major source of soil organic carbon (SOC) pool, significantly influencing soil carbon sequestration. The effects of long-term water and nitrogen addition on MNC in soils at different depths, as well as their interactions, remain poorly understood. In this study, we examined the influence of water addition (+51.67 mm), nitrogen addition (25, 50, 100 kg N ha−1 yr−1), and their interactions on MNC accumulation at different soil depths in temperate grasslands. The addition of water and nitrogen over nine years has been observed to exhibit a decreasing trend in the MNC at different soil depths. Notably, MNC in the topsoil layer (0–10 cm) decreased significantly by 18.56 % under low nitrogen addition treatment, while MNC in the subsoil layer (40–60 cm) declined significantly by 27.19 % under high nitrogen addition treatment. Fungal microbial necromass carbon (FNC) contributed 3.25 times more to SOC than bacterial microbial necromass carbon (BNC). In the 0–10 cm soil layer, MNC is primarily governed by both microbial attributes and the physicochemical properties of the soil, in the 20–40 cm soil layer, the physicochemical properties of the soil predominantly control MNC, in the 40–60 cm layer, microbial characteristics exert a more significant influence on MNC. Collectively, our observations suggest that soil MNC decreased with the addition of water and nitrogen in the 0–60 cm soil slope, which could enable the accurate prediction of global change impacts on the accumulation of soil carbon, thus facilitating the implementation of strategies to augment soil carbon sequestration.
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•The soil MNC in the 0–10 cm layer was higher than that in the subsoil layer (20–40 cm, 40–60 cm).•The contribution of FNC to SOC was significantly higher than that of BNC.•Nitrogen addition led to a decrease in MNC accumulation while simultaneously elevating the FNC/BNC ratio.•The regulation mechanisms of MNC vary across different soil depths. |
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ISSN: | 0048-9697 1879-1026 1879-1026 |
DOI: | 10.1016/j.scitotenv.2024.176825 |