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- W4387343395 abstract "<strong class=journal-contentHeaderColor>Abstract.</strong> Understanding the changes in soil organic carbon (SOC) storage and chemical stabilization dynamics is important for accurately predicting ecosystem C sequestration and/or potential C loss, but the relevant information, especially for the intervention of environmental controls on grassland soil is limited in Tibetan plateau regions. Here we used a 9-year two-way factorial experiment involving warming with open top chambers (+1.80 °C in the daytime and +0.77 °C in the nighttime at the soil surface) and multilevel nitrogen (N) enrichment treatments (0, 5, 10, and 15 g m<sup>-2</sup> year<sup>-1</sup>) in the Tibetan plateau to investigate the changes in SOC pool size and chemical structure. 9-year warming treatment significantly decreased SOC stock in the Tibetan grassland. We observed decreasing SOC concentrations which may be related to changes in the C-degrading enzymes. Surprisingly, the SOC molecular structure remained unchanged in all N enrichment and warmed plots, suggesting that both treatments had affected all forms of SOC, from simple and complex polymeric in a similar way. Our results suggest that long-term warming stimulates soil C loss but no preference in SOC loss with different chemical structure." @default.
- W4387343395 created "2023-10-05" @default.
- W4387343395 date "2023-10-04" @default.
- W4387343395 modified "2023-10-05" @default.
- W4387343395 title "Comment on bg-2023-123" @default.
- W4387343395 doi "https://doi.org/10.5194/bg-2023-123-rc2" @default.
- W4387343395 hasPublicationYear "2023" @default.
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