Changes in Temperature Sensitivity and Activation Energy of Soil Organic Matter Decomposition in Different Qinghai-Tibet Plateau Grasslands

• Published in: PloS one Vol. 10; no. 7; p. e0132795
• Main Authors: Li, Jie, He, Nianpeng, Wei, Xuehong, Gao, Yang, Zuo, Yao
• Format: Journal Article
• Language: English
• Published: United States Public Library of Science 15.07.2015; Public Library of Science (PLoS)
• Subjects: Activation energy; Alpine environments; Biochemistry; Biogeochemistry; Biology; Carbon; Climate; Climate Change; Decomposition; Deserts; Ecology; Ecosystem biology; Energy; Environmental Monitoring; Global climate; Global temperature changes; Grassland; Grasslands; Hydrogen-Ion Concentration; Hypotheses; Laboratories; Molecular structure; Molecular weight; Natural resources; Organic matter; Organic soils; Oxidation-Reduction; Poaceae; Quality; Respiration; Science; Sensitivity; Soil - chemistry; Soil carbon; Soil organic matter; Soil sciences; Soil temperature; Soils; Studies; Substrates; Temperature; Temperature effects; Thermodynamics; Tibet; Tibetan Plateau
• ISSN: 1932-6203; 1932-6203
• DOI: 10.1371/journal.pone.0132795

Qinghai-Tibet Plateau grasslands are unique geographical regions and store substantial soil organic matter (SOM) in the soil surface, which make them very sensitive to global climate change. Here, we focused on three main grassland types (alpine meadow, steppe, and desert) and conducted a soil incubation experiment at five different temperatures (5, 10, 15, 20, and 25°C) to investigate SOM decomposition rates (R), temperature sensitivity (Q10), and activation energy (Ea). The results showed that grassland type and incubation temperature had significant impact on R (P < 0.001), and the values of R were exponential correlated with incubation temperature in three alpine grasslands. At the same temperature, R was in the following order: alpine meadow > alpinesteppe > alpine desert. The Q10 values differed significantly among different grasslands, and the overall trends were as follows: alpine meadow (1.56 ± 0.09) < alpine steppe (1.88 ± 0.23) < alpine desert (2.39 ± 0.32). Moreover, the Ea values differed significantly across different grassland types (P < 0.001) and increased with increasing incubation time. The exponential negative correlations between Ea and R at 20°C across all grassland types (all Ps < 0.001) indicated that the substrate-quality temperature hypothesis is applicable to the alpine grasslands. Our findings provide new insights for understanding the responses of SOM decomposition and storage to warming scenarios in this Plateau.