Organic carbon mineralization responses to temperature increases in subtropical paddy soils

• Published in: Journal of soils and sediments 2014, Vol.14 (1), p.1-9
• Main Authors: Zhou, Ping, Li, Yong, Ren, Xiu’e, Xiao, He’ai, Tong, Chengli, Ge, Tida, Brookes, Philip C, Shen, Jianlin, Wu, Jinshui
• Format: Article
• Language: English
• Subjects: Availability; carbon; Carbon dioxide; Carbon sequestration; carbon sinks; Clay; Clay loam; clay loam soils; Clay minerals; Clay soils; Climate; Climate change; Coefficients; Dissolved organic carbon; Dynamics; Earth and Environmental Science; Environment; Environmental Physics; High temperature; Incubation period; Loam; Loam soils; Mineralization; Moisture content; Organic soils; paddy soils; Sandy loam; sandy loam soils; Sandy soils; Sec 1 • Soil Organic Matter Dynamics and Nutrient Cycling • Research Article; Sensitivity; silty clay soils; Soil; soil organic carbon; Soil Science & Conservation; Soil stabilization; Soil temperature; Soils; Temperature; Temperature effects; Water content
• ISSN: 1439-0108; 1614-7480
• DOI: 10.1007/s11368-013-0781-4

PURPOSE: Understanding organic carbon mineralization and its temperature response in subtropical paddy soils is important for the regional carbon balance. There is a growing interest in factors controlling soil organic carbon (SOC) mineralization because of the potential for climate change. This study aims to test the hypothesis that soil clay content impedes SOC mineralization in subtropical paddy soils. MATERIALS AND METHODS: A 160-day laboratory incubation at temperatures from 10 to 30 °C and 90% water content was conducted to examine the dynamics of SOC mineralization and its temperature response in three subtropical paddy soils with different clay contents (sandy loam, clay loam, and silty clay soils). A three-pool SOC model (active, slow, and resistant) was used to fit SOC mineralization. RESULTS AND DISCUSSION: Total CO₂ evolved during incubation following the order of clay loam > silty clay > sandy loam. The temperature response coefficients (Q ₁₀) were 1.92 ± 0.39, 2.36 ± 0.22, and 2.10 ± 0.70, respectively, for the sandy loam soil, clay loam soil, and silty clay soil. But the soil clay content followed the order of silty clay > clay loam > sandy loam. The sandy loam soil neither released larger amounts of CO₂ nor showed higher temperature sensitivity, as expected, even though it contains lower soil clay content among the three soils. It seems that soil clay content did not have a dominant effect which results in the difference in SOC mineralization and its temperature response in the selected three paddy soils. However, dissolved organic carbon (DOC; representing substrate availability) had a great effect. The size of the active C pool ranged from 0.11 to 3.55% of initial SOC, and it increased with increasing temperature. The silty clay soil had the smallest active C pool (1.40%) and the largest Q ₁₀ value (6.33) in the active C pool as compared with the other two soils. The mineralizable SOC protected in the silty clay soil, therefore, had even greater temperature sensitivity than the other two soils that had less SOC stabilization. CONCLUSIONS: Our study suggests that SOC mineralization and its temperature response in subtropical paddy soils were probably not dominantly controlled by soil clay content, but the substrate availability (represented as DOC) and the specific stabilization mechanisms of SOC may have great effects.