Warming-dominated climate change impacts on soil organic carbon fractions and aggregate stability in Mollisols

• Published in: Geoderma Vol. 438; p. 116618
• Main Authors: Zhou, Meng, Xiao, Yang, Zhang, Xingyi, Sui, Yueyu, Xiao, Leilei, Lin, Jinkuo, Cruse, Richard M., Ding, Guangwei, Liu, Xiaobing
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.10.2023; Elsevier
• Subjects: aggregate stability; agricultural land; Carbohydrate; carbohydrates; climate change; dissolved organic carbon; ecosystems; fractal dimensions; FTIR; latitude; Lignin; microaggregates; microbial carbon; Mollisols; Particulate organic matter; silt; Silt and clay fractions; soil organic carbon; Solid-state13C NMR; Lignin; Silt and clay fractions; Carbohydrate; Particulate organic matter; FTIR; Solid-state13C NMR
• ISSN: 0016-7061; 1872-6259
• DOI: 10.1016/j.geoderma.2023.116618

[Display omitted] •Higher initial SOM bulk Mollisols are more sensitive to long-term climate warming.•Recalcitrant carbon fraction in macroaggregates is sensitive to climate warming.•Increased carbohydrate and decreased lignin reduce aggregate stability under warming.•Warming affects soil organic carbon stabilization by physical protection of particulate organic matter.•Warming affects soil organic carbon stabilization by chemical protection of mineral association. Mollisols contain high amounts of soil organic carbon (SOC), which is highly susceptible to climate change; thus, climate change could indirectly influence soil aggregate stability, but the dominant factor affecting aggregate stability remains controversial. Here, a soil transplanting test from high-latitude to low-latitude locations was initiated in 2004 to investigate the influences of warming-dominated climate change (approximately 3–4.7 ℃) on the quantity and molecular composition of OC fractions in surface (0–20 cm) soils, aggregate stability changes and underlying mechanisms. Different initial soil organic matter (SOM) contents of 50.6 g kg−1 (SOM5), 58.8 g kg−1 (SOM6), and 108.9 g kg−1 (SOM11) were established in situ soils and in transplanted soils to simulate warming. The 15-year warming-dominated climate change presented no noticeable change in the SOC content in the lower SOM Mollisols (SOM5 and SOM6) but increased the SOC content by 13.3% in the higher SOM Mollisol (SOM11). In terms of labile OC fractions, warming-dominated climate change significantly increased the dissolved organic carbon (DOC) content by 20.1%–47.7% but reduced the easily oxidizable organic carbon (EOC) and microbial biomass carbon (MBC) contents by 22.1%–33.6%. Irrespective of any treatment, warming-dominated climate change decreased soil aggregate stability, as evidenced by the reduction in mean weight diameter (MWD) and geometric mean diameter (GMD) of 41.7%–79.3% and an increase in fractal dimension (D) of 28.6%–58.5%. For hierarchically organized soil aggregates, warming-dominated climate change increased the proportion and OC content of particulate organic matter inside free microaggregates (Fm-POM) as well as nonaggregated silt + clay-sized organic matter (nA-MOM). However, climate change decreased the proportion and OC content of silt + clay-sized fractions inside microaggregates within macroaggregates (mM-MOM). Of importance, warming-dominated climate change increased the amount of carbohydrates and decreased the amount of lignin in the mM-MOM, Fm-POM, and nA-MOM fractions. Therefore, we speculated that chemical protection by mineral association within macroaggregates and nA-MOM fractions and physical protection by the occlusion of POM within free microaggregates might be the primary mechanisms for SOC stabilization under long-term climate change in Mollisols. The long-term warming-dominated climate change results demonstrated a positive effect on SOC content in higher SOM Mollisols, DOC, carbohydrate C, free microaggregate-associated C and nonaggregated silt + clay-sized associated C but exhibited a negative effect on EOC, MBC, lignin C, silt + clay-sized inside microaggregates within macroaggregates C and aggregate stability. These variables all contributed to the reduction in soil aggregate stability and might act as sensitive indicators of warming-dominated climate change in Mollisols, which in turn affect farmland ecosystem C fluxes in response to further climate change.