The impact of climate-soil-vegetation-human interaction on SOC change over 30 years across the National Ecological Observatory Network, USA

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Jie Hu, Jingyi Huang and Alfred E. Hartemink, Department of Soil Science, University of Wisconsin-Madison, Ankur R. Desai, Atmospheric and Oceanic Sciences, University of Wisconsin-Madison

Background/Question/Methods
Pedosphere is the largest terrestrial carbon sink and has the potential to mitigate climate change. Large uncertainties still exist about where, and which soil is promising to achieve carbon sequestration as soil is inherently complex under soil forming factors including climate, organisms, relief, parent material, and time. In this study, a spatial-temporal framework was used to study the change in soil organic carbon (SOC) across National Ecological Observatory Network (NEON), USA over 30 years. We hypothesize that: 1) on the continental scale, the hot-spots and cold-spots of SOC change vary with soil orders across different eco-climatic domains, controlled by all soil forming factors that affect carbon input and output; 2) within the same eco-climatic regime, the effects of disturbance on SOC change are controlled by physical and biogeochemical processes, represented by varying soil properties including clay, bulk density, pH, and CEC. To separate the effects of disturbance under different land-use scenarios on SOC change, space-for-time substitution was used in combination with the Continuous Change Detection and Classification algorithm and structural equation models (SEM).
Results/Conclusions
Results suggested that 1) under natural vegetation, Ultisols, Spodosols, and Inceptisols showed a large SOC accumulation especially in the eastern coast, while Inceptisols, Andisols, and Aridisols in the western US showed a large SOC loss; 2) compared with the same reference soils under natural vegetation, Mollisols and Alfisols showed a large SOC decrease due to human disturbance (e.g., farming and grazing); 3) Inceptisols (+6.2 g/kg) and Gelisols (+27.5 g/kg) in Alaska presented the largest SOC increase among all the soil orders within the subsoil (B horizon); 4) water (soil moisture and precipitation) and CEC were the most dominant factors that affected SOC content across the NEON sites. This empirical analysis of the 30-years SOC change across eco-climatic regimes could be used for ecosystem modelers to benchmark the models across biomes and study the physical and biogeochemical controls on SOC change under different land management scenarios.