Timber harvesting causes substantial changes in forest soil microenvironmental conditions, yet the long-term effects on soil greenhouse gas (GHG) fluxes remain poorly understood, particularly in Korean mixed forests. This study investigated the effects of timber harvesting on soil temperature, moisture, CO2 efflux, and CH4 uptake over a three-year monitoring period at the Kangwon National University Experimental Forest. A total of 19 harvested plots and 14 non-harvested control plots were established on the same slope. Soil GHG fluxes were measured monthly using a static closed chamber method, and linear mixed-effects models (LMMs) were applied to evaluate treatment effects over time. Harvesting significantly elevated soil temperature and moisture at the harvested site relative to the reference site throughout the monitoring period, though the effect on soil temperature was inconsistent, whereas elevated moisture persisted across all three years. Normalized soil CO2 efflux was consistently higher at the harvested site than at the reference site, with annual relative differences of approximately 60%, 49%, and 35% in 2023, 2024, and 2025, respectively. Conversely, soil CH4 uptake was suppressed at the harvested site compared with the reference site, with relative suppression declining from 17% in 2023 to 9% in 2025. Soil CO2 efflux was primarily regulated by soil temperature, whereas CH4 uptake showed stronger dependence on soil moisture. The diminishing magnitude of treatment differences over time implies an ongoing recovery of soil microenvironmental conditions at the harvested site. These findings demonstrate that timber harvesting reorganizes soil temperature and moisture regimes in ways that generate divergent and persistent responses in CO2 efflux and CH4 uptake, underscoring the importance of long-term monitoring for evaluating post-harvest soil carbon dynamics.
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Abstract Introduction Materials and Methods Site description Field measurements Soil CO2 flux normalization Data analysis Results Seasonal variation in soil temperature and moisture following timber harvesting Seasonal variation in soil greenhouse gas flux following timber harvesting Relationships between environmental variables and soil greenhouse gas fluxes Discussion Conclusion Acknowledgements References