Spatiotemporal patterns and environmental controls of dissolved carbon and water-air CO₂ fluxes in Southwest China's alpine canyon rivers.
Wu Zihan Z, Wang Hongwei H, Li Yong Y, Yang Xiaobo X
Mountain rivers remain insufficiently understood within regional and global carbon cycles, particularly high-slope systems that are highly sensitive to anthropogenic disturbance and climate change. We investigated a high-slope alpine gorge river in southwestern China (Upper Min River) through five seasonal surveys in 2023, quantifying dissolved inorganic carbon (DIC), dissolved organic carbon (DOC), and water-air CO2 flux (FCO₂) and assessing their controls. DIC (8.28-58.97 mg/L; mean 32.61 mg/L) decreased from carbonate headwaters to downstream non-carbonate reaches, indicating strong carbonate-weathering control and providing the main inorganic substrate sustaining CO2 supersaturation. DOC (0.01-8.21 mg/L; mean 1.53 mg/L) was enriched near urban and agricultural sections, and its wet-season association with ammonia nitrogen suggests that storm runoff mobilizes anthropogenic organic matter. Yet DOC showed little relationship with FCO2, implying that rapid downstream export in steep channels limits in-stream DOC mineralization. FCO2 ranged from -1.90 to 227.78 mmol/(m²·d) (mean 24.05 mmol/(m²·d)) and was positive in >95 % of measurements, evidencing persistent CO2 evasion driven by inorganic carbon supply, turbulence, and reduced atmospheric pressure at high elevation. Carbonate-underlain turbulent reaches acted as outgassing hotspots, whereas retentive reaches exhibited reduced efflux or short-lived CO2 uptake during periods of high primary productivity. Overall, carbonate weathering, anthropogenic DOC inputs, and hydrodynamic conditions jointly regulate dissolved carbon and CO2 outgassing in alpine gorge rivers, underscoring their role in regional carbon budget assessments.