Fig. 5From: Hydrological and biogeochemical controls on temporal variations of dissolved carbon and solutes in a karst river, South Chinaa mean monthly contributions from all end-members; b rates of physical and chemical weathering; c variations in temperature and discharge; d the CO2 consumption fluxes of silicates and carbonates; e linear relationships between CO2 consumption fluxes of silicates and carbonates versus discharge in the Guijiang River during the hydrological yearBack to article page