Fig. 7From: Hydrological and biogeochemical controls on temporal variations of dissolved carbon and solutes in a karst river, South Chinaa Relationships between [HCO3−]/[Ca2+ + Mg2+] (in molar ratios) and δ13CDIC values; b DOC and DIC contents with variations in δ13CDIC values; c DIC contents and δ13CDIC values with variations in discharge; d mean monthly contributions of riverine DIC sources under different climatic conditions in the Guijiang River during the hydrological yearBack to article page