A combination of chemical and carbon stable isotopic compositions has been used to examine controlling processes of groundwater chemistry along the flow paths in the Ohmama Alluvial Fan (OAF) in Gunma Prefecture. The groundwater modifies its chemical compositions from Ca-HCO
3 type to Ca-(SO
4+NO
3) type along the paths; from upper part to lower part of the OAF. In addition, increases of NO
3- and SO
42- concentrations, a decrease of dissolved inorganic carbon (DIC) concentrations, and a rise of δ
13C
DIC values in the groundwater are observed. These observations can be attributed to three processes; one was oxidation process of ammonium sulfate fertilizer in vegetable fields distributing widely in the OAF and the others were processes of CO
2 degas and mineral dissolution associated with the oxidation process. Furthermore, it is noted that EC values in the groundwater drastically decrease at the lowest part of the OAF where paddy fields distribute. The most plausible cause of this EC decrease is infiltration of paddy water. Model calculations based on Cl
- concentrations indicate that paddy water occupied high ratio, such as approximately 80%, in groundwater at the lower part of the OAF.
View full abstract