[SVC48-P10] Geochemical study of the Uchinomaki hot spring within Aso caldera: time series change before and after the Kumamoto Earthquake
Keywords:Aso caldera floor, Hot spring reservoir, Horizontal slide
More than 30 water samples were collected from the Uchinomaki hot spring and adjacent areas. After measurement of temperature, pH, electic conductivity and oxidation-reduction potential, the water sample was filtered with a 0.45 um disk filter and stored. Chemical analysis was conducted by ICP-OES for cations (Na+, K+, Ca2+, Mg2+, Fe2+), ion chromatography for anions (Cl-, SO42-), and alkalinity tiration for carbonate (HCO3-). Isotopic composition of hydrogen and oxygen was determined by Wavelength-Scanned Cavity Ring-down Spectroscopy.
Time series change before and after the earthquake in hot spring water chemistry from the Uchinomaki area was not recognized. Their chemical composition was characterized by SO4-rich signature, which is commonly observed in groundwater within Aso caldera. Groundwater collected from the area on the southside of the Uchinomaki area is known as “Akamizu” from its high Fe concentration associated with high SO4 concentration. In this study, the Uchinomaki hot spring waters showed Na+K-rich signature, whereas Akamizu groundwaters showed Ca-rich signature. The difference in cation composition would be attributed to that Uchinomaki hot spring and Akamizu groundwater have distinctive reservoirs.
The most vigorous emanation from a rice paddy was observed at the southwest side of the Uchinomaki hot spring area, which is in accordance with that the geophysical study demonstrates westward movement of the horizontal sliding. The emanated warm fluid showed Fe-rich and Ca-rich signature that is similar to chemical composition of the Akamizu groundwater. The horizontal landslide is likely not to have affected the fluid reservoirs but caused significant change of surface groundwater pathways in wide area around the Uchinomaki hot spring.