JavaScript requeired.
Geochemical Journal
Geochemical Journal An open access journal for geochemistry
Published for geochemistry community from Geochemical Society of Japan.

An easier approach for helium isotope flux estimation in a submerged caldera

Ma Teresa Nakajima, Naoto Takahata, Hajime Obata, Takanori Kagoshima, Yuji Sano
Geochemical Journal, Early Release (Accepted: 2024/01/03)


Wakamiko Caldera is an isolated basin located in the northern part of Kagoshima Bay. The underwater caldera is known for the active fumaroles that continuously discharge volcanic substances into the overlying water. Due to the limited exchange of waters in the caldera with the surrounding area, the water column gets stagnant and stratified from spring to autumn. Previous studies have shown that overturning occurs in the winter. Based on new data obtained by field observation in Wakamiko Caldera, we show that during winter, vertical mixing “resets” the helium isotope profile. After winter, as the water column regains its stratification, fluids with mantle helium slowly build up near the seafloor, resulting in the high 3He/4He ratio previously observed. We now use the temporal variation of 3He/4He ratio in different seasons to calculate the flux of 3He. Using this method, we estimate the 3He flux at approximately 0.013 mol/year.


Keywords: submerged caldera, volatiles, gas flux, helium isotopes, carbon dioxide

All Issues

Current Issue:
Impact Factor: 0.8 (2022)
Submission to final decision: 9.6 weeks (2022)
Geochemical Society of Japan

page top