Japan Geoscience Union Meeting 2025

Presentation information

[J] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-CG Complex & General

[A-CG53] Coastal Ecosystems - 1. Water Cycle and Land-Ocean Interactions

Wed. May 28, 2025 9:00 AM - 10:30 AM Exhibition Hall Special Setting (3) (Exhibition Hall 7&8, Makuhari Messe)

convener:Ryo Sugimoto(Faculty of Marine Biosciences, Fukui Prefectural University), Masahiko Fujii(Atmosphere and Ocean Research Institute, The University of Tokyo), Tomohiro Komorita(Faculty of Environmental and Symbiotic Sciences, Prefectural University of Kumamoto), Makoto Yamada(Faculty of Economics, Ryukoku University), Chairperson:Masahiko Fujii(Atmosphere and Ocean Research Institute, The University of Tokyo), Tomohiro Komorita(Faculty of Environmental and Symbiotic Sciences, Prefectural University of Kumamoto)

9:30 AM - 9:45 AM

[ACG53-03] Significance of submarine groundwater discharge in Ise Bay using radium isotopes

*Ryo Sugimoto1, Yuitsu Tochio1, Toshimi Nakajima2, Makoto Okada3, Tomohiko Kobayashi3, ATSUYOSHI MANDA4 (1.Faculty of Marine Biosciences, Fukui Prefectural University, 2.Atmosphere and Ocean Research Institute, The University of Tokyo, 3.Mie Prefecture Fisheries Research Institute, 4.Mie University)

Keywords:Submarine groundwater discharge, Radium, Nutrient

Recent studies revealed that the nutrient supply from groundwater inflow to coastal waters is comparable to that from surface river water worldwide. Here, we conducted field surveys to assess the submarine groundwater discharge of fresh groundwater and recirculated groundwater into Ise Bay using radium isotopes (223Ra; τ1/2=11.4 days, 224Ra; τ1/2=3.66 days, 226Ra; τ1/2=1600y, and 228Ra; τ1/2=5.75y). The results showed that the freshwater groundwater inflow was on average about 0.4 times higher than the river water inflow and the recirculating groundwater inflow was 1.3 times higher than the river water inflow. In the presentation, we will show the results of nutrient fluxes associated with groundwater inflow.