Japan Geoscience Union Meeting 2018

Presentation information

[EE] Evening Poster

A (Atmospheric and Hydrospheric Sciences) » A-HW Hydrology & Water Environment

[A-HW22] Hydrological Cycle and Water Environment

Thu. May 24, 2018 5:15 PM - 6:30 PM Poster Hall (International Exhibition Hall7, Makuhari Messe)

convener:Seiya Nagao(Institute of Nature and Environmental Technology, Kanazawa University), Isao Machida(Geological Survey of Japan), Shin'ichi Iida(国立研究開発法人森林研究・整備機構森林総合研究所森林研究部門森林防災研究領域水保全研究室, 共同), Takeshi Hayashi(Faculty of Education and Human Studies, Akita University)

[AHW22-P07] Research of submarine groundwater discharge using 222Rn in Nanao West Bay

*Atsushi Fujita1, Seiya Nagao2, Shinya Ochiai2, Ryo Sugimoto3, Matthew Charette4, Paul Henderson4 (1.Graduate School of Natural Science and Technology, Kanazawa University, 2.Institute of Nature and Environmental Technology, Kanazawa University, 3.Reseach Center for Marine Bioresources, Fukui Prefectural University, 4.Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institute)

Keywords:SGD, radon-222, groundwater, Nanao West bay

Biological production is more active in coast areas than in open sea because large amount of nutrients from terrestrial areas are carried by rivers. On the other hand, contribution of nutrients from groundwater to coast areas is also important, but identification of submarine groundwater discharge (SGD) is tedious work. Many scientists have been using 222Rn to specify the contribution of groundwater. 222Rn is a daughter nuclide of 226Ra, water-soluble and noble gas. The sedimentary layer is rich in 238U and 226Ra which belong among Uranium series, so the concentration of 222Rn is higher in groundwater than surface water. 222Rn is lost in surface water because of diffusion to atmosphere. Moreover 222Rn has a half-life of 3.83 days and is used to specify the contribution of groundwater with short residence time. In this study, research was carried out at Nanao West Bay, which is located at the Noto Peninsula and is the semi-closed feature, to identify the presence of SGD by measuring 222Rn concentration. Surface and bottom sea waters were collected at 11 sites in May and November 2017. Water quality such as salinity, water temperature, dissolved oxygen was determined by Conductivity Temperature Depth profiler. The six liter of sea water samples was measured for 222Rn concentration by electronic Rn detector (RAD 7: Durridge) after the sample collection. Figure 1 shows 222Rn concentration in the bottom sea water in November 2017. The concentration of 222Rn ranged from 30.4 to 78.2 Bq/m3 and was higher in the center-east area of Nanao West Bay. Figure 2 shows 222Rn concentration as a function of salinity. The solid line indicates the mixing between river water and seawater outside the bay and dashed line indicates the mixing between groundwater and seawater outside the bay. The higher 222Rn concentration collected at three sites is plotted at the closed area of dashed line. The results suggest that SGD is observed at the center-east area of Nanao West Bay.