日本地球惑星科学連合2023年大会

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[E] オンラインポスター発表

セッション記号 A (大気水圏科学) » A-HW 水文・陸水・地下水学・水環境

[A-HW18] 流域圏生態系における物質輸送と循環:源流から沿岸海域まで

2023年5月25日(木) 10:45 〜 12:15 オンラインポスターZoom会場 (5) (オンラインポスター)

コンビーナ:細野 高啓(熊本大学大学院先端科学研究部)、伴 修平(公立大学法人 滋賀県立大学)、齋藤 光代(広島大学 大学院先進理工系科学研究科 )、Adina Paytan(University of California Santa Cruz)


現地ポスター発表開催日時 (2023/5/26 17:15-18:45)

10:45 〜 12:15

[AHW18-P08] Spatial variation in groundwater discharge on a tidal flat in an island of western japan

*高 啓迪1小野寺 真一1齋藤 光代1友澤 裕介1、松原 怜哉2 (1.広島大学大学院先進理工系科学研究科、2.広島大学総合科学部)


キーワード:海底地下水湧出、空間分布、干潟、海島

To manage and conserve the seagrass bed and ecosystem in tidal flats, this study examined to confirm spatial distribution in groundwater (SGD) on tidal flats with the area of around 100 m square in a small and steep island. Various groundwater and nutrient discharges were observed at the W and E sites. 1) Based on the water budget, the groundwater flux was estimated to be 8.68 m/yr or 23.9 mm/day in E, and 17.75 m/yr or 48.6 mm/day in W, respectively. 2) Spatial distributions of groundwater contribution ratio (%) in pore water at W was around 60% in average, which was 8 times of that in E site. 3) The NO3-N concentration in pore water at W site was about 30 times of that at E because of the low attenuation rate with high groundwater velocity. 4) The temporal variation in groundwater flux with tidal fluctuation indicated 2.5 m/day in maximum and -4.0 m/day in minimum. This huge difference between the average flux and maximum indicated also large seawater recirculation and heterogeneous distribution of SGD. This heterogeneous distribution at this tidal flat would contribute to the activity of seagrass and diversity of ecosystem.

Acknowledgment
This research was supported by JSPS Grant-in-Aid for Scientific Research (B) (No. 21H03650, PI: Mitsuyo Saito) and Fostering Joint International Research (A) (No. 20KK0262, PI: Mitsuyo Saito).