日本地球惑星科学連合2018年大会

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セッション記号 A (大気水圏科学) » A-CG 大気水圏科学複合領域・一般

[A-CG42] 沿岸海洋生態系─1.水循環と陸海相互作用

2018年5月24日(木) 09:00 〜 10:30 201B (幕張メッセ国際会議場 2F)

コンビーナ:杉本 亮(福井県立大学海洋生物資源学部)、小路 淳(広島大学大学院生物圏科学研究科)、山田 誠(龍谷大学経済学部、共同)、藤井 賢彦(北海道大学大学院地球環境科学研究院)、座長:小路 淳藤井 賢彦

09:30 〜 09:45

[ACG42-02] 硝酸の三酸素同位体組成を用いた森林由来硝酸の河川から海域への輸送量評価

*平井 タケル1杉本 亮1 (1.福井県立大学)

キーワード:硝酸沈着、硝酸フラックス、三酸素同位体、陸域ー海域相互作用

Terrestrial nitrate from river water and groundwater to coastal seas is an important nutrient source for coastal ecosystems. Recent accelerated depositions of atmospheric nitrate transported from the East Asia may stimulate leaching of nitrate from the forest and thus alter nutrient dynamics of coastal ecosystems. In this study, we have evaluated quantitative effect of forest-derived nitrate on total nitrate flux from the Kita River into Obama Bay using the nitrate triple oxygen isotope. Total flux of nitrate from the Kita River changed seasonally : lower in summer (from May to August) and higher in winter (from November to February). We divided this nitrate flux into two sources of forest-derived nitrate and others by means of two-source mixing of O nitrate. As a result, forest-derived nitrate occupied 21-93% of total nitrate flux in summer and 49-84% in winter. Furthermore, regardless of the season, 81-96% of forest-derived nitrate was accounted for nitrate generated by nitrification in the forest. These results mean that nitrogen saturation status of the forest ecosystem in the Kita River watershed dominate the riverine flux and may alter nutrient levels of Obama Bay.