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-HW 水文・陸水・地下水学・水環境

[A-HW20] 流域の物質輸送と栄養塩循環-人間活動および気候変動の影響-

2018年5月21日(月) 09:00 〜 10:30 コンベンションホールB(CH-B) (幕張メッセ国際会議場 2F)

コンビーナ:齋藤 光代(岡山大学大学院環境生命科学研究科)、小野寺 真一(広島大学大学院総合科学研究科)、細野 高啓(熊本大学大学院先導機構、共同)、Adina Paytan(University of California Santa Cruz)、座長:細野 高啓(熊本大学先導機構)

10:15 〜 10:30

[AHW20-17] 河川系における地質由来ヒ素の水田灌漑用水を経由する土壌水から水稲への輸送と蓄積

*中屋 眞司1遅 海1室田 健吾1益田 晴恵2 (1.信州大学工学部水環境・土木工学科、2.大阪市立大学大学院生物地球系専攻/地球学科 )

キーワード:ヒ素、水稲、河川系

Geogenic arsenic (As) exceeding WHO standard is often detected in rivers and in river soils along volcanic front of Japanese Island. In recent years, arsenic (As) has been detected in Japanese paddy rice grains at concentrations often exceeding the upper limit (0.2 ppm) stipulated by the Codex Alimentarius Commission (Ministry of Agriculture, Forestry and Fisheries, 2014; Matsumoto et al., 2015). Japanese paddy rice is cultivated under flooding using paddy water from rivers. Paddy rice seems to be one of the sink of As in river system. In this study, we focus on the behavior of geogenic, toxic trace elements, As from soil water to paddy rice via irrigation water in Japanese paddy rice fields in the study area along volcanic front. One irrigation water originates from a small river sprang in an active volcano, Mt. Asama, and the other originates from a small river sprang in a currently inactive volcano, Yatsugatake Mountains in Nagano, Japan. In these small rivers, the majority of As is transported in the dissolved form, predominantly as arsenate, with low abundance of particulate matter. The concentration range of As in irrigation water of paddy field is almost same to that in small rivers. However, the concentration range of As in root of paddy rice is a thousand – a hundred thousand times as high as that of irrigation water. The As in root of paddy rice increases with Fe, while the As in water does not increase with Fe. The relationship between As and Fe concentrations at roots of paddy rice is different from those relationships of river water, of irrigation water and of extraction waters from paddy soil under both reducing and oxide conditions. In general, As and Fe are taken up and transported via each ion channel and each transporter, separately, at roots in paddy rice (e.g., Ma et al., 2006; Ma et al., 2007). Our findings suggest that As in paddy rice is not directly derived from As in the irrigation water from the river under flooding.