日本地球惑星科学連合2015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-HW27] 流域の水及び物質の輸送と循環-源流域から沿岸域まで-

2015年5月24日(日) 18:15 〜 19:30 コンベンションホール (2F)

コンビーナ:*中屋 眞司(信州大学工学部土木工学科)、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)、知北 和久(北海道大学大学院理学研究院自然史科学部門)、入野 智久(北海道大学 大学院地球環境科学研究院)、小林 政広(独立行政法人森林総合研究所)、吉川 省子(農業環境技術研究所)、奥田 昇(総合地球環境学研究所)

18:15 〜 19:30

[AHW27-P05] 都市及び近郊からなる大和川流域における地下水涵養の空間分布

*小野寺 真一1清水 裕太2齋藤 光代3大西 晃暉4丸山 豊1金 广哲1 (1.広島大学総合科学研究科、2.学振PD, 農研機構近中農研センター、3.岡山大学、4.復建調査設計)

In coastal megacities, sever groundwater depression and land subsidence occurred. For sustainable groundwater use and risk management of flood, it is necessary to estimate not only groundwater recharge in upstream area of a megacity but flood discharge in subsidence area. In addition, spatial distributions of them would be especially expected in various annual precipitations. However, such estimations and predictions in future have not been fully done in previous studies. Therefore, we aimed to evaluate spatial distribution in groundwater recharge and flood discharge in an urban and suburban watershed of 1000km2 scale including Osaka metropolitan city. We applied SWAT model to predictions of floods and groundwater recharge from 1990 to 2013 in Yamato river watershed. It was calibrated by the daily river runoff data from 2003 to 2004 in Japanese Ministry of Land, Infrastructure and Transport and it was validated the data from 2008 to 2009. The daily variation in river runoff in 2012 indicated the typical increase at the rainfall event with the amount above 100mm, especially it was one of the largest flood on the end of June in 2012. According to these results, the increase of the flood risk on the Osaka megacity was suggested. Based on the river runoff simulation, the spatial distributions in groundwater recharge were also evaluated. The urban area indicated the low recharge rate but forest area had the high rate. For the sustainable groundwater use and decline of flood risk, it was suggested that we should keep the present percentage of forest cover.