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)

09:30 〜 09:45

[AHW20-14] Estimation of flow path in headwater area, using hourly resolution SWAT Model analysis

*Yang Cao1Shin-ichi Onodera1Tomoki Ohira1Yusuke Tomozawa1Fandy Tri Admajaya1 (1.Graduate School of Integrate Arts and Sciences, Hiroshima University)

キーワード:SWAT, headwater, hourly simulation, runoff, rock

This study aimed to compare the water budgets of two headwater areas with different geological conditions using the SWAT model. The simulation results show that NS has been obtained 0.54 and 0.75 respectively during the calibration and validation period in Akamatsu area, and Shimo-akamatsu area result in NS 0.70 and 0.54 respectively in those two periods. Based on the results of the water budget in these two areas, we found that the average annual contribution of deep aquifer recharge as a relative percentage to precipitation in Akamatsu where the granites are widely distributed is less than that in Shimo-akamatsu where rhyolites are widely distributed. And the variation of lateral flow and groundwater in both study areas are also consistent with their geology. It shows that the SWAT hourly simulation is reliable in estimating the water budget for different geological conditions and can be effectively used as a water management policy for the both geologic conditions.