日本地球惑星科学連合2022年大会

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[E] 口頭発表

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-HW24] 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

2022年5月24日(火) 13:45 〜 15:15 303 (幕張メッセ国際会議場)

コンビーナ:安元 純(琉球大学 農学部)、コンビーナ:小林 政広(国立研究開発法人森林研究・整備機構 森林総合研究所)、奥田 昇(神戸大学)、コンビーナ:Paytan Adina(University of California Santa Cruz)、座長:小林 政広(国立研究開発法人森林研究・整備機構 森林総合研究所)

14:30 〜 14:45

[AHW24-16] Variation Of Water Balance Components in the Kurose River Basin Between The 1980s and 2000s Using SWAT

*Sharon Bih Kimbi1Kunyang Wang1Shin-ichi Onodera2、Ichirow Kaihotsu1Yuta Shimizu3Yusuke Tomozawa2 (1.Graduate School of Integrated Arts and Sciences, Hiroshima University、2.Graduate School of Advanced Science and Engineering, Hiroshima University、3.Western Region agricultural Research Center, National agriculture and Food Research Organization)

キーワード:Groundwater, Kurose River basin, Landuse change, Water Balance, SWAT

Hydrologic models have been used to evaluate water availability and determine long-term sustainable water resources management policies through a comprehensive assessment of all water cycle components. The Kurose River Basin with a total area of 39.95km2 has undergone the cumulative effects of increased population and land-use change which has pressured the availability of groundwater resources in it its watershed. The study was aimed to analyse the impact of land-use change on groundwater using the SWAT model. This is a physically-based semi-distributed hydrological model with various applications to simulate water balance and watershed management. Daily discharge records for 1980-1993 and 2000-2007 with land use data for 1987 and 2009 were used in this research to compare the water balance between the 1980s and 2000s, emphasising groundwater recharge. The results showed that the calibration and validation exhibited satisfactory criteria for hydrologic simulations with both NSE and R2 coefficients greater than 0.55. Simulation results showed that land-use changes have resulted in a corresponding increase in surface runoff and a decrease in groundwater recharge from the 1980s to the 2000s. Also, paddy areas were observed to be high groundwater recharge zones but due to urbanization processes, these areas have been encroached thus leading to a decrease in groundwater recharge in the recent historic years.