日本地球惑星科学連合2019年大会

講演情報

[E] ポスター発表

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-HW22] 流域の物質輸送と栄養塩循環-源流域から沿岸海域まで-

2019年5月30日(木) 17:15 〜 18:30 ポスター会場 (幕張メッセ国際展示場 8ホール)

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)、吉川 省子(農業・食品産業技術総合研究機構 農業環境変動研究センター)、安元 純(琉球大学 農学部 地域農業工学科)、Adina Paytan(University of California Santa Cruz)

[AHW22-P09] Estimation of groundwater recharge and phosphorus transport under different precipitation conditions in a suburban catchment, using SWAT model

*王 崑陽1,2小野寺 真一1齋藤 光代3奥田 昇4大久保 卓也5 (1.広島大学、2.首都師範大学、3.岡山大学、4.総合地球環境学研究所、5.滋賀県立大学)

キーワード:リン輸送、地下水涵養、異なる降水条件、SWATモデル

The quantification of the groundwater recharge and phosphorus transport in water is one of the most important indicators of the water cycle in lakes because these processes are related to the transport of large nutrient loads. The Yasu River is one of the important water sources of the Biwa Lake. In this paper, Geographic Information System technology is used to analyze and predict the land use change in the Yasu River Basin. The water balance was simulated using the Soil and Water Assessment Tool. Simulations of different years in different precipitation seasons were carried out. The correlation coefficient and the Nash Sutcliffe coefficient are higher than the reference values. The sensitivity analysis of the parameters reveals the different degrees of sensitivity of the parameters in different water seasons, CN2 always has a high sensitivity during all kinds of water season. The total groundwater recharge and discharge are 180 million m3 and 179 million m3 in the normal precipitation season, respectively. The trends differ in the dry and wet seasons. In the dry season of 2007, the groundwater recharge was below 140 million m3, while it exceeded 240 million m3 in the rainy season in 2003. In addition, the process of phosphorus loss in the basin and release into Lake Biwa are explained from the perspective of space and time. This is closely related to the spatial distribution of the main channel and the time distribution of precipitation. The total amount of nonpoint source pollution of phosphorus in three years is equivalent to 4.08 kg/ha of paddy fields in the watershed. The spatial distribution of phosphorus loss is related to the stream flow, it is mainly concentrated in the area with paddy fields and urban. The time distribution is related to the distribution of the precipitation. With increasing precipitation, the nonpoint source pollution of phosphorus slightly increases. This is due to the driving effect of precipitation on the phosphorus transfer and erosion of soil.