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) 09:00 〜 10:45 301B (3F)

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)、座長:入野 智久(北海道大学 大学院地球環境科学研究院)

09:30 〜 09:45

[AHW27-03] Soil Loss and sediment yield assessment from 1974-2012 in the some west-coast river catchments, Penang Island Malaysia

*NAJIB, Sumayyah aimi MOHD1RAHAMAN, Zullyadini A.1 (1.Universiti Sains Malaysia)

キーワード:Soil Erosion, Soil loss and sediment yield assessment, USLE, GIS, Penang Island, Malaysia

Soil erosion is a worldwide problem because of its economic and environmental impacts. Many human-induced activities, such as mining, construction, and agricultural activities disturb land surface , resulting in accelerated erosion. There are many land clearing activities in catchment areas that could add an enormous amount of sediment to rivers. Nowadays, land has become one of limited resources in Penang due to the topography of the hilly and flat area. Penang Island is a city of rapid industrialization and density, and in order to face future challenges caused by rapid economic development, there is a high demand for flat land requirements. Land clearing activities contributes to the total concentration of sediment, affecting the health of the catchment area. To estimate soil loss, soil erosion model such as Universal Soil Loss Equation (USLE) is used to estimated average soil loss generated from splash, sheet and rill erosion. Use of the USLE has recently been extended for predicting soil losses and plan control practices in the agricultural catchment by effective integration of Geographic Information Systems (GIS) based on procedures to estimate the factor values in a grid cell basis. This study was performed to predict soil loss by USLE/GIS and the factor to calculate soil loss is Rainfall erosivity (R), Soil erodibility factor (K), Topographic factor (LS), Land cover management factor (C) and Conservation practices factor (P). Result shows that soil loss was 100.7 t/ha/year and sediment yield was 2336 t/km2/year in 2012, 84 t/ha/year and 1907 tan/km2/year in 2004; 144 t/ha/year and 1889 tan/km2/year in 1984 and 1974 the soil loss was 61 t/ha/year and the sediment yield was 1272 tan/km2/year.