Spatio-temporal patterns of soil erosion and suspended sediment dynamics in the Mekong River Basin

被引:31
|
作者
Suif, Zuliziana [1 ,2 ]
Fleifle, Amr [1 ,3 ]
Yoshimura, Chihiro [1 ]
Saavedra, Oliver [1 ,4 ]
机构
[1] Tokyo Inst Technol, Dept Civil Engn, Meguro Ku, Tokyo 1528552, Japan
[2] Natl Def Univ Malaysia, Fac Engn, Dept Civil Engn, Kuala Lumpur 57000, Malaysia
[3] Univ Alexandria, Dept Irrigat Engn & Hydraul, Alexandria, Egypt
[4] Egypt Japan Univ Sci & Technol, Energy Resources & Environm Engn Program, Alexandria, Egypt
基金
日本学术振兴会;
关键词
Integrated framework; RUSLE; Sediment erosion; Suspended sediment load; Suspended sediment concentration; Mekong River Basin; LANDSAT TM; WATER; MODEL; RESERVOIR; DELIVERY; IMPACTS; MONSOON; LOAD;
D O I
10.1016/j.scitotenv.2015.12.134
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Understanding of the distribution patterns of sediment erosion, concentration and transport in river basins is critically important as sediment plays a major role in river basin hydrophysical and ecological processes. In this study, we proposed an integrated framework for the assessment of sediment dynamics, including soil erosion (SE), suspended sediment load (SSL) and suspended sediment concentration (SSC), and applied this framework to the Mekong River Basin. The Revised Universal Soil Loss Equation (RUSLE) model was adopted with a geographic information system to assess SE and was coupled with a sediment accumulation and a routing scheme to simulate SSL. This framework also analyzed Landsat imagery captured between 1987 and 2000 together with ground observations to interpolate spatio-temporal patterns of SSC. The simulated SSL results from 1987 to 2000 showed the relative root mean square error of 41% and coefficient of determination (R-2) of 0.89. The polynomial relationship of the near infrared exoatmospheric reflectance and the band 4 wavelength (760-900 nm) to the observed SSC at 9 sites demonstrated the good agreement (overall relative RMSE = 5.2%, R-2 = 0.87). The result found that the severe SE occurs in the upper (China and Lao PDR) and lower (western part of Vietnam) regions. The SSC in the rainy season (June-November) showed increasing and decreasing trends longitudinally in the upper (China and Lao PDR) and lower regions (Cambodia), respectively, while the longitudinal profile of SSL showed a fluctuating trend along the river in the early rainy season. Overall, the results described the unique spatio-temporal patterns of SE, SSL and SSC in the Mekong River Basin. Thus, the proposed integrated framework is useful for elucidating complex process of sediment generation and transport in the land and river systems of large river basins. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:933 / 945
页数:13
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