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Runoff response to land use change in Baimahe basin of China based on SWAT model.

WANG Xue1,2,5, ZHANG Zu-lu2,3**, NING Ji-cai4   

  1. (1Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 2 School of Population, Resources and Environment, Shandong Normal University, Jinan 250014, China; 3 Shandong Key Laboratory of Soil and Water Conservation and Environmental Protection/Linyi University; Linyi 276005, Shandang China; 4 Yantai Institute of Coastal zone Reseavchi Chinese Academy of Sciences, Yantai  264003, Shandong China; 5Lniversity of Chinese Academy of Sciences, Beijing 100049, China)
  • Online:2013-01-10 Published:2013-01-10

Abstract: By using 3S technology, and based on the analysis and prediction of the land use change in Baimahe basin, a SWAT model was established to study the runoff response of the basin under the scenarios of different land use. In the meantime, the contribution coefficients of the main land use types in the basin to the runoff depth were calculated. From 1987 to 2017, the main land use types in the basin were farmland, construction land, forestland, and shrub land, occupying 96% or more of the total land area, while the grassland, waters, and unused land only had a smaller proportion. The four main land use types had different effects on the runoff depth. The contribution coefficient of forestland, shrub land and construction land to the runoff depth was 2.61, 0.38, and 0.34 mm·km-2, respectively, implying that these three land use types had positive effects on the runoff depth in this basin. On the contrary, the contribution coefficient of farmland was -0.11 mm·km-2, implying that farmland had negative effect on the runoff depth.