4.4 Article

Effects of the Check Dam System on Water Redistribution in the Chinese Loess Plateau

Journal

JOURNAL OF HYDROLOGIC ENGINEERING
Volume 18, Issue 8, Pages 929-940

Publisher

ASCE-AMER SOC CIVIL ENGINEERS
DOI: 10.1061/(ASCE)HE.1943-5584.0000689

Keywords

Arid lands; Loess; Dams; Sediment; China; Water resources; Arid region; Loess Plateau; Check dam system; Sedimentary field; Numerical calculation; Water redistribution

Funding

  1. Japan Society for the Promotion of Sciences (JSPS) Core University Program
  2. Global COE Program of the Ministry of Education, Cultural, Sports, Science and Technology, Japan
  3. National Natural Science Foundation of China (NSFC) [41271046]
  4. Postdoctoral Science Foundation of China for overseas scholars [87328]
  5. Heilongjiang Provincial Department of Education Scientific Research Foundation for overseas scholars, China [1251H017]

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The objectives of this study are to evaluate the effects of the check dam system on water redistribution in a small basin in Chinese Loess Plateau by using a practical numerical method for the water budget process. Hydrological and meteorological observations were carried out in the small dam basin (). To quantitatively evaluate the effects of the check dam system on the water redistribution, hydrogeological modeling was applied to the check dam system in the basin. The numerical modeling was developed by kinematic wave theory for water flow. The model was verified by the numerical simulation of surface runoff discharge and groundwater level. Numerical calculation was carried out on the water budget of two cases: Case 1, no check dam (the control), and Case 2, with the check dam system in the year 2006. The model showed that the water budget of the surface runoff and groundwater flow in Case 1 was 97.3 and 2.7%, respectively. Conversely, the water budget of the runoff, evapotranspiration, infiltration, and change of water storage in Case 2 was 39.1, 49.3, 11.6, and 0%, respectively. The surface runoff in Case 2 decreased to 37.0% of that in Case 1. Compared with Case 1, two new componentsevapotranspiration and infiltrationappeared in Case 2. Moreover, groundwater outflow slightly increased, and the surface runoff decreased. The study indicates that these effects of the check dam system are mainly caused by the formation of the sedimentary field. Evapotranspiration and infiltration are generated from the sedimentary field. (C) 2013 American Society of Civil Engineers.

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