Features of Baseflow and Its Influencing Factors for Small Watersheds in Loess Hilly and Gully Region
|更新时间:2025-03-12
|
Features of Baseflow and Its Influencing Factors for Small Watersheds in Loess Hilly and Gully Region
Bulletin of Soiland Water ConservationVol. 30, Issue 1, Pages: 87-92(2011)
作者机构:
1. 北京林业大学水土保持学院,北京,100083
2. 华北电力大学能源与环境研究中心,北京,102206
3. The Federal Institute of Land and Water Management Research, A-3252, Petzenkirchen,Austria
作者简介:
基金信息:
DOI:
CLC:X37
Published:2011
稿件说明:
移动端阅览
GUO Jun-ting, ZHANG Zhi-qiang, WANG Sheng-ping, et al. Features of Baseflow and Its Influencing Factors for Small Watersheds in Loess Hilly and Gully Region[J]. Bulletin of Soiland Water Conservation, 2011, 30(1): 87-92.
DOI:
GUO Jun-ting, ZHANG Zhi-qiang, WANG Sheng-ping, et al. Features of Baseflow and Its Influencing Factors for Small Watersheds in Loess Hilly and Gully Region[J]. Bulletin of Soiland Water Conservation, 2011, 30(1): 87-92.DOI:
Features of Baseflow and Its Influencing Factors for Small Watersheds in Loess Hilly and Gully Region
especially in the arid loess hilly and gully region.It accounts for a large proportion of total runoff and provide additional flow supply to the rivers during the dry seasons.Therefore
the research of baseflow characteristics and its impact factors in this area could contribute to more reasonable water regulations and more efficient uses of water resources.In this paper
digital filtering method was used to separate the baseflow of Caijiachuan basin from 2006to 2008.By calculating the baseflow index (BFI)
controlling factors including precipitation events
land use
vegetation cover and terrain characteristics of the basin were analyzed.The results show that annual BFI averages ranged from 0.68 to 0.82.BFIs decreased with increase of precipitation.Agricultural land
scrub and plantation had negative effects on the base flow.BFIs had a linear relationship with rainfall amounts(P)
river networks densities (D)and river gradients(S).The regression analysis provides a basis to analyze the characteristics of baseflow in ungauged area.