[1]ZHANG Zhi-ling,FAN Hao-ming,GUO Cheng-jiu,et al.The Temporal and Spatial Variation of Runoff and Sediment Discharge in Liuhe River Basin[J].Research of Soil and Water Conservation,2008,15(01):229-231.
Copy
The Temporal and Spatial Variation of Runoff and Sediment Discharge in Liuhe River Basin
Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
15
Number of periods:
2008 01
Page number:
229-231
Column:
Public date:
2008-02-20
- Title:
- The Temporal and Spatial Variation of Runoff and Sediment Discharge in Liuhe River Basin
- CLC:
- S157;P332.5
- DOI:
- -
- Abstract:
- Liuhe River basin is one of the most serious rivers in the sediment problem of the northeast region, having the characteristics of river sediment to silt up severity, a great deal of deposition and outputting the quantity high toward the Liao River.This text analyzed runoff and sediment discharge of temporal and spatial variation from the middle of 20 centuries to 21 centuries, and studied runoff and sediment discharge to close related connection coefficient and connection of amount of sand.As a result, the Liuhe River basin runoff temporal and spatial variation is asymmetry, and have with time of development, more the trend of asymmetry.Runoff with sediment discharge has a very close relation, the connection of each station from 0.560 to 0.921, but total up, the connection is bigger.
- References:
-
[1] 范昊明, 蔡强国, 杨传强, 等.柳河流域沙量平衡分析(1968-1983)[J].农业工程学报, 2005, 21(增刊):52-55.
[2] 冯光杨.水文年内不均匀系数的探讨[J].山地研究, 1991, 9(1):27-32.
[3] 刘德林, 刘贤赵, 张继平.大沽夹河流域径流年内分配特征的量化研究[J].水土保持研究, 2006, 13(6):106-109.
[4] 汪翔.资水流域泥沙特征分析[J].湖南水利水电, 2000(6):23-25.
[5] 范昊明, 蔡强国.柳河流域悬移质泥沙颗粒特征分析[J].辽宁工程技术大学学报, 2005, 24(6):1-4.
[6] Haoming Fan, Qiangguo Cai.A Suspended Sediment Budget for Liu River Drainage Basin (1968-2003)[C].Sediment Budget 1, Proceedings of workshop held at Fozdo Iguacu, Brazil, 2005, IAHS Publ.2005, 291:243-249.
- Similar References:
Memo
-
Last Update:
1900-01-01