This paper describes meandering alluvial rivers with mean annual suspended-sediment concentrations of more than 100 kgm-3 on the Loess Plateau, China, and explains their formation as caused by the effect of hyperconcentrated water flow. When the river is dominated by hyperconcentrated flow, the rate
β¦ LIBER β¦
Erosion caused by hyperconcentrated flow on the Loess Plateau of China
β Scribed by Xu Jiongxin
- Book ID
- 117499396
- Publisher
- Elsevier Science
- Year
- 1999
- Tongue
- English
- Weight
- 363 KB
- Volume
- 36
- Category
- Article
- ISSN
- 0341-8162
No coin nor oath required. For personal study only.
π SIMILAR VOLUMES
Meanders caused by hyperconcentrated wat
β
Xu Jiongxin
π
Article
π
1993
π
John Wiley and Sons
π
English
β 880 KB
Consequences of hyperconcentrated flow f
β
Rudi Hessel
π
Article
π
2006
π
John Wiley and Sons
π
English
β 342 KB
A study of physico-geographical factors
β
Jiongxin Xu
π
Article
π
1998
π
Elsevier Science
π
English
β 350 KB
Soil erosion processes in the loess plat
β
Zhang Zonghu
π
Article
π
1991
π
Springer Netherlands
π
English
β 880 KB
The soil erosion processes in the Loess Plateau may be divided into three types: namely, waterflow erosion; gravitational erosion; wind erosion. The waterflow erosion is most widely distributed and is the main erosion action in the Loess Plateau. The main factors dominating the occurrence and develo
An early Holocene erosion phase on the l
β
Chun Chang Huang; Jiangli Pang; Ping Huang
π
Article
π
2002
π
Elsevier Science
π
English
β 223 KB
Precipitationβvegetation coupling and it
β
Xu Jiongxin
π
Article
π
2005
π
Elsevier Science
π
English
β 337 KB