Comment on 'Scale relationships in hillslope runoff and erosion' (Earth Surface Processes and Landforms 31: 1364-1383 (2006))

Earth Surface Processes and Landforms

Volumn 33, Issue 10, 2008, Pages 1632-1636

  Kinnell, Peter I A ^a  

^a UNIVERSITY OF CANBERRA   (Australia)

Author keywords

Runoff; Sediment yield; Slope length; Soil erosion

Indexed keywords

EID: 54749147529     PISSN: 01979337     EISSN: 10969837     Source Type: Journal    
DOI: 10.1002/esp.1630     Document Type: Note

References (6)

1. Kinnell PIA, Risse LM. 1998. USLE-M: empirical modelling rainfall erosion through runoff and sediment concentration. Soil Science Society America Journal 62: 1667-1672.
2. Parsons AJ, Brazier RE, Wainwright J, Powell DM. 2006a. Scale relationships in hillslope runoff and erosion. Earth Surface Processes and Landforms 31: 1364-1393.
3. Parsons AJ, Wainwright J, Abrahams AD. 1993. Tracing sediment movement in interrill overland flow on a semi-arid grassland hillslope using magnetic susceptibility. Earth Surface Processes and Landforms 18: 712-732.
4. Parsons AJ, Wainwright J, Powell DM, Kaduk J, Brazier RE. 2004. A conceptual model for determining soil erosion by water. Earth Surface Processes and Landforms 29: 1293-1302.
5. Parsons AJ, Wainwright J, Powell DM, Kaduk J, Brazier RE. 2006b. Is sediment delivery a fallacy? Earth Surface Processes and Landforms 31: 1325-1328.
6. Rejman J, Usowich B, Debicki R. 1999. Sources of error in predicting silt soil erodibility with USLE. Polish Journal of Soil Science 32: 13-22.