Sediment yield and transport process assessment from reservoir monitoring in a semi-arid mountainous river

2018 ◽  
Vol 32 (19) ◽  
pp. 2990-3005 ◽  
Author(s):  
Agustín Millares ◽  
Antonio Moñino
2004 ◽  
Vol 29 (11) ◽  
pp. 1359-1372 ◽  
Author(s):  
Allen C. Gellis ◽  
Milan J. Pavich ◽  
Paul R. Bierman ◽  
Eric M. Clapp ◽  
Amy Ellevein ◽  
...  

Solid Earth ◽  
2015 ◽  
Vol 6 (2) ◽  
pp. 433-443 ◽  
Author(s):  
P. Sarah ◽  
M. Zonana

Abstract. Semi-arid areas where grazing is the main land use exhibit a "three-phase-mosaic" pattern of dominant surface patches: shrubs, trampling routes, and intershrub areas. This pattern differs from the "two-phase mosaic" seen in grazing-free semi-arid areas. The patches might create a positive feedback process in which enhanced infiltration beneath shrubs minimizes overland flow from under their canopies, thereby strengthening the sink–source mechanism by which overland flow generated between shrubs rapidly infiltrates into the soil beneath them, where it deposits soil particles, litter, nutrients and organic matter, thereby enhancing infiltration by changing the local microtopography, and improving soil properties. To analyze sink–source relationships among the patches in grazed areas in rangelands of the semi-arid northern Negev region of Israel, we constructed small runoff plots, 0.25–1.0 m2 in area, of five types: shrub (Sarcopoterium spinosum), intershrub, route, route–shrub combination, and intershrub–shrub combination. The shrubs always occupied the downslope part of the plot. Overland flow and sediment deposits were measured in all plots during 2007/8 and 2008/9. The combined plots yielded much less overland flow and sediments than intershrub, routes and shrub ones, indicating that the shrubs absorbed almost all the yields of the upper part of their plots. The shrubs generated less runoff and sediments than routes and intershrubs; runoff flows from the routes and intershrubs were similar; sediment yield was highest in the intershrubs. Thus, runoff yield exhibited a two-phase mosaic pattern, and sediment yield, i.e., soil erosion, a three-phase mosaic pattern.


2012 ◽  
Vol 38 (4) ◽  
pp. 383-390 ◽  
Author(s):  
V. O. Polyakov ◽  
M. A. Nearing ◽  
A. A. Hawdon ◽  
S. N. Wilkinson ◽  
M. H. Nichols

2015 ◽  
Vol 40 (13) ◽  
pp. 1827-1838 ◽  
Author(s):  
Naomi Geeraert ◽  
Fred Ochieng Omengo ◽  
Fredrick Tamooh ◽  
Paolo Paron ◽  
Steven Bouillon ◽  
...  

2016 ◽  
Vol 7 (13) ◽  
pp. 271-263
Author(s):  
مجید کارگر ◽  
محمدرضا جوادی ◽  
سید علی اصغر هاشمی ◽  
مریم محمد ابراهیمی ◽  
◽  
...  
Keyword(s):  

2008 ◽  
Vol 58 (3) ◽  
pp. 403-409 ◽  
Author(s):  
Olfa Fourti ◽  
Yassine Haydri ◽  
Fuio Murano ◽  
Naceur Jedidi ◽  
Abdennaceur Hassen

2005 ◽  
Vol 30 (8) ◽  
pp. 935-953 ◽  
Author(s):  
Paul R. Bierman ◽  
Joanna M. Reuter ◽  
Milan Pavich ◽  
Allen C. Gellis ◽  
Marc W. Caffee ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document