Assessment of marl properties effect on sediment and runoff rate at different rainfall intensity under field rainfall simulator
نویسندگان
چکیده
منابع مشابه
CHANGE OF SPLASH EROSION RATE IN RAINFALL DIFFERENT DURATION AND INTENSITY ON MARL SOILS
Splash erosion is recognized as the first stage in the process of erosion that results in bombardment of the soil's surface with rain drops. Two basic processes in soil erosion are the dispersion of soil particles by rain drops and the changes caused to the soil's structure, which are then moved by runoff. In this research, the effect of various rainfall intensity (60, 90 and 120 mm/hr) on the ...
متن کاملInteraction Effect of Slope Aspect and Precipitation Intensity in Runoff and Sediment in Acid Rainfall
Soils are severely damaged by acid rain; acid rain also leads to excessive dissolving of minerals and valuable nutrients in the soil, which weakens vegetation. In this study, in order to determine the interaction effect between the slope aspect and precipitation intensity relative to acid rainfall in the Aghajari and Gachsaran formations, a part of Margha and Kuhe Gach watersheds of Izeh city w...
متن کاملeffect of nanozeolite on decreasing runoff using fel3 rainfall simulator at different slope
0
متن کاملInvestigation of Effective Factors on Runoff Generation and Sediment Yield of Loess Deposits Using Rainfall Simulator
متن کامل
assessment of runoff and sediment generation in neogene's units under rainfall simulator (case study: taleghan basin
in iran, fine grained formations (neogene's units) are very susceptible to erosion. also, they are the units producing runoff and causing soil loss in watersheds. the objectives of this study is to assess the effect of physical - chemical and mechanical properties of these formations on sediment and runoff rates at different rainfall intensities, based on using field simulator in taleghan ...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
ژورنال
عنوان ژورنال: Bulletin of the Serbian Geographical Society
سال: 2009
ISSN: 0350-3593,2406-078X
DOI: 10.2298/gsgd0904085h