Rainfall simulation for the study of the effects of efficient factors on run-off rate

被引:1
作者
Vahabi, J. [1 ]
Mahdian, M. H. [1 ]
机构
[1] Soil Conservat & Watershed Management Res Ctr, Tehran, Iran
来源
CURRENT SCIENCE | 2008年 / 95卷 / 10期
关键词
Antecedent soil moisture content; rainfall simulator; run-off rate; slope and vegetation cover;
D O I
暂无
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Depending upon the watershed characteristics and weather conditions, a substantial part of the precipitation may be changed into run-off. Knowledge about the discharge and volume of the run-off generated by rainfall, especially in ungauged catchments, plays an important role in water resources management planning. In the absence of sufficient data recorded from the real rainfall events, use of rainfall simulators in the field and laboratory may be recommended to simulate runoff in different conditions of soil, vegetation cover, slope and rainfall. In this study, a rainfall simulator ( a portable non-pressurized type) was used to examine the effects of slope steepness, vegetation cover, clay, sand, silt and antecedent soil moisture content on run-off amount. Two sets of simulated rainfall events with 24.5 and 32 mm/h intensity were applied on 145 experimental plots with dimensions 1.2 m x 0.89 m in Taleghan watershed, Iran, and the relevant run-off amounts were measured in each experimental plot. Based on the results obtained from the correlation matrix, the most influential factors on run-off were vegetation cover, antecedent soil moisture content, clay, sand, silt and slope, for rainfall intensity of 24.5 mm/h. While for the rainfall intensity of 32 mm/h, vegetation cover, sand, antecedent soil moisture content, silt, clay and slope were the most influential factors. Two regression equations were also developed for predicting surface run-off with different field and rainfall conditions.
引用
收藏
页码:1439 / 1445
页数:7
相关论文
共 8 条
[1]   Aggregate stability as an indicator of soil susceptibility to runoff and erosion;: validation at several levels [J].
Barthès, B ;
Roose, E .
CATENA, 2002, 47 (02) :133-149
[2]  
CHARKHABI AH, 2003, P 8 SOIL SCI C IR, P899
[3]  
EATEMADI H, 1997, THESIS T MODARRES U
[4]  
GIORDANENGO JH, HYDROLOGIC RESPONSE
[5]   Runoff and sediment yield in a semi-arid environment:: the effect of land management after farmland abandonment [J].
Lasanta, T ;
García-Ruiz, JM ;
Pérez-Rontomé, C ;
Sancho-Marcén, C .
CATENA, 2000, 38 (04) :265-278
[6]  
Lasanta T, 2001, MT RES DEV, V21, P69, DOI 10.1659/0276-4741(2001)021[0069:MLAEIT]2.0.CO
[7]  
2
[8]   SLOPE AND PHOSPHOGYPSUMS EFFECTS ON RUNOFF AND EROSION [J].
WARRINGTON, D ;
SHAINBERG, I ;
AGASSI, M ;
MORIN, J .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1989, 53 (04) :1201-1205