吉林农业大学学报
吉林農業大學學報
길임농업대학학보
JOURNAL OF JILIN AGRICUL TURAL UNIVERSITY
2014年
1期
77-81
,共5页
王宇%宋金函%马悦%吕士东%裴乔%赵兰坡%张洪江
王宇%宋金函%馬悅%呂士東%裴喬%趙蘭坡%張洪江
왕우%송금함%마열%려사동%배교%조란파%장홍강
黑土坡面%初始产流时间%径流量%径流系数%细沟
黑土坡麵%初始產流時間%徑流量%徑流繫數%細溝
흑토파면%초시산류시간%경류량%경류계수%세구
slope of black soil%initial runoff production time%runoff amount%runoff coefficient%rill
以土槽模拟自然坡面,在人工降雨条件下,对黑土坡面径流参数进行了分析。结果表明:随着降雨强度(简称“雨强”)和坡度的增大,黑土坡面径流的初始产流时间缩短,径流量和径流系数增加。在前期降雨条件下,二次降雨所表现的径流侵蚀特征均强于首次降雨。黑土坡面产生细沟的时间随坡度增大而缩短,当坡度>15°时,细沟产生时间基本一致,细沟的数量及长、宽、深等参数增大,坡度对沉积的影响作用大于降雨强度。
以土槽模擬自然坡麵,在人工降雨條件下,對黑土坡麵徑流參數進行瞭分析。結果錶明:隨著降雨彊度(簡稱“雨彊”)和坡度的增大,黑土坡麵徑流的初始產流時間縮短,徑流量和徑流繫數增加。在前期降雨條件下,二次降雨所錶現的徑流侵蝕特徵均彊于首次降雨。黑土坡麵產生細溝的時間隨坡度增大而縮短,噹坡度>15°時,細溝產生時間基本一緻,細溝的數量及長、寬、深等參數增大,坡度對沉積的影響作用大于降雨彊度。
이토조모의자연파면,재인공강우조건하,대흑토파면경류삼수진행료분석。결과표명:수착강우강도(간칭“우강”)화파도적증대,흑토파면경류적초시산류시간축단,경류량화경류계수증가。재전기강우조건하,이차강우소표현적경류침식특정균강우수차강우。흑토파면산생세구적시간수파도증대이축단,당파도>15°시,세구산생시간기본일치,세구적수량급장、관、심등삼수증대,파도대침적적영향작용대우강우강도。
Runoff parameters of black soil slope were analyzed depending on artificial rainfall simulation experiment .The results show that on black soil slope,initial runoff production time was shortened,and runoff amount and runoff coefficient were increased as rainfall intensity and slope increased .On pre-rain-fall conditions,runoff erosion characteristics of the second rainfall were stronger than the first rainfall . The time of rill forming was shortened as slope increased .When the slope was increased to 1 5°,rill gen-erated at approximately the same time,amount,length,width and depth of rill were increased along with the increase of slope,and the effect of slope gradient on deposition was greater than rainfall intensity .