南昌工程学院学报
南昌工程學院學報
남창공정학원학보
JOURNAL OF NANCHANG INSTITUTE OF TECHNOLOGY
2014年
4期
58-61
,共4页
坡面水流%红壤%坡面%径流率
坡麵水流%紅壤%坡麵%徑流率
파면수류%홍양%파면%경류솔
slope flow%red soil%slope%runoff rate
为了研究坡面径流特征,采用上方人工放水实验模拟坡面水流,研究不同放水流量强度、不同坡长及不同坡度条件下红壤坡面径流过程特征。结果表明:(1)不同放水流量强度条件下,坡面径流率随径流历时的变化总体上呈先逐渐增大,后趋于稳定的变化过程,且放水流量强度越小,坡面径流率的增长速度反而越大;(2)不同坡长条件下,坡面径流率随径流历时的变化过程总体上先逐渐增大,后趋于稳定,且随坡长的增大,坡面径流率越小;(3)不同坡度条件下,坡面径流率随径流历时大部分先逐渐增大,后趋于稳定,对于两个较陡坡(50°和65°)且放水流量较大的坡面,坡面径流率随历时先逐渐减小,后趋于稳定。
為瞭研究坡麵徑流特徵,採用上方人工放水實驗模擬坡麵水流,研究不同放水流量彊度、不同坡長及不同坡度條件下紅壤坡麵徑流過程特徵。結果錶明:(1)不同放水流量彊度條件下,坡麵徑流率隨徑流歷時的變化總體上呈先逐漸增大,後趨于穩定的變化過程,且放水流量彊度越小,坡麵徑流率的增長速度反而越大;(2)不同坡長條件下,坡麵徑流率隨徑流歷時的變化過程總體上先逐漸增大,後趨于穩定,且隨坡長的增大,坡麵徑流率越小;(3)不同坡度條件下,坡麵徑流率隨徑流歷時大部分先逐漸增大,後趨于穩定,對于兩箇較陡坡(50°和65°)且放水流量較大的坡麵,坡麵徑流率隨歷時先逐漸減小,後趨于穩定。
위료연구파면경류특정,채용상방인공방수실험모의파면수류,연구불동방수류량강도、불동파장급불동파도조건하홍양파면경류과정특정。결과표명:(1)불동방수류량강도조건하,파면경류솔수경류력시적변화총체상정선축점증대,후추우은정적변화과정,차방수류량강도월소,파면경류솔적증장속도반이월대;(2)불동파장조건하,파면경류솔수경류력시적변화과정총체상선축점증대,후추우은정,차수파장적증대,파면경류솔월소;(3)불동파도조건하,파면경류솔수경류력시대부분선축점증대,후추우은정,대우량개교두파(50°화65°)차방수류량교대적파면,파면경류솔수력시선축점감소,후추우은정。
In order to study the characteristics of slope runoff of red soil,this paper conducts artificial drainage experiments to simulate the slope runoff under different water flow intensity,slope length and gra-dient. The results show that:(1)under the condition of different water flow intensity,the runoff rate in-creases in the beginning but becomes stable later. The growth rate is greater when the flow becomes smal-ler;(2)under the condition of different slope length,the rate changing shows the same tendency,but the figure is smaller when the slope length becomes longer;(3)the same changing pattern is also found in most time under the condition of different slope,but exception is observed in two more steep slopes(50° and 65°)where the pattern is decreasing first before stabilization.