SEDIMENT DELIVERY PROCESSES AT BASIN-SCALE

被引:191
作者
FERRO, V [1 ]
MINACAPILLI, M [1 ]
机构
[1] UNIV PALERMO,FAC AGR,DIPARTIMENTO EITA,I-90128 PALERMO,ITALY
来源
HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES | 1995年 / 40卷 / 06期
关键词
D O I
10.1080/02626669509491460
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Since eroded sediments are produced from different sources distributed throughout a basin, sediment delivery processes at basin scale have to be modelled by a spatially distributed approach. In this paper a new theoretically based relationship is proposed for evaluating the sediment delivery ratio, SDR(i), of each morphological unit, i, into which a basin is divided. Then, using the sediment balance equation written for the basin outlet, a relationship between the basin sediment delivery ratio, SDR(w) and the SDR(i) is deduced. This relationship is shown to be independent of the soil erosion model used. Finally, a morphological criterion for estimating a coefficient, beta, is proposed.
引用
收藏
页码:703 / 717
页数:15
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