Width of streams and rivers in response to vegetation, bank material, and other factors

被引:80
作者
Anderson, RJ
Bledsoe, BR
Hession, WC
机构
[1] Telesto Solut Inc, Ft Collins, CO 80525 USA
[2] Colorado State Univ, Dept Civil Engn, Ft Collins, CO 80523 USA
[3] Univ Vermont, Dept Civil & Environm Engn, Burlington, VT 05405 USA
来源
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION | 2004年 / 40卷 / 05期
关键词
river restoration; river engineering; stable channel design; fluvial geomorphology; hydraulics; watershed management;
D O I
10.1111/j.1752-1688.2004.tb01576.x
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
An extensive group of datasets was analyzed to examine factors affecting widths of streams and rivers. Results indicate that vegetative controls on channel size are scale dependent. In channels with watersheds greater than 10 to 100 km(2) widths are narrower in channels with thick woody bank vegetation than in grass lined or nonforested banks. The converse is true in smaller streams apparently due to interactions between woody debris, shading, understory vegetation, rooting characteristics, and channel size. A tree based statistical method (regression tree) is introduced and tested as a tool for identifying thresholds of response and interpreting interactions between variables. The implications of scale dependent controls on channel width are discussed in the context of stable channel design methods and development of regional hydraulic geometry curves.
引用
收藏
页码:1159 / 1172
页数:14
相关论文
共 81 条
[1]   Where along a river's length will vegetation most effectively stabilise stream banks? [J].
Abernethy, B ;
Rutherfurd, ID .
GEOMORPHOLOGY, 1998, 23 (01) :55-75
[2]  
ALLMENDINGER NL, 1999, EOS T AM GEOPHYS U S, V80
[3]  
ANDREWS ED, 1984, GEOL SOC AM BULL, V95, P371, DOI 10.1130/0016-7606(1984)95<371:BEAHGO>2.0.CO
[4]  
2
[5]  
Annable W.K, 1996, DATABASE MORPHOLOGIC
[6]  
[Anonymous], 1962, GEOL SURV PROF PAPER
[7]  
[Anonymous], USDA SOIL CONSERVATI
[8]  
[Anonymous], 2001, SPLUS 6 WIND US GUID
[9]  
[Anonymous], 2022, INTRO RECURSIVE PART
[10]  
Barnes Jr H. H., 1967, 1849 US GEOL SURV