EFFECTS OF GLEN CANYON DAM ON COLORADO RIVER SAND DEPOSITS USED AS CAMPSITES IN GRAND-CANYON NATIONAL-PARK, USA

被引:34
作者
KEARSLEY, LH
SCHMIDT, JC
WARREN, KD
机构
[1] National Park Service, Division of Resources Management, Flagstaff, Arizona, 86002
[2] Watershed Science Unit, Department of Geography and Earth Resources, Utah State University, Logan, Utah
[3] National Park Service, Division of Resources Management, Arizona, 86023
来源
REGULATED RIVERS-RESEARCH & MANAGEMENT | 1994年 / 9卷 / 03期
关键词
SAND BARS; EROSION; COLORADO RIVER; REGULATED RIVERS; CAMPSITES;
D O I
10.1002/rrr.3450090302
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Glen Canyon Dam, located on the Colorado River 24 km upstream from Grand Canyon National Park, has affected downstream alluvial sand deposits which are used as campsites by recreational boaters. Inventories of campsite numbers and sizes conducted in 1973, 1983 and 1991, and comparison of aerial photograph series taken in 1965, 1973, 1984 and 1990 show that there has been a system-wide decrease in the number and size of campsites. Campsites are unevenly distributed along the river, and availability is regarded as 'critical' along reaches comprising 45% of the river, based on interviews with river guides. During the first 10 years of Glen Canyon Dam operations, at least 30% of all campsites decreased in size. During the next 18 years, between 1973 and 1991, 32% of all campsites decreased in size, and campsite capacity decreased by 44%. High annual dam releases in excess of power plant capacity in 1983 caused a net system-wide increase in the number of campsites, but decreased campsite capacity in two critical reaches. The 'benefit' of sand aggradation due to the 1983 high flow was short-lived, and by 1991 only a few campsites were larger than they had been in 1973. In contrast, other sites, especially in critical reaches, were eroded by the 1983 high flows and have not recovered in size. Options for future dam management must consider the variable response of campsites to high flows in critical and non-critical reaches and the duration over which 'beneficial' high flow effects persist.
引用
收藏
页码:137 / 149
页数:13
相关论文
共 33 条
[1]  
Andrews E.D., ‘Downstream effects of Flaming Gorge Reservoir on the Green River, Colorado and Utah’, Geol. Soc. Am. Bull., 97, pp. 1012-1023, (1986)
[2]  
Andrews E.D., The Colorado River
[3]  
a perspective from Lees Ferry, Arizona, Surface Water Hydrology. The Geology of North America, 1, pp. 304-310, (1990)
[4]  
Beus S.S., Carothers S.W., Avery C.C., ‘Topographic changes in fluvial terrace deposits used as campsite beaches along the Colorado River in Grand Canyon’, J. AZ‐NV Acad. Sci., 20, pp. 111-120, (1985)
[5]  
Beus S.S., Kaplinski M.A., Hazel J.E., Tedrow L.A., Mayes H.B., Fillmore R.P., (1993)
[6]  
Brian N.J., Thomas J.R., (1984)
[7]  
Hazel J.E., Kaplinski M.A., Beus S.S., Tedrow L.A., ‘Sand bar stability and response to interim flows after a barbuilding event on the Colorado River, Grand Canyon, Arizona: implications for sediment storage and sand bar maintenance’ [abstract], EOS, 74, (1993)
[8]  
Hirsch R.V., Walker J.F., Day J.C., Kallio R., The influence of man on hydrologic systems, Surface Water Hydrology. The Geology of North America, 1, pp. 329-359, (1990)
[9]  
Howard A.D., Doland R., ‘Geomorphology of the Colorado River in Grand Canyon’, J. Geol., 89, pp. 269-298, (1981)
[10]  
Johnson R.R., Historic changes in vegetation along the Colorado River in the Grand Canyon, National Research Council, Colorado River Ecology and Dam Management. Proceedings of a Symposium held 24–25 May 1990, Santa Fe, New Mexico, pp. 178-206, (1991)