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River regulation and riparian woodlands: Cottonwood conservation with an environmental flow regime along the Waterton River, Alberta

机译:河流调节和河岸林地:艾伯塔省沃特顿河沿岸的杨木保育和环境流动机制

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Following water withdrawal, riparian cottonwoods have declined downstream from some dams in western North America. Analyses of aerial photographs and field observations in the 1980s suggested that the black and narrowleaf cottonwoods (Populus trichocarpa and Populus angustifolia) along the Waterton River, Alberta, were declining due to drought stress following the 1964 damming and diversion. This raised concern for the riverine ecosystems and in 1991, functional flows commenced with 2 changes: (a) the minimum flow was increased from 0.9 to 2.3m(3)/s (mean discharge 21.9m(3)/s) and (b) flow ramping provided gradual stage recession after the spring peak. This provided an environmental flow regime that was delivered for 2 decades and this study investigated the consequent river flow patterns and riparian woodlands upstream and downstream from the Waterton Dam. Analyses of aerial photographs from 1951 to 2009 assessed 4 flow management intervals: (a) the free-flowing predam condition, (b) the initial dammed interval to the mid-1970s, (c) a drought interval in the 1980s, and (d) with the environmental flow regime after 1991. Analyses revealed woodland reduction from 1961 to 1985 due to losses through bank erosion with major floods and apparent decline due to low flows following a regional drought and water withdrawal for irrigation. With the subsequent environmental flow regime, there was apparent woodland recovery, despite drought in 2000 and 2001. This study demonstrated that the correspondence between river flow patterns and the extent of riparian woodlands and the benefit from the environmental flow regime that probably reduced drought stress and mortality.
机译:取水后,沿河三角叶杨木在北美西部的一些水坝下游已经下降。对1980年代航空摄影和实地观察的分析表明,由于1964年大坝和改道后的干旱压力,沿亚伯大省沃特顿河沿岸的黑色和窄叶杨木(Populus trichocarpa和Populus angustifolia)正在减少。这引起了对河流生态系统的关注,1991年,功能流量开始发生了两个变化:(a)最小流量从0.9增加到2.3m(3)/ s(平均流量21.9m(3)/ s)和(b )流量上升提供了弹簧峰值后的逐步衰退。这提供了一个持续了20年的环境水流状态,本研究调查了由此导致的河水流型和沃特顿大坝上游和下游的河岸林地。对1951年至2009年的航拍照片进行的分析评估了4个流量管理间隔:(a)自由流动的坝前状况,(b)到1970年代中期的初始坝期,(c)1980年代的干旱期,和(d ),并采用1991年后的环境流量制度。分析显示,1961年至1985年,林地减少是由于大洪水造成的河岸侵蚀造成的损失,以及区域干旱和灌溉取水后流量低造成的明显减少。在随后的环境流量制度下,尽管2000年和2001年发生了干旱,林地仍出现了明显的恢复。这项研究表明,河流流量模式与河岸林地的范围之间的对应关系以及环境流量制度的好处可能减轻了干旱压力和死亡。

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