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首页> 外文期刊>River Research and Applictions >QUANTIFYING THE EFFECT OF RIPARIAN FOREST VERSUS AGRICULTURAL VEGETATION ON RIVER MEANDER MIGRATION RATES, CENTRAL SACRAMENTO RIVER, CALIFORNIA, USA
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QUANTIFYING THE EFFECT OF RIPARIAN FOREST VERSUS AGRICULTURAL VEGETATION ON RIVER MEANDER MIGRATION RATES, CENTRAL SACRAMENTO RIVER, CALIFORNIA, USA

机译:量化美国加利福尼亚州中部萨克拉门托河的里帕里亚森林对农业植被的影响,对河流调理迁移率的影响

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摘要

Riparian forest vegetation is widely believed to protect riverbanks from erosion, but few studies have quantified the effect of riparian vegetation removal on rates of river channel migration. Measured historical changes in a river channel centreline, combined with mapped changes in floodplain vegetation, provide an opportunity to test how riparian vegetation cover affects the erodibility of riverbanks. We analysed meander migration patterns from 1896 to 1997 for the central reach of the Sacramento River between Red Bluff and Colusa, using channel planform and vegetation cover data compiled from maps and aerial photography. We used a numerical model of meander migration to back-calculate local values for bank erodibility (i.e. the susceptibility of bank materials to erosion via lateral channel migration, normalized for variations in near-bank flow velocities due to channel curvature). A comparison of migration rates for approximately 50 years before and after the construction of Shasta dam suggests that bank migration rates and erodibility increased roughly 50%, despite significant flow regulation, as riparian flood-plains were progressively converted to agriculture. A comparison of migration rates and bank erodibilities between 1949 and 1997, for reaches bordered by riparian forest versus agriculture, shows that agricultural floodplains are 80 to 150% more erod-ible than riparian forest floodplains. An improved understanding of the effect of floodplain vegetation on river channel migration will aid efforts to predict future patterns of meander migration for different river management and restoration scenarios.
机译:人们普遍认为河岸森林植被可以保护河岸不受侵蚀,但是很少有研究量化河岸植被的清除对河道迁移速率的影响。测得的河道中心线的历史变化,与洪泛区植被的地图绘制变化相结合,为检验河岸植被覆盖如何影响河岸易蚀性提供了机会。我们使用渠道平面图和从地图和航空摄影中收集的植被覆盖数据,分析了1896年至1997年萨克拉曼多河在Red Bluff和Colusa之间的中游曲折迁移方式。我们使用了一个曲折迁移的数值模型来反算堤岸可侵蚀性的局部值(即,堤岸材料通过横向通道迁移而易受侵蚀的敏感性,针对因河道曲率而引起的堤岸近岸流速变化进行了归一化)。对沙斯塔水坝兴建前后约50年的迁移率进行比较,结果表明,尽管河流量大幅度调节,河岸迁移率和易蚀性仍增加了约50%,这是由于河岸漫滩逐渐转化为农业。通过对1949年至1997年之间沿河林与农业接壤的河段的迁移率和河岸通透性进行比较,可以看出,农业洪泛区的易蚀性比河岸森林洪泛区高80%至150%。更好地了解洪泛区植被对河道迁移的影响,将有助于预测不同河流管理和恢复情景下河道迁移的未来模式。

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