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The effect of the shortage of gravel sediment in midstream river channels on riparian vegetation cover

机译:中游河道碎石沉积物短缺对河岸植被的影响

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摘要

The vegetation cover in the steep, gravelly reaches of rivers was originally low. However, significant vegetation colonization can currently be observed in these riparian areas, and understanding the cause of this colonization is important for management. The objective of this study was to assess the effect of sediment deposition and erosion on vegetation colonization in gravel bed rivers. The delay in colonization by herbs and trees after sediment deposition or erosion was investigated using aerial photos of 6 Japanese rivers. A field study was conducted before and after a large flood at depositional and erosional locations. The colonization of vegetation after flushing was substantially delayed at sites where gravels were deposited compared with that at erosional sites, and it was faster in sandy reaches compared with gravelly reaches. Little tree colonization was observed at the depositional sites of gravelly sediments, whereas at erosional sites, new shoots sprouted from the collapsed live trees in the following spring, achieving a rapid increase in tree density. The nutrient and moisture contents of the sediment were significantly higher at the erosional sites. Gravels are deposited after washing and being segregated from fine sediment during floods. This coarse-sediment layer is low in moisture and nutrients compared with the erosional sites, at which the underlying sediments are exposed by flooding. However, moisture and nutrients are the primary requirements for vegetation colonization. Therefore, the reduction in gravelly sediments due to gravel mining, river regulation, and modification of river basins can have a substantial effect on vegetation colonization.
机译:陡峭的砾石河段的植被覆盖度本来很低。但是,目前在这些河岸地区可观察到大量植被定殖,因此了解这种定殖的原因对于管理很重要。这项研究的目的是评估沉积物沉积和侵蚀对砾石河床植被定殖的影响。使用6条日本河流的航拍照片调查了沉积物沉积或侵蚀后草药和树木的定居延迟。在沉积和侵蚀位置发生大洪水之前和之后进行了实地研究。冲刷后植被的定植在砂砾沉积的地点比在侵蚀地点的定植明显延迟,而在沙质段比砂砾段要快。在砾石沉积物的沉积部位观察到很少的树木定植,而在侵蚀部位,次年春天从倒塌的活树上发芽了新芽,树木密度迅速增加。在侵蚀点沉积物的养分和水分含量明显更高。砾石在洗涤后沉积,并在洪水期间与细沙分离。与侵蚀部位相比,该粗沉积层的水分和养分含量低,在该部位,下沉的沉积物被洪水淹没。但是,水分和养分是植被定殖的主要条件。因此,由于砾石开采,河流调节和流域改建而造成的砾石沉积物减少对植被定殖有重大影响。

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