首页> 外文期刊>Earth Surface Dynamics Discussions >Morphodynamic regime change in a reconstructed lowland stream
【24h】

Morphodynamic regime change in a reconstructed lowland stream

机译:重建的低地河流形态动力学变化

获取原文
           

摘要

With the aim to establish and understand morphological changes in response to channel reconstruction, a detailed monitoring plan was implemented in a lowland stream called Lunterse Beek, located in the Netherlands. Over a period of almost 2 years, the monitoring programme included serial morphological surveys, continuous discharge and water level measurements, and riparian vegetation mapping, from photographs and field surveys. Morphological processes occurred mainly in the initial period, before riparian vegetation developed. The initial period was largely dominated by upstream sediment supply, which was associated with channel incision upstream from the study area. Herbaceous vegetation started to develop approximately 7 months after channel reconstruction. The monitoring period included two growing seasons. A clear increase of riparian vegetation cover from first to the second year was observed. Detailed morphological and hydrological data show a marked difference in morphological behaviour between the pre-vegetation and post-vegetation stage. A linear regression procedure was applied to relate morphological activity to time-averaged Shields stress. In the initial stage after channel reconstruction, with negligible riparian vegetation, channel morphology adjusted, showing only a weak response to the discharge hydrograph. In the subsequent period, morphological activity in the channel showed a clear relation with discharge variation. The two stages of morphological response to the restoration measures may be largely associated with the upstream sediment supply in the initial period. Riparian vegetation may have played a substantial role in stabilizing the channel banks and floodplain area, gradually restricting the morphological adjustments to the channel bed.
机译:为了建立和了解响应通道重建的形态变化,在位于荷兰的低地河流Lunterse Beek中实施了详细的监测计划。在将近2年的时间里,监测计划包括一系列的形态学调查,连续的流量和水位测量以及来自照片和现场调查的河岸植被测绘。形态过程主要发生在河岸植被发展之前的初期。初始阶段主要由上游沉积物供应所主导,这与研究区域上游的河道切口有关。通道重建后约7个月,草本植被开始发育。监测期包括两个生长季节。从第一年到第二年,河岸植被覆盖率明显增加。详细的形态和水文数据表明,植被前和植被后阶段之间的形态行为存在明显差异。应用线性回归程序将形态活动与平均时间的Shields应力相关。在河道重建后的初期,河岸植被可以忽略不计,河道形态得以调整,仅显示了对排放水位图的较弱响应。在随后的时期中,通道中的形态活动与放电变化呈明显关系。对恢复措施的形态反应的两个阶段可能与初期的上游沉积物供应有关。河岸植被可能在稳定河岸和洪泛区,逐步限制河床形态调整方面起了重要作用。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号