首页> 外文期刊>River Research and Applications >A GEOMORPHIC MONITORING AND ADAPTIVE ASSESSMENT FRAMEWORK TO ASSESS THE EFFECT OF LOWLAND FLOODPLAIN RIVER RESTORATION ON CHANNEL-FLOODPLAIN SEDIMENT CONTINUITY
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A GEOMORPHIC MONITORING AND ADAPTIVE ASSESSMENT FRAMEWORK TO ASSESS THE EFFECT OF LOWLAND FLOODPLAIN RIVER RESTORATION ON CHANNEL-FLOODPLAIN SEDIMENT CONTINUITY

机译:地貌监测和自适应评估框架,以评估低地洪泛河道恢复对渠道-洪泛区沉积物连续性的影响

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摘要

The state of the science of lowland river floodplain restoration reflects the relatively new and experimental nature of large river floodplain rehabilitation efforts. Based on results of a case study of floodplain restoration at the lowland Cosumnes River, California, we present a geomorphic monitoring and adaptive assessment framework that addresses the need to inform and utilize scientific knowledge in lowland floodplain river restoration activities. Highlighting hydrogeomorphic processes that lead to habitat creation, we identify a discharge threshold for connectivity and sediment transfer from the channel to the floodplain and integrate discharge magnitude and duration to quantify a threshold to aid determination of when geomorphic monitoring is warranted. Using floodplain sand deposition volume in splay complexes as one indicator of dynamic floodplain habitat, we develop a model to aid prediction of the sand deposition volume as an assessment tool to use to analyze future monitoring data. Because geomorphic processes that form the physical structure of a habitat are dynamic, and because the most successful restoration projects accommodate this fundamental characteristic of ecosystems, monitoring designs must both identify trends and be adapted iteratively so that relevant features continue to be measured. Thus, in this paper, adaptive assessment is defined as the modification of monitoring and analysis methods as a dynamic system evolves following restoration activities. The adaptive monitoring and assessment methods proposed facilitate long-term measurements of channel-floodplain sediment transfer, and changes in sediment storage and morphology unique to lowland river-floodplain interactions and the habitat that these physical processes support. The adaptive assessment framework should be integrated with biological and chemical elements of an interdisciplinary ecosystem monitoring program to answer research hypotheses and to advance restoration science in lowland floodplain river systems.
机译:低地河流漫滩恢复的科学状况反映了大型河流漫滩恢复工作的相对较新的实验性质。基于加利福尼亚低地科苏姆内斯河漫滩恢复的案例研究结果,我们提出了一种地貌监测和适应性评估框架,解决了在低陆漫滩河恢复活动中提供信息和利用科学知识的需求。着重介绍导致栖息地形成的水文地貌过程,我们确定了连通性和沉积物从河道到洪泛区的排放阈值,并整合了排放量和持续时间以量化阈值,以帮助确定何时需要进行地貌监测。我们使用发play综合体中的洪泛区沙沉积量作为动态洪泛区生境的指标,我们开发了一个模型来辅助预测沙沉积量,并将其作为评估工具来分析未来的监测数据。由于形成栖息地物理结构的地貌过程是动态的,并且由于最成功的修复项目具有生态系统的这一基本特征,因此监控设计必须既能识别趋势又能进行迭代调整,以便继续测量相关特征。因此,在本文中,自适应评估被定义为随着动态系统随着恢复活动的发展而对监视和分析方法的修改。提出的自适应监测和评估方法有助于长期测量河道-滩涂沉积物的转移,以及低地河流-滩涂相互作用和这些物理过程所支持的栖息地所特有的沉积物存储和形态变化。适应性评估框架应与跨学科生态系统监测计划的生物和化学要素相结合,以回答研究假设并促进低地洪泛河系的恢复科学。

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