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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Making connections: Changing sediment sources and sinks in an upland catchment
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Making connections: Changing sediment sources and sinks in an upland catchment

机译:建立联系:在高地流域改变沉积物来源和汇

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The effect of changes in catchment processes and conditions can be studied by using connectivity as a framework for understanding the feedbacks and interactions occurring within the system. The sediment record preserved in reservoirs can be a useful archive of catchment changes, but needs to be considered in conjunction with the different elements that compose and act on the system to take into account its complexity. Changing patterns of connectivity have been studied in the Ingbirchworth Catchment (Yorkshire, UK), using a multiple methodology approach combining the analysis of reservoir-sediment records with knowledge of recent land-use history, high resolution rainfall records, catchment characteristics and management aspects. Sedimentation rates inferred from reservoir-sediment cores from two reservoirs in the Ingbirchworth catchment show sedimentation peaks which coincide with periods of significant changes in the catchment, such as the introduction of arable crops, the establishment of land drainage and the widespread intensification and mechanization of agriculture. Rainfall patterns, including combinations of events such as droughts and increased precipitation, contribute to increased sediment transfer under catchment conditions in which more sediment and/or new pathways are made available due to catchment changes. Sediment fingerprinting supports the notion that changes in sedimentation rates are not just related to increased/reduced erosion and transport in the same areas, but also to the establishment of different pathways increasing sediment connectivity. The results demonstrate that typical calculations of catchment-area yields are not sufficient as sediment-contributing areas vary as a consequence of changing conditions. The study provides insights into the complex interactions influencing connectivity, such as the relation between catchment changes and climatic inputs, and the subsequent effect on catchment conditions and transfer networks.
机译:可以通过将连通性用作理解系统内发生的反馈和相互作用的框架来研究集水过程和条件变化的影响。保存在水库中的泥沙记录可以作为流域变化的有用档案,但是需要结合组成系统并对其起作用的不同要素加以考虑,以考虑其复杂性。在英格比尔奇沃思集水区(英国约克郡),已使用多种方法方法对水库泥沙记录进行了分析,并结合了近期土地使用历史,高分辨率降雨记录,集水特征和管理方面的知识,研究了连通性的变化模式。从英格比尔沃思流域的两个水库的水库-沉积物核心推断出的沉积率显示出沉积峰,与该流域发生重大变化的时期相吻合,例如引入耕种作物,建立土地排水系统以及广泛的集约化和机械化农业。降雨方式,包括干旱和降水增加等事件的组合,有助于在集水条件下增加沉积物的转移,在这些条件下,由于集水量的变化,会有更多的沉积物和/或新的途径。泥沙指纹法支持这样一种观点,即沉积速率的变化不仅与同一地区的侵蚀和运输增加/减少有关,而且与增加沉积物连通性的不同途径的建立有关。结果表明,流域面积产量的典型计算是不够的,因为条件变化的结果是沉积物分布面积会发生变化。该研究为影响连通性的复杂相互作用提供了见解,例如流域变化和气候输入之间的关系,以及对流域条件和转移网络的后续影响。

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