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首页> 外文期刊>Earth-Science Reviews: The International Geological Journal Bridging the Gap between Research Articles and Textbooks >The behavioural characteristics of sediment properties and their implications for sediment fingerprinting as an approach for identifying sediment sources in river basins
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The behavioural characteristics of sediment properties and their implications for sediment fingerprinting as an approach for identifying sediment sources in river basins

机译:沉积物特性的行为特征及其对沉积物指纹的启示,作为识别流域沉积物来源的一种方法

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摘要

Sediment fingerprinting is a technique that is increasingly being used to improve the understanding of sediment dynamics within river basins. At present, one of the main limitations of the technique is the ability to link sediment back to their sources due to the non-conservative nature of many of the sediment properties. The processes that occur between the sediment source locations and the point of collection downstream are not well understood or quantified and currently represent a black-box in the sediment fingerprinting approach. The literature on sediment fingerprinting tends to assume that there is a direct connection between sources and sinks, while much of the broader environmental sedimentology literature identifies that numerous chemical, biological and physical transformations and alterations can occur as sediment moves through the landscape. The focus of this paper is on the processes that drive particle size and organic matter selectivity and biological, geochemical and physical transformations and how understanding these processes can be used to guide sampling protocols, fingerprint selection and data interpretation. The application of statistical approaches without consideration of how unique sediment fingerprints have developed and how robust they are within the environment is a major limitation of many recent studies. This review summarises the current information, identifies areas that need further investigation and provides recommendations for sediment fingerprinting that should be considered for adoption in future studies if the full potential and utility of the approach are to be realised.
机译:泥沙指纹识别是一项越来越多的技术,用于增进对流域内泥沙动力学的理解。目前,由于许多沉积物性质的非保守性质,该技术的主要局限性之一是其能够将沉积物重新连接到其来源。在沉积物来源位置和下游收集点之间发生的过程尚未得到很好的理解或量化,目前代表着沉积物指纹法中的黑匣子。关于沉积物指纹的文献倾向于假定源与汇之间存在直接联系,而许多更广泛的环境沉积学文献都指出,随着沉积物在景观中的移动,会发生许多化学,生物和物理转化和变化。本文的重点是驱动粒径和有机物选择性以及生物,地球化学和物理转化的过程,以及如何理解这些过程可用于指导采样协议,指纹选择和数据解释。在不考虑独特的沉积物指纹如何发展以及它们在环境中有多健壮的情况下,统计方法的应用是许多近期研究的主要局限。这篇综述总结了当前的信息,确定了需要进一步研究的领域,并提供了沉积物指纹识别的建议,如果要充分利用该方法的潜力和实用性,则应在以后的研究中予以考虑。

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