高山环境沉积物源指纹识别的优势与局限性及其与土壤恢复的相关性

A. Frankl, O. Evrard, E. Cammeraat, A. Stokes
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引用次数: 0

摘要

高山环境是地球上最敏感的环境之一。由于人为干扰和气候变化,最近由于滑坡等原因引起的风土动员率一直在加速。结果,土壤退化,地质灾害发生,山洪暴发对下游地区造成负面影响。因此,迫切需要恢复高山环境中的土壤,并更好地了解基于自然的土地退化解决办法。寻找侵蚀源的起源是完善土壤修复策略和指导实施有效土壤修复措施的第一步,本文讨论了高山土壤修复背景下的沉积物源指纹研究。在此基础上,对沉积物源指纹技术在高山环境中的应用进行了综述,并对基于土地利用的标记物和土壤修复等方面的研究进行了展望。目前,沉积物物源研究在高山环境中的应用还很有限。虽然一些研究根据环境放射性核素或元素地球化学对沉积物来源进行了粗略区分,但它们不能反映多种半自然植被类型,而这些类型是高山环境中应加以区分的相关来源类型。因此,我们探索新兴技术,如eDNA追踪,可能会根据土地利用和覆盖来源来完善沉积物来源的信息。然后,我们将讨论具有挑战性的高山水文地貌环境,以及在这种背景下设计适当的沉积物示踪研究的意义。最后,展望了沉积物源指纹技术在地质灾害频发、土壤修复迫切需要的高山环境中的应用前景。关键词:高寒,环境DNA,侵蚀,滑坡,植被
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Strengths and limitations of sediment source fingerprinting in high mountain environments and relevance for soil restoration

High mountain environments are among the most sensitive on Earth. Due to anthropogenic disturbances and climate change, rates of regolith mobilization due to for example landsliding have been accelerating recently. As a result, soils degrade, geohazards occur and flash floods have negative consequences in downstream areas. The restoration of soils in high mountain environments and an improved understanding of nature-based solutions to land degradation is, therefore, urgent. As finding the origin of erosion sources is a first step to improve mitigation strategies and guide the implementation of effective soil restoration measures, we discuss sediment source fingerprinting research in the context of soil restoration in high mountain environments. A literature review was done based on articles that apply sediment source fingerprinting in high mountain environments and additional articles on land use-based markers and soil restoration were used to develop an outlook for future research. The application of sediment provenance studies in high mountains environments has been limited so far. While some studies yield a rough distinction between sediment sources based on environmental radionuclides or elemental geochemistry, they cannot reflect multiple semi-natural vegetation types which are relevant source types that should be discriminated in high mountain environments. Therefore, we explore emerging techniques such as eDNA tracing that could potentially refine the information on the provenance of sediment based on land use and cover sources. Then, we will address the challenging hydro-geomorphic environment of high mountains and the implications for designing properly a sediment tracing study in such a context. We will conclude by presenting an outlook to guide future applications of sediment source fingerprinting in high mountain environments, where geohazards are imminent and soil restoration is urgent.

Key words: alpine, environmental DNA, erosion, landslide, vegetation

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