探地雷达作为改善湿地遗产管理的工具

C. Bunting, N. Branch, S. Robinson, P. Johnes
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引用次数: 4

摘要

湿地是一种不可再生资源,具有很高的有机考古沉积和古环境序列潜力。这一资源正受到发展和气候变化的威胁。在西北欧已确定的湿地中,只有一小部分对其深度、地层结构和遗产资产进行了研究。这项研究的重点是提高对如何使用探地雷达来解决这个问题的理解。数据是从已知与考古遗迹有关的湿地收集的。地质考古和地球化学分析钻孔验证了探地雷达结果。结果表明,探地雷达可以在一定范围的湿地沉积物中获得有意义的结果。深度取决于沉积物类型,含水量和水化学,使用200MHz天线在泥炭中清晰成像80ns (2.5m),在富含粘土的沉积物中大大减少。考古遗迹和建筑是可探测的。鉴定和绘制当地地层单位也成为可能,这对在景观和沉积环境中确定考古遗址很重要。通过对钻孔的收集和分析,大大提高了探地雷达测量的解释能力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Ground penetrating radar as a tool to improve heritage management of wetlands
Wetlands are a non-renewable resource of high potential for organic archaeological deposits and palaeoenvironmental sequences. This resource is at threat from development and climate change. Only a small percentage of the identified wetlands in North West Europe have been studied with regard to their depth, stratigraphic architecture and the heritage assets they contain. The focus of this research is to improve understanding of how GPR can be used to tackle this problem. Data has been collected from wetland sites known to be associated with archaeological remains. The GPR results have been validated by boreholes subjected to geoarchaeological and geochemical analysis. The results show that GPR can obtain meaningful results in a range of wetland sediments. The depth is limited depending on the sediment type, water content and water chemistry with a depth of 80ns (2.5m) imaged clearly in fen peat using a 200MHz antenna greatly reduced in clay rich sediments. Archaeological monuments and structures are detectable. Identification and mapping of local stratigraphic units important for setting archaeological sites in a landscape and sedimentary context has also been possible. Interpretation of GPR surveys is greatly improved with the collection and analysis of boreholes.
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