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首页> 外文期刊>Journal of Archaeological Science >In situ shallow subsurface reflectance spectroscopy of archaeological soils and features: a case-study of two Native American settlement sites in Kansas
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In situ shallow subsurface reflectance spectroscopy of archaeological soils and features: a case-study of two Native American settlement sites in Kansas

机译:考古土壤和特征的原位浅层地下反射光谱:以堪萨斯州的两个美国原住民定居点为例

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摘要

The results of in situ shallow subsurface reflectance spectroscopy surveys at two late 18th e 19th century Native American sites in Kansas contribute to a growing literature on the chemical characterization of anthropogenic features at archaeological sites. Near infrared and visible diffuse reflectance spectroscopy of known sub-soil features (hearths, storage pits, earthlodge walls, living surfaces, and defensive palisades) yielded characteristic signatures distinguishable from background spectra of adjacent locations. The spectra, obtained by insertion of a reflectance probe into the ground to depths up to 1 m at a series of locations, are further correlated with: electrical resistivity and magnetic gradiometry surveys; electrical conductivity and insertion force (soil compaction) contour plots; organic carbon, phosphorus, magnesium, and calcium spectra from analysis of core samples; and archaeological features recorded via excavation. The close spatial correlation of the spectroscopic data with known archaeological features supplements traditional topographic, surface, and subsurface geophysical survey methods by providing chemical information about ancient features and activity areas. The in situ recording of data has significant advantages over laboratory-based analyses.
机译:在堪萨斯州18世纪至19世纪末的两个美国原住民遗址进行的原位浅层地下反射光谱学调查的结果,为有关考古遗址中人为特征的化学表征的文献的发展做出了贡献。已知地下土壤特征(炉膛,储藏坑,土方墙,活动表面和防御性栅栏)的近红外和可见漫反射光谱法产生了可与相邻位置的背景光谱区分开的特征特征。通过在一系列位置将反射探头插入地面深达1 m所获得的光谱进一步与以下各项相关:电阻率和磁梯度测量;电导率和插入力(土壤压实)轮廓图;核心样品分析得到的有机碳,磷,镁和钙光谱;以及通过发掘记录的考古特征。光谱数据与已知考古特征的紧密空间相关性通过提供有关古代特征和活动区域的化学信息,补充了传统的地形,地表和地下地球物理勘测方法。与基于实验室的分析相比,数据的原位记录具有明显的优势。

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