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首页> 外文期刊>Journal of Archaeological Method and Theory >The Ben Lawers Historic Landscape Project: Simultaneous Multi-element Analysis of Former Settlement and Arable Soils by X-ray Fluorescence Spectrometry
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The Ben Lawers Historic Landscape Project: Simultaneous Multi-element Analysis of Former Settlement and Arable Soils by X-ray Fluorescence Spectrometry

机译:Ben Lawers历史景观项目:通过X射线荧光光谱法同时分析前居民区和耕地的多元素

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X-ray fluorescence spectrometry (XRFS) was used in the analysis of A horizon soil samples collected from a former farming settlement and its associated area of infield (i.e. arable) located in the Central Highlands of Scotland. To date, XRFS has not been extensively used in geoarchaeological research, but in our study the simultaneous multi-element capabilities of this instrumental technique allowed the total concentrations of 25 major, minor, and trace elements to be fully quantified with acceptable levels of accuracy and precision. Included within this group of chemical elements are a number (e.g. Ba, Ca, P, Pb, Sr and Zn) that have proved to be of value to archaeological interpretation in earlier investigations undertaken in Scotland. In our preliminary work documented here, significant differences were found between the A horizon soils of former settlement and infield areas for 18 chemical elements. Subjecting the XRFS data—and three other measured variables: soil organic carbon (SOC), pH and A horizon depth—to discriminant analysis indicates that soils of former settlement and arable farming can be effectively classified according to their pH, SOC content and Ca, Cu, Mg, Rb, and Zn concentrations. The inference is that areas of former infield and settlement elsewhere at this study location in the Central Highlands may be able to be identified according to their soil chemical composition and use of discriminant function, even though the surface remains of pre-eighteenth century settlement sites are not readily evident today because they were constructed of perishable materials.
机译:X射线荧光光谱法(XRFS)用于分析从苏格兰前高地的一个前农业定居点及其相关的内地(即耕地)区域收集的A地平线土壤样品。迄今为止,XRFS尚未在地质考古研究中广泛使用,但是在我们的研究中,这种仪器技术的同时多元素功能允许对25种主要,次要和痕量元素的总浓度进行充分定量,并达到可接受的准确度和精确。这组化学元素中包括许多元素(例如Ba,Ca,P,Pb,Sr和Zn),这些元素在苏格兰较早的研究中对考古解释具有重要意义。在我们这里记录的初步工作中,在前定居点的A层土壤与内场区域的18种化学元素之间发现了显着差异。对XRFS数据和其他三个测量变量:土壤有机碳(SOC),pH和地平线深度进行判别分析,结果表明,可以根据其pH,SOC含量和Ca, Cu,Mg,Rb和Zn浓度。推论是,即使在18世纪以前的聚落地点的表面仍然存在,也可以根据它们在土壤中的化学成分和判别功能的使用来确定中高地本研究地点内野和聚居地的区域。由于它们是由易腐烂的材料制成的,因此今天还不太明显。

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