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Identification of ancient human activity using multi-element analysis of soils at a Medieval harbor site in Masuda City, Shimane Prefecture, Japan

机译:使用日本岛根县增田市中世纪港口遗址的土壤多元素分析方法识别古代人类活动

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A large-scale Medieval harbor site has recently been discovered at Nakazu Higashihara in Masuda City, Shimane Prefecture, Japan. Archaeological information indicates that the maritime trade network at this site was on an East Asian scale. The concentrations of 22 elements in 40 soil samples from the archaeological floor horizon and overlying topsoils in the Trench NKZ were determined by X-ray fluorescence spectroscopy, in order to identify the geochemical signatures due to human activity in the harbor site. The results show that chemical feature of soils from the archaeological floor was influenced by ancient anthropogenic activities, while that of the topsoil samples were not. Significant differences in chemical feature of soils occur between areas of differing activity. Strong relationships exist between As, Pb, Cu, Br, TS (total sulfur), MnO and P_2O_5 concentrations in the fire pit and charcoal area, and between Cr, Sr, Sc, F, I, TS, CaO, MnO and P_2O_5 in a building pillar area. Soils from an area of ancient metallurgical activity (blacksmithing) showed strong correlations between As, Pb, Zn, Cu, V, Sc, MnO, Fe_2O_3* and P_2O_5. Those elements can be potential discriminators in this Medieval harbor archaeological site. In contrast, Y, Nb, Zr, Th and TiO_2 are not key elements archaeologically, and are mainly of natural origin. However, these elements are useful for identify the element sources and their origins. Cross-plots against TiO_2 clearly illustrate that Zn, Cu, and P_2O_5 are significantly enriched above detrital background levels in the fire pit and charcoal area, as are As and Pb in the blacksmith area. Those from the building pillar area lie on background trends, and hence anthropogenic activity in that did not greatly affect soil chemistry.
机译:最近在日本岛根县益田市的中原东原发现了一个大型的中世纪港口。考古信息表明,此地点的海上贸易网络处于东亚范围。通过X射线荧光光谱法测定了Trench NKZ上的考古地面层和上层表土中40个土壤样品中22种元素的浓度,以鉴定由于人类活动引起的地球化学特征。结果表明,古代人为活动影响了考古层土壤的化学特征,而表层土壤样品的化学特征不受影响。不同活动区域之间的土壤化学特征存在显着差异。火坑和木炭区的As,Pb,Cu,Br,TS(总硫),MnO和P_2O_5浓度之间,以及Cr,Sr,Sc,F,I,TS,CaO,MnO和P_2O_5之间存在密切关系。建筑支柱区域。古代冶金活动(锻造)区域的土壤显示As,Pb,Zn,Cu,V,Sc,MnO,Fe_2O_3 *和P_2O_5之间具有很强的相关性。这些元素可能是这个中世纪港口考古遗址中的潜在区分因素。相比之下,Y,Nb,Zr,Th和TiO_2并不是考古学上的关键元素,主要是天然来源的。但是,这些元素对于标识元素来源及其来源很有用。针对TiO_2的交叉图清楚地表明,火坑和木炭区域中的Zn,Cu和P_2O_5显着高于碎屑本底水平,铁匠区域的As和Pb也是如此。来自建筑支柱地区的那些生物具有背景趋势,因此其中的人为活动并未对土壤化学产生很大影响。

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