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The ceramic artifacts in archaeological black earth (terra preta) from Lower Amazon Region, Brazil: chemistry and geochemical evolution

机译:巴西下亚马逊地区的考古黑土(terra preta)中的陶瓷人工制品:化学和地球化学演化

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This paper carried out a chemical investigation of archaeological ceramic artifacts found in archaeological sites with Black Earth (ABE) in the Lower Amazon Region at Cachoeira-Porteira, State of Pará, Brazil. The ceramic artifacts, mostly of daily use, belong to Konduri culture (from 900 to 400 years BP). They are constituted of SiO2, Al2O3, Fe2O3, Na2O and P2O5; SiO2 and Al2O3 together add up to 80 % and indicate influence of acid rocks, transformed into clay minerals basically kaolinite. The relative high contents of P2O5 (2.37 % in average) come out as (Al,Fe)-phosphate, an uncommon fact in primitive red ceramics, but found in some roman and egyptian archaeological sites. The contents of the trace elements are similar or below the Earth's crust average. This chemical composition (except P2O5) detaches saprolite material derived acid igneous rocks or sedimentary ones as the main raw material of the ceramics. The contents of K, Na and Ca represent the feldspars and rock fragments possibly introduced into saprolitic groundmass, indicated by mineralogical studies. The presence of cauixi and cariapé as well as quartz sand was confirmed by optical microscope, SEM analyses and by the high silica contents of ceramic fragments. Phosphorus was possibly incorporated into groundmass during cooking of foods, and ABE soil profile formation developed on yellow Latosols. The raw materials and its tempers (cauixi, or cariapé, feldspar, crushed rocks, old ceramic artifacts and quartz fragments) are found close to the sites and therefore and certainly came from them.
机译:本文对在巴西帕拉州Cachoeira-Porteira的下亚马逊地区的黑土(ABE)考古遗址中发现的考古陶瓷文物进行了化学调查。这些陶瓷制品大多属于日常使用,属于Konduri文化(从BP到900到400年)。它们由SiO 2,Al 2 O 3,Fe 2 O 3,Na 2 O和P 2 O 5组成。 SiO2和Al2O3的总和达到80%,并表明了酸性岩石的影响,基本上转变成粘土矿物,主要是高岭石。 P2O5相对较高的含量(平均2.37%)以(Al,Fe)-磷酸盐的形式出现,这在原始的红色陶瓷中并不常见,但在一些罗马和埃及的考古遗址中发现。痕量元素的含量相似或低于地壳平均含量。这种化学成分(P2O5除外)可分离出腐泥土材料,它们是由酸性火成岩或沉积岩作为陶瓷的主要原料。矿物学研究表明,钾,钠和钙的含量代表可能引入腐泥质岩体中的长石和岩石碎片。通过光学显微镜,SEM分析和陶瓷碎片的高二氧化硅含量证实了Cauixi和Cariapé以及石英砂的存在。食物烹饪过程中磷可能掺入了地面物质中,黄色Latosols上形成了ABE土壤剖面。原材料及其回火(cauixi或cariapé,长石,碎石,旧陶瓷制品和石英碎片)被发现在这些地点附近,因此肯定来自它们。

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