首页> 外文期刊>Journal of Archaeological Science >Geochemistry of sauceboats excavated from Independence National Historical Park (Philadelphia): evidence for a Bonnin and Morris (c. 1770e73) provenance and implications for the development of nascent American porcelain wares
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Geochemistry of sauceboats excavated from Independence National Historical Park (Philadelphia): evidence for a Bonnin and Morris (c. 1770e73) provenance and implications for the development of nascent American porcelain wares

机译:从国家独立历史公园(费城)出土的酱汁船的地球化学:波恩和莫里斯(c。1770e73)出处的证据及其对新生美国瓷器发展的影响

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Porcelain sauceboats excavated from a privy with a late 18th century (1786 or later) context at IndependenceNational Historical Park (INHP) are anomalously Al-rich compared with previously analysed Anglo-American sulphurous phosphatic wares. Apart from their S content, they are most similar to phosphatic Wm Reid porcelain (Brownlow Hill, Liverpool, c. 1755e67, and its branch at Shelton, Staffordshire) in terms of their major element constituents, but they contain heavy minerals (e.g., TiO_2 polymorphs) and in this regard resemble a dated (1773) silicious-aluminous-calcic (S-A-C) Bonnin and Morris porcelain (Philadelphia) openwork porcelain basket. In terms of morphology and composition, some TiO_2 polymorphs in the 1773 basket match those from clay from White Clay Creek, Delaware, a resource reputedly exploited by Bonnin and Morris. Their high Nb/Cr ratios indicate derivation from a metapelitic (or granitic pegmatite) source. So too do some from the INHP sauceboats, although others are chrome-rich (w1% Cr_2O_3), indicating a mafic source. The bedrock beneath White Clay Creek includes metasediments, granitic pegmatite, and metabasites (e.g., of the Wissahickon Formation), pointing to a local source for the TiO_2 polymorphs in the porcelains described here. Although the evidence for a Bonnin and Morris provenance for the INHP sauceboats is circumstantial, their enrichment in heavy minerals, unusual e perhaps experimental e compositions, and aesthetic characteristics nonetheless suggest a Philadelphia origin for these artifacts. The compositions of 18th century Philadelphia porcelain support the contention that knowledge of phosphatic and S-A-C pastes originating in London was transferred first to Staffordshire and Liverpool, and then to Philadelphia, perhaps via a potter by the name of Wm Ball.
机译:与先前分析的英美硫磷产品相比,在独立国家历史公园(INHP)处发现的具有18世纪晚期(1786年或更晚)环境的私人所开的瓷碟船富含铝。除了其S含量外,就主要元素成分而言,它们与磷酸盐Wm Reid瓷(布朗霍山,利物浦,约1755e67,及其在斯塔福德郡谢尔顿的分支)最相似,但它们含有重矿物(例如TiO_2多形体),在这方面类似于过时的(1773)硅质铝钙(SAC)波宁和莫里斯瓷(费城)镂空瓷篮。在形态和组成方面,1773篮子中的一些TiO_2多晶型物与特拉华州White Clay Creek的粘土中的那些相匹配,Bonnin和Morris认为这是一种资源。它们的高Nb / Cr比值表明其来自变质岩(或花岗岩伟晶岩)来源。 INHP调味船也是如此,尽管其他一些富含铬(w1%Cr_2O_3),表明镁铁质来源。 White Clay Creek下的基岩包括变质沉积物,花岗伟晶岩和变质岩(例如Wissahickon组),指向此处描述的TiO_2多晶型物的本地来源。尽管关于INHP酱汁船的波恩和莫里斯出处的证据是间接的,但它们富含重矿物质,不寻常的也许是实验性的成分以及美学特征仍然暗示了这些人工制品的费城起源。 18世纪费城瓷器的成分支持这样一种论点,即起源于伦敦的磷酸盐和S-A-C糊状物的知识首先转移到了斯塔福德郡和利物浦,然后又转移到了费城,也许是通过一个名为Wm Ball的陶工。

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