PROVENANCE STUDIES OF KOREAN CELADONS OF THE KORYǑ PERIOD BY NEUTRON ACTIVATION ANALYSIS*

Neutron activation analyses of the body fabric of celadons from the main production sites of the Koryǒ period have shown differences in composition between kilns. Comparison of over 50 celadon objects in the collections of the British Museum with this data base from the production sites has permitted the assignment of over 40 of the pieces to their kiln of origin The majority show the trace element pattern of the Sadangri kilns, a smaller proportion are assigned to Yuchǒnri, while others are assigned to the kilns at Chinsanri (underglaze iron) and Kyǒngsǒ-dong (unglazed). A representative group of Chinese Yue wares arc clearly different from Koryǒ celadons in trace element composition.     

A SCIENTIFIC STUDY OF TRADITIONAL KOREAN CELADONS AND THEIR MODERN DEVELOPMENTS

Eighty sherds from nine different kiln sites representing a wide geographic distribution and a long time span of Korean celadon culture are analysed for macroscopic and compositional characteristics. Additionally chemical and mineral compositions of six unglazed sherds are compared with those of some modern raw materials. Unusually high values of alumina in the earliest Kangjin pieces of the middle ninth and early tenth century (I¹) could represent a significant technological innovation at the end of this period at this most important celadon production centre. Similarity in chemical and mineral compositions between unglazed sherds and some raw materials such as Kangjin clay and pottery stone show the possibility that many of the celadons were made from these types of raw materials as found in nature without additives and only after mechanical refining.     

唐、五代景德镇蓝田窑青瓷科技研究

随着2012年景德镇蓝田窑的发现和发掘,出土了大量的青釉瓷器。通过对窑址及出土陶瓷文物的整理与研究,专家提出蓝田窑是目前为止景德镇发现的早期烧制青瓷的窑址之一,其中出土的部分青瓷应为唐代时期烧造。因此,研究蓝田窑唐代和五代时期青瓷对探索景德镇早期青瓷的发展有着至关重要的作用。鉴于此,本研究以唐代和五代景德镇蓝田窑青瓷为研究对象,利用能量色散X射线荧光光谱分析仪、热膨胀仪等对24件唐、五代蓝田窑青瓷样品进行了测试,对比分析了唐代和五代景德镇蓝田窑青瓷的组成和工艺特征,为研究景德镇早期青瓷及其初步发展提供了一定的数据支撑。     

Inheritance relationship between Zhanggongxiang kiln celadon and Ru Guan celadon: Comments on the rationality of Raman Ip value evaluating firing temperature

The development of Chinese ceramics culminated during the Song dynasty. At this time, exquisite celadon works emerged, such as Ru Guan celadon and Southern Song dynasty official kiln celadon, which exhibited the glory of their era. Since the excavation of Zhanggongxiang kiln celadon in Ruzhou city, Henan province, China, it has been attracting widespread scholarly attention at home and abroad. Most scholars have suggested that Zhanggongxiang is the official kiln of the Northern Song dynasty. In this paper, taking the celadon unearthed from the Zhanggongxiang kiln as a sample, the combination of laser Raman spectrum and thermal expansion methods is used to study the inheritance relationship between Zhanggongxiang celadon and Ru Guan celadon in the firing process. Meanwhile, the rationality of using Raman I_p value to evaluate the firing temperature of ceramics is reviewed. The main conclusions are as follows. First, the firing temperature of Zhanggongxiang celadon with various glaze colours is quite different, whereas the firing temperature of the same glaze colour is similar, thereby inheriting the firing technology of Ru Guan porcelain. Second, the I_p value of glaze cannot evaluate the firing temperature of porcelain with similar firing temperature. The I_p value corresponds to a range, within which it does not fully conform to the rule that the larger the I_p value, the higher the firing temperature. The I_p value is also associated with the formulation in addition to firing temperature. It is applicable to evaluating porcelains with a similar formulation but a large temperature difference.     

A scientific study of Choson white ware: early porcelain from a royal kiln at Kwangju Usanni

Scientific study of kiln site no. 9 at Usanni, one of the earliest royal Kwangju kiln complexes in operation (from the early 15th to the early 16th century), shows that the technological expertise used to produce white ware was inherited from the celadon technology of the Koryo dynasty. The body material, of low Al₂O₃ and high SiO₂ content, is based on porcelain stone. Such a material, with almost no titanium and a low level of iron, was a rediscovery of the white ware material used earlier at the Sori kiln from the 9th century through to the 11th century. Ash continued to be one of the major ingredients of the glaze, and wares were fired in much the same way as the Koryo celadon, in kilns constructed of mud and rocks and in two steps. The Confucian philosophy and aesthetic of frugality and simplicity adopted from the Ming dynasty onwards by the new government acted as the catalyst for the successful ascent of the new technology.     

河南安阳灵芝窑出土瓷器的分析研究

本工作利用能量色散X-射线荧光光谱、体视及岩相显微镜、高温电子膨胀仪等实验方法,对灵芝窑有代表性的黑瓷、青瓷、白瓷等作了系统的分析测试。分析结果表明,灵芝窑不同种类的瓷器,在胎釉的化学组成、显微结构、烧制温度上等方面都存在一定的差异,由此推断,不同瓷器可能采用不同的原料及其加工工艺。     

汝州东沟窑金元时期青瓷与钧瓷原料和工艺特征的比较研究

金元时期在豫西中部地区多个窑址同时生产青瓷和钧瓷,发掘于2005年的汝州东沟窑遗址即是该类窑址典型代表之一。为系统了解东沟窑青瓷和钧瓷的胎釉元素组成特征和工艺特点、揭示两类瓷器各自随时代变化的规律,本项研究采用EDXRF和OM对东沟窑遗址出土且地层明确的43件金、元时期青瓷与钧瓷标本胎、釉化学组成和工艺性能进行测试分析,探讨了胎、釉的原料配比、釉层厚度和胎釉反应层厚度等工艺特征随时代和标本类型的变化规律。研究结果表明:东沟窑同时期青瓷和钧瓷胎体元素组成较接近,而两者釉的元素组成差异明显,金元钧瓷釉的SiO2/Al2O3摩尔比值都明显高于同时代青瓷的相应比值,呈现钧瓷釉典型的高硅低铝组成特征。从金代到元代,东沟窑青瓷和钧瓷釉都呈现从钙釉向钙-碱釉的转变。本项研究还观察到金元钧瓷的釉层和反应层厚度均高于同时代的青瓷;而从金过渡到元,两类瓷片的釉层和反应层厚度均趋厚。本项研究对揭示金元时期豫西中部地区青瓷和钧瓷间的传承和演化关系提供了有意义的科技数据。     

Tracing the origin of Chinese early white porcelain in the late sixth century—evidence from Xing kiln

As the criterion used by archaeologists for determining early white porcelain is quite ambiguous, the origin of Chinese white porcelain remains a point of disagreement. In this study, we systematically investigate 61 typical Xing porcelains of the late Northern dynasties to the early Sui dynasty (550–600 CE) using spectrophotometer, X-ray fluorescence (XRF), scanning electron microscopy (SEM), and X-ray powder diffraction (XRD), and analyze the differences between early white porcelain and celadon of Xing kiln in terms of their whiteness and raw materials characteristic. The results show that early white porcelain is a new type of ware that differs from celadon, which can be distinguished by whiteness, with a whiteness greater than 8% being early white porcelain and a whiteness less than 8% being celadon. It is assumed that the ancient potters created the whiter wares based on celadon by improving the glaze and selecting new raw materials for the body, but the production of this type of ware was short lived and subsequently refined in the Sui dynasty (581–618 CE) owing to the limited improvement in whiteness.     

Comparison of celadon from the Yaozhou and Xicun kilns in the Northern Song Dynasty of China by X-ray fluorescence and microscopy

The Xicun kiln is a typical kiln for firing porcelains for export, including celadon, which imitates the products of the Yaozhou kilns. In this paper, 10 pieces of celadon from the Xicun kiln and 8 celadon samples from the Yaozhou kiln were analysed in situ non-destructively by energy dispersive X-ray fluorescence microprobe and optical microscopy. The results indicated that the body of the Xicun celadon contained less TFe₂O₃, Cr, Sr and Zr, and more K₂O and Rb than that of the Yaozhou celadon. Also, the glaze of the Xicun celadon contained lower quantities of Sr and higher Rb; thus, these elements could be employed as relevant markers for the non-destructive discrimination of the provenance of Xicun celadon. In addition, the thicker glaze, the numerous bubbles, and the existence of the middle layer could be used as auxiliary indicators for a micro-structural distinction between samples from the Yaozhou kiln and those originating from Xicun.     

Study on the Material and Manufacturing Technology of Different Types of Longquan Ware Imitations from Dapu Kiln of Guangdong Province in the Ming Dynasty of China (ad 1368–1644)

Research on ancient Longquan wares and their imitations has attracted considerable attention. Using a series of experimental methods, including micro X‐ray fluorescence spectroscopy (μ‐XRF), X‐ray diffractometry (XRD), optical microscopy (OM), polarizing microscopy (PLM), dilatometry (DIL) and spectrophotometery, different samples of Longquan imitations from Dapu in Guangdong Province were collected and analysed. The study of different types of celadon from the Dapu kiln factories shows that the pale yellow body had a higher TFe₂O₃ content, and the body material must therefore have been treated differently or have come from a different source. The SiO₂ and Al₂O₃ contents in the body can be used as auxiliary parameters to identify Longquan wares and its imitations. The study also found that both kinds of glaze recipe—including calcium–alkali glaze and alkali–calcium glaze—existed in the Dapu products, which suggested that while imitating Longquan ware, the potters in Dapu also showed innovation in the recipe for the glaze material. Moreover, there were some differences in the TFe₂O₃ content, as well as the size, number and distribution of bubbles in the different types of glaze. Finally, the study revealed that the material of both the saggars and separators were composed of another porcelain clay, different from that of the celadon body. In addition, the white and compact body of the celadon had a higher firing temperature, of 1140–1187 °C, compared with other types of wares, which had a lower firing temperature of 1050–1080 °C.     

Compositional and Microstructural Study of KoryŎ Celadon and Whiteware Excavated from SŎRi Kiln in Kyŏnggi Province

An extensive study of the composition and microstructure of celadon and whiteware sherds excavated at Sori, one of the most important sites that were active during the founding stage of the stoneware and porcelain industry in Korea, was carried out. The analysed sherds were organized according to four different levels of the excavation and four different styles of haemurigup foot rim. Principal component analysis of the chemical compositions of the sherds revealed slight differences in their body and glaze compositions between the levels of excavation. Porcelain stone with high silica and low aluminium contents was generally used as the body material and wood ash as the chief flux in the glaze. Over the period of operation, the aluminium content in the bodies of the ceramics decreased and the P₂O₅ content in the glazes increased. Glazed bodies were fired in a single step, in contrast to the two‐step method used in later ceramic production. Firing conditions were adjusted to produce vitrification of the glazes, which meant that vitrification of the ceramic bodies occurred to varying extents, mostly determined by the relative contents of flux in the body and the glaze.     

Elemental Characterization by EDXRF of Imperial Longquan Celadon Porcelain Excavated from Fengdongyan Kiln,Dayao County

A mass of Longquan porcelain shards carved with ‘Guan’ or the dragon patterns were unearthed in the early Ming Dynasty layer of the Fengdongyan kiln site at Dayao County. These celadon shards were fired in the Hongwu and Yongle eras of the Ming Dynasty. In order to research the raw materials and firing technology of the imperial porcelain, 85 typical shards were analysed by energy‐dispersive X‐ray fluorescence (EDXRF). The results indicate that the contents of TiO₂ and Fe₂O₃ in the body vary in the Hongwu and Yongle eras. Compared with Longquan glazes in the Southern Song Dynasty, the average values of K₂O, Fe₂O₃ and TiO₂ are higher, but that of CaO is lower in early Ming imperial porcelain glazes. Principal components analysis (PCA) shows that different degrees of elutriation of the same raw materials are the main reason for this difference in the Hongwu and Yongle periods. However, the raw materials of imperial porcelain glazes show no obvious changes and have inherited the earlier tradition. The production and firing technology of imperial porcelain reached a higher level and had not declined in the Early Ming Dynasty.     

New light on early caprine herding strategies from isotope analysis: a case study from Neolithic Anatolia

The measurement of stable carbon (δ¹³C) and nitrogen (δ¹⁵N) isotopes of caprine bone collagen from the Neolithic sites of Çatalhöyük and Aşıklı Höyük in south-central Anatolia have allowed examination of exploitation and herding practices of sheep and goats. The isotope values from protodomestic caprines at Aşıklı Höyük suggests that these animals were consuming very similar foods to each other and were all confined to the same or similar environments with no access to C₄ plants. At Çatalhöyük, the results show how the caprine management strategy develops from the strategy seen at Aşıklı Höyük into a more varied practice at an early stage as the site grows with an increasing dietary contribution obtained from C₄ plants. No change in diet is isotopically discernible at Aşıklı Höyük. Interestingly, no distinction could be made between the diets of sheep and goats at either site. Therefore, such studies are a useful method of examining the development of early herding or management strategies of caprines in the Near East.     

The World's Oldest Stone Artefacts from Gona, Ethiopia: Their Implications for Understanding Stone Technology and Patterns of Human Evolution Between 2·6–1·5 Million Years Ago

The systematic archaeological and geological survey and excavations at Gona between 1992–1994 led to the discovery of well-flaked stone artefacts which are currently the oldest known from anywhere in the world. More than 3000 surface and excavated artefacts were recovered at 15 localities documented east and west of the Kada Gona river. Based on radioisotopic dating (⁴⁰Ar/³⁹Ar) and magnetostratigraphy, the artefacts are dated between 2·6–2·5 million years ago (Ma). EG10 and EG12 from East Gona are the most informative with the highest density, providing the best opportunity for characterizing the oldest assemblages and for understanding the stone working capability of the earliest tool makers. Slightly younger artefact occurrences dated to 2·4–2·3 Ma are known from Hadar and Omo in Ethiopia, and from Lokalalei in Kenya. Cut-marked bones dated to 2·5 Ma from Bouri in Ethiopia are now providing important clues on the function of these artefacts. In addition, Australopithecus garhi known from contemporary deposits at Bouri may be the best candidate responsible for the oldest artefacts. Surprisingly, the makers of the Gona artefacts had a sophisticated understanding of stone fracture mechanics and control similar to what is observed for Oldowan assemblages dated between 2·0–1·5 Ma. This observation was corroborated by the recent archaeological discoveries made at Lokalalei. Because of the similarities seen in the techniques of artefact manufacture during the Late Pliocene–Early Pleistocene, it is argued here that the stone assemblages dated between 2·6–1·5 Ma group into the Oldowan Industry. The similarity and simplicity of the artefacts from this time interval suggests a technological stasis in the Oldowan.     

RAW MATERIALS OF GLASS FROM AMARNA AND IMPLICATIONS FOR THE ORIGINS OF EGYPTIAN GLASS*

Analysis has been conducted on 19 blue glasses from Amarna in Middle Egypt dated to around 1350 BC. The results suggest that these glasses fall into two distinct types: cobalt coloured glasses with a natron based alkali made from local Egyptian materials, and copper coloured glasses with a plant ash alkali, which follow a Mesopotamian tradition of glass making. It is suggested that at least some of this copper/plant ash glass is imported into Egypt during the Amarna period despite extensive local production of cobalt/natron glass. Existing analyses (Lilyquist and Brill 1995) of the earliest glass from the reign of Tuthmosis III (c. 1450 BC) suggest that during this period the same two types of glass are present. Local Egyptian cobalt and natron in these early glasses implies that, despite the lack of archaeological evidence for production sites, glass was produced from its raw materials in Egypt as early as the reign of Tuthmosis III.     

用微探针型EDXRF技术研究南宋官窑瓷片的化学组成及其含义

本文报道了用ENGLE-Ⅱ微探针能量色散型X荧光光谱（EDXRF）技术测定一批青瓷残片中的16种元素氧化物的含量．其残片来自浙江杭州地区南宋的郊坛窑和老虎洞窑。由主量元素判别方程。值表明,郊坛和老虎洞青釉瓷均属官窑制品,与龙泉民窑产品有很大差别。从主成分统计分析看出．郊坛下官窑与老虎洞官窑的瓷釉成分有明显不同,但其胎质成分的分布却有部分的重叠。这显示两类同属官窑的制品,其釉料可有不同的矿物组合。但胎料有时会交流使用。从釉层、中间层、和胎层的Al2O3和CaO的含量变化数据表明,郊坛下官窑和老虎洞官窑的青瓷制品有厚度分别为120-140um和230-240μm的中间层,反映出烧造工艺上有一定的差别。化学成分鉴定证实了考古工作者认为老虎洞窑实为史书记载的修内司官窑的观点．     

GOVERNMENT AND THE CANADIAN URBAN SYSTEM: INCOME TAX,TRANSFER PAYMENTS,AND EMPLOYMENT

The impact of government on the Canadian urban system is explored using Revenue Canada data from personal income tax returns. Variations in taxes and in certain forms of government expenditure among urban places are linked with city size, economic base, per capita income, and rate of growth. It is found that many locations are heavily dependent on the public sector and that, overall, government programmes redistribute income toward smaller and less prosperous places. The most significant effect, however, is the stabilization of local economies by means of a large and relatively constant public sector. L'impact du gouvernement sur le système urbain canadien est étudié en utilisant des données de Revenu Canada qui proviennent des déclarations d'impǒt sur le revenu des particuliers. Les variations de taxes et de certains types de dépenses publiques parmi les régions urbaines sont associés avec les variables de taille urbaine, base économique, revenu per capita, et taux de croissance. Il est démontré que plusieurs régions sont fortement dépendantes du secteur public et que, globalement, les programmes gouvernementaux redistribuent le revenue vers les régions les plus petites et les moins prospères. Mais l'effet le plus significatif est celui de la stabilisation des économies locales par le biais d'un large et relativement constant secteur public.     

Radiocarbon Chronology of the Siberian Paleolithic

We have compiled 462 C-14 determinations for 120 Paleolithic and Mesolithic sites from Siberia and the Russian Far East. The Mousterian sites are dated to ca. 46,000–28,500 BP. The Middle–Upper Paleolithic transition dates to ca. 43,300–28,500 BP. Although there are a few earlier sites, most of the Upper Paleolithic sites are dated to the time interval between ca. 34,000 BP and 10,000 BP. The earlier Upper Paleolithic stage is characterized by macroblade technology and is radiocarbon-dated to ca. 34,000–20,000 BP. The earliest microblade technology occurs in the late stage of the Upper Paleolithic, dated to ca. 23,000–20,000 BP, but the majority of microblade sites is dated to ca. 20,000–11,000 BP. The Final Paleolithic (Mesolithic) sites date to ca. 12,000–6000 BP. At ca. 13,000–11,000 BP, the earliest Neolithic appeared in both the Russian Far East (Amur River basin) and the Transbaikal. The Paleolithic–Neolithic transition occurred ca. 13,000–6000 BP.     

Upper Paleolithic raw material economies at Üçağızlı cave, Turkey

This paper addresses variation in lithic raw material economy within the early Upper Paleolithic at Üçağızlı cave (south-central Turkey). The stratigraphic sequence documents some 12,000 years of the early Upper Paleolithic, entailing changes in lithic technology, raw material exploitation, and game use. Although the same lithic raw materials were exploited throughout the sequence to make quite similar ranges of products, there are marked changes in the ways raw materials from different source areas were treated, including patterns of transport and raw material consumption. The concept of technological provisioning is used to understand changing strategies for procuring and managing supplies of flint from different source locations. Shifts in raw material economy are argued to represent responses to changes in residential mobility and the scale/duration of occupations at the cave itself: data on cultural features and foraging strategies provide independent evidence for these shifts in land use. Results have implications for more nuanced approaches to investigating of lithic raw material economies and the significance of “raw material transfers.”     

PROCESSUS D'EDIFICATION DE LA STRUCTURE DE POUSSÉE DU GLACIER THOMPSON, ÎLE AXEL HEIBERG, TERRITOIRES DU NORD-OUEST

Les photographies aériennes du complexe glaciaire formé par les glaciers White et Thompson (ǐle Axel Heiberg, Territoires du Nord-Ouest) acquises au cours des 30 dernières années indiquent que la structure de poussée qui se forme au front du glacier Thompson s'est élargie dans sa zone centrale ainsi que dans sa portion ouest, mais qu'elle a été comprimée dans sa portion est. Les observations sur le terrain confirment le caractère contemporain du développement asymétrique de la structure vers le sud-ouest, caractere qui a été propose dans une étude antérieure. Les observations effectuées en 1989 et en 1990 permettent ?affirmer que la structure ?empilement de blocs de graviers fluvioglaciaires qui forme ce que ?aucuns appellent la « moraine de poussée » du glacier Thompson ne résulte pas principalement de poussées horizontals de surface ni ?un dépǒt de strates de glace basale riche en materiel au front du glacier par écoulement compressif, mais plutǒt ?un ensemble de processus de nature glaciotectonique. On propose enfin un modèle de développement de la structure après avoir passé en revue les fondements théoriques de ?édification des structures de poussée en milieu gla-ciaire. The aerial photograph record depicting the proglacial area of the White and Thompson glaciers, Axel Heiberg Island, Northwest Territories, shows that the width of the Thompson Glacier push structure has increased in its western and central sectors, but has decreased in its easternmost sector over the last 30 years. The push structure, which is often referred to as a ‘push moraine’, is mainly composed of stacked up slabs of outwash material resulting from glaciotectonic activity. Recent observations were found to reinforce the asymmetric development trend of the structure toward the southwest that had been noted in an earlier study. Field observations in 1989 and 1990 also suggest that a set of processes related to glaciotectonism, rather than simple bulldozing or deposition of material-laden slabs of basal ice at the front, is mainly responsible for changes in the Thompson Glacier push structure. Theoretical aspects are discussed and a model relating to formative processes in the Thompson Glacier push structure is proposed.