特制绢地书画作品修复——以清代莫晋绢本书法立轴为例

特制绢地书画作品的修复历来是一大难题,因困于材料的特殊性与稀缺性,如寻觅不到同类补绢,就较难实现理想的修复效果。清代莫晋绢本书法立轴的画心材质为一种经过涂布、染色、描绘等工艺制成的特制绢本,因保存不当,画心已出现严重断裂残缺、部分涂层填料脱落等劣化现象,亟需修复保护。但画心用绢的质地和颜色特殊,无法找到与之接近的补绢。本次修复通过对绢的表面涂层进行检测分析,并参阅传统纸张再加工材料的检测报告和研究文献,再结合对材料的老化实验等,确定将瓷土和高岭土按一定比例混合来代替原涂层中的铅白作为本次修复的涂布材料。最后通过对修补涂层的全色,取得较为理想的修复效果。     

Lead isotope analysis as a new method for identifying material culture belonging to the Vázquez de Coronado expedition

Archaeological evidence has become an increasingly important component of efforts to identify the route of the Francisco Vázquez de Coronado expedition through northern Mexico and the southwestern United States (1540-1542). Here, we report the first high-precision lead isotopic measurements of artifacts from two archaeological sites with strong material evidence for the expedition’s presence: Piedras Marcadas Pueblo in New Mexico and the Jimmy Owens Site in Texas. The analysis of lead and copper armaments from both sites reveals that many artifacts have overlapping or extremely similar isotopic ratios. We propose that the narrow range of lead isotopic ratios measured on these artifacts can be interpreted as a geochemical fingerprint for some of the Coronado expedition’s surviving material culture, and provides evidence that we interpret to suggest the expedition derived lead and copper metal from Mexican sources. Such a geochemical fingerprint presents an empirical method for discriminating between artifacts that belonged to the Coronado expedition and those related to subsequent Spanish, historical, or modern activity in the Southwest U.S. Thus, this method could significantly impact the search for and identification of archaeological sites associated with the Coronado expedition.     

青铜器铅同位素指示意义的范铸实验研究

铅同位素比值作为探索青铜器产地和矿料来源的指示剂而被广泛采用,为论证这种方法的可行性,进行了仿古范铸实验。测试分析表明,长江中、下游出土古铜锭含铅量大多在1％以下,样品中添加铅的含量远高于铜、锡料所带入的微量铅。结果证明,青铜器铅同位素的指示意义是不确定的,并且在冶铸过程中可能存在铅同位素的分馏。     

A truly refractory crucible from fourth millennium Tepe Hissar, Northeast Iran

From the Early Chalcolithic to the Late Iron Age, melting and smelting crucibles were usually made from non-refractory ceramic fabrics, which required heating of the charge from within the crucible to avoid collapsing the ceramic itself. In this paper, an unusual melting crucible from Northeast Iran, radiocarbon-dated to the Late Chalcolithic (ca. 3600 BCE), will be presented that significantly changes our understanding of the development of technical ceramics in Southwest Asia. This crucible, made of a highly refractory talc-based ceramic held together by an outer layer of traditional non-refractory ceramic, is to our knowledge unprecedented at such an early date. As will be argued, this ancient crucible was heated from the exterior or from below and not from the interior. This method of firing, combined with the highly-specialized construction technique, makes this crucible so far unique in prehistoric metallurgy, and forces us to re-examine traditional models for the development of technical ceramics and metallurgical practices in the Old World.     

在硫代硫酸钠—醋酸铅双组分体系中黄铜器表面着色的动力学研究

通过调整流代硫酸钠一醋酸铅双组分试液的不同浓度比以及控制着色温度、试液酸度和着色时间,确定黄铜试样表面着以不同颜色的条件。用x射线衍射方法测定不同颜色表面膜的成分,并对膜形成的动力学进行了探讨．为研究黄铜着色提供了一种新的方法。     

海昏侯墓出土马蹄金、麟趾金内嵌物的分析研究

南昌西汉海昏侯墓发掘出土了数量较多的马蹄金,为汉代黄金货币的研究工作提供了宝贵资料,出土马蹄金内均存在镶嵌物,大部分腐蚀严重。结合偏光显微分析、背散射扫描电镜\能谱、红外光谱、X射线衍射光谱对海昏侯墓主棺头箱出土的部分马蹄金内嵌物进行分析研究,依据分析结果将马蹄金内嵌物分为透闪石软玉、蛋白石、铅钡玻璃和疑似高铅玻璃4种类型。其中,铅钡玻璃基本保留玻璃态,腐蚀产物随着埋藏环境的变化存在二次结晶现象,腐蚀的最终产物是碳酸铅;疑似高铅玻璃表现出完全不同的腐蚀状态,外层硅质成分较高形成较为致密的壳状结构,内部碳酸铅以葡萄状填充在少量的硅质成分中。研究结果可为后续的保护处理与马蹄金、麟趾金的复制工作提供理论支持。     

Historical signature of Roman mining activities in the Bidasoa estuary (Basque Country,northern Spain): an integrated micropalaeontological,geochemical and archaeological approach

This work presents an integrated micropalaeontological (foraminiferal content), geochemical (Pb, Zn, Cu, Ni, Cr, and Al, Pb isotope ratios, radiocarbon dating) and archaeological approach to the environmental impact caused by Roman mining in the Bidasoa estuary (northern Spain). Sediments collected in the ancient Roman port of Irun represent a typical infilling sequence, reflecting a progressive isolation from the estuarine environment. They exhibit elevated contents of Pb, clearly higher than those recommended nowadays for acceptable sediment quality. Isotope composition confirms exploitation of local galenas as the main source for this metal. Results from a borehole (25 m long) reveal that Pb pollution extended also to the adjacent estuarine area. The beginning of Roman mining activities is recorded by a marked increase in Pb concentrations. However, the maximum value appears later in time (after 660 cal AD). Although this enrichment could be related to the reworking upstreams of previously polluted materials, recently obtained archaeological data suggest that episodes of historically non-documented mining activities could have taken place in the surrounding area after Roman times.     

The impact of mining activities on the environment reflected by pollen,charcoal and geochemical analyses

This article presents results of a multi-proxy study of a fen deposit in the former mining district of Falkenstein near Schwaz in the Tyrol, Austria. The aim of the study in the framework of the special research program HiMAT (The History of Mining Activities in the Tyrol and Adjacent Areas – Impact on Environment & Human Societies) was to disclose the ecological impact of mining in pollen and heavy metal diagrams and to create a model combining the changes in palaeoecological proxies with historical evidences for mining. The application of this palaeoecological–historical model to prehistoric times allowed us to reconstruct the impact of mining and metallurgic activities in the surroundings of the fen during the last millennia. The results of stratigraphy, radiocarbon dating, LOI, pollen and micro-charcoal analyses as well as geochemical analyses of scandium, lead and lead isotopes validated by historical and archaeological data are hereby presented.     

MEDIEVAL SILVER PRODUCTION AROUND SIJILMÂSA,MOROCCO

Sijilmâsa (south-east Morocco) was one of the most strategic cities in a far-reaching exchange network, that is, the Trans-Saharan trade, linking the Maghreb with West Africa during the medieval period (from the 8^th to the 15^th century CE). It was also one of the most important gold and silver monetary workshops at the time. If gold came from West Africa, we know from written sources that silver was produced in Morocco, although archaeological evidence of silver mining and smelting has remained elusive. Thanks to a thorough analysis of the lead isotopic data from silver mining districts in Morocco and from ores and slags of our study, we were able to refine the tracing of our materials and provide tangible evidence of medieval mining in the close hinterland of Sijilmâsa city.     

Pb and Sr Isotopes and the Provenance of the Painting Materials of Cornelius Krieghoff in 19th‐Century Canada

Radiogenic lead and strontium isotope data are presented for lead‐ and calcium carbonate/barium sulphate‐containing paint and ground samples from 15 paintings, executed between 1844 and 1871, by 19th‐century Canadian artist Cornelius Krieghoff. Like many artists of this era, Krieghoff used lead‐based pigments such as lead white, chrome yellow and Naples yellow, and extenders such as calcium carbonate and barium sulphate. The lead isotope analyses of the majority of these pigments are consistent with the isotopic compositions of lead mined from European lead deposits in England and/or Germany. However, three samples from Krieghoff's early career yield lead isotope compositions that are much more radiogenic than European sources. The lead isotope compositions of these three samples are consistent with the addition of a more radiogenic lead component that is similar to the lead derived from North American lead deposits in Missouri and Illinois (Mississippi Valley Pb–Zn type deposits). The strontium isotope compositions of the extenders suggest that the raw materials for calcium carbonate or barium sulphate extenders were largely derived from Palaeozoic to modern‐day marine environments. This study shows that pigments manufactured from North American lead were being incorporated into Canadian paintings as early as 1844.