罗马诺拉剧院(意大利撒丁岛南部)砂浆中使用的地质材料的矿物学、岩石学和化学分析

S. Columbu, A. Garau
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引用次数: 28

摘要

对诺拉剧院(公元一世纪)的古代砂浆和混凝土中使用的原材料的成分和来源进行了分析,以确定它们的来源和罗马时期的建筑技术。在砂浆的粘结剂/骨料混合物中使用的土工材料根据其在不同部门(即结构墙,法庭拱顶,外部壁龛墙,洞穴层的基础,舞台内壁)的功能而有所不同,也根据剧院或工作步骤的不同施工阶段而有所不同。具有结构功能的砂浆主要是水工砂浆(如拱顶混凝土、洞房的接缝和基础砂浆),石灰砂浆主要用于抹灰,很少用作层理砂浆。根据Vitruvius的建议,在水力砂浆中主要使用火山岩,作为粗粒和细粒火山灰砾石(pulvis puteolanus)和石英-长石砂(以晶体碎屑的形式存在,比例几乎恒定,分别为2:1左右)。cocciopesto异常罕见或不存在。在砂浆中还使用了局部英灰质火山岩,特别是在混凝土中用作水泥。灰黑色火山岩为玻璃质,其特征更接近黑曜岩,而不太接近罗马时期通常使用的天然火山灰。为了确定这些玻璃的来源,利用XRF和SEM-EDS / WDS分析,对从战场迫击炮和一些可能的撒丁岛来源地区的火山露头样品进行了地球化学比较。为了验证火山灰的质量(通过其与粘合剂的化学反应),用SEM-EDS显微探针分析了火山玻璃的边缘和内部,用XRPD和TG/DSC方法分别分析了粘合剂的组成特征和水力程度。使用这种没有当地起源的火山灰玻璃是一种新奇的东西,因为在诺拉考古遗址的迫击炮中从未发现过这种玻璃。鉴于撒丁岛黑曜石在新石器时代或石器时代广泛用于生产工具和仪器,对其使用、起源和贸易进行了一些考虑。
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Mineralogical, petrographic and chemical analysis of geomaterials used in the mortars of Roman Nora theatre (south Sardinia, Italy)
The composition and the origin of raw materials used in the ancient mortars and concrete of the Nora theatre (first century AD) have been analysed to define their provenance and construction technologies of the Roman period.The use of geomaterials in the binder / aggregate mixtures of the mortars vary according to their function in the different sectors (i.e., structure-wall, tribunalia vaults, wall of external niches, foundation of cavea tiers, stage inner wall) but also according to different construction phases of the theatre or the work-steps. The mortars with structural function are mainly hydraulic (e.g., concrete of vaults, jointing and foundation mortars of cavea ashlars), while the lime mortars were used mainly for plasters, and rarely as bedding mortars. As recommended by Vitruvius, in the hydraulic mortars were mainly used volcanic rocks, as coarse and fine pozzolanic aggregate (pulvis puteolanus), and quartz-feldspar sands (present as crystal-clasts with an almost constant ratio of about 2:1, respectively). The cocciopesto is anomalously rare or absent. In the mortars local dacitic volcanic rock were also used, especially in the concrete as caementia.The grey-black volcanic rocks are glasses with characteristics more near to obsidian and less to natural pozzolan normally used in the Roman period. To identify the provenance of these glasses, a geochemical comparison between the samples taken from the theatre mortars and the volcanic outcrops of some probable Sardinian source areas is made by XRF and SEM-EDS / WDS analysis.To verify the quality of the pozzolan (by its chemical reaction with the binder), the edges and inside of volcanic glasses were analysed with an SEM-EDS microprobe, while the compositional characteristics and the hydraulic degree of the binder was analysed with XRPD and TG/DSC methods, respectively.The use of this kind of pozzolanic glass, without local origins, is a novelty because it has never been found in the mortars of the archaeological site of Nora. Given the wide use of Sardinian obsidian in the Neolithic or Calcolithic periods for production of tools and instruments, some considerations about its use, origin and trade are made.
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