3.1 Weathering effects of ancient glass
Table 4 shows the chemical results of natural surface and polishing surface for some typical samples by EDXRF. The results show that weathering can cause the levels of contents for the glass matrix vary and has a significant impact on quantitative analysis. the chemical compositions of the weathered layer are different from that of the inner part. the levels of Na2O and the K2O for polishing surface are much higher than that of weathered surface. The Al2O3 content is slightly higher, while the CaO content become slightly lower after weathering in potash glass. SEAG-031 is a special sample with a high level of PbO. As the degree of weathering increases, the PbO content of SEAG-031 increases while the K2O content decreases. (Liu et al. 2011; Dong et al. 2012) The quantitative analysis results of trace elements Rb, Sr, and Zr are relatively less affected by weathering.
In order to accurately judge the glass systems of those glass Jue samples, this article comprehensively evaluates the contents of Na2O, MgO, Al2O3, CaO, K2O and trace elements Rb, Sr.
3.2 Glass types
The chemical compositions of 44 glass Jue were analyzed by EDXRF and the results are shown in Table 5. Based on the contents of Na2O, MgO, Al2O3, K2O, CaO and trace elements Rb, Sr, Zr in the glass matrix, the glass samples analyzed in this article are divided into three types: potash glass, soda-alumina glass, and potash-lead glass.
Potash glass is the most in samples. Except for SEAG-031 and SEAG-036, the other 42 glass samples are all potash glass (Dussubieux 2021; Li et al. 2019). The major constituent of 42 potash glass Jue is SiO2, and the content range is 66.96%~88.16%. The secondary component is K2O. Except for SEAG-004, SEAG-009, SEAG-012, the mass fractions of K2O in other potash glass Jue are all more than 10%. The K2O and Na2O contents of SEAG-004, SEAG-009 and SEAG-012 are still low after polishing because of the thick weathered layer. And since the mass fraction of K2O is higher than the content of Na2O and trace elements, it can be preliminarily inferred that they are potash glass.
According to the mass fractions of Al2O3 and CaO in 42 potash glasses and the contents of trace elements Rb and Sr (Liu et al. 2013) (Fig. 2 and Fig. 3), it can be seen that they are divided into two subgroups: the one group with high Al2O3 content and high Rb/Sr is m-K2O-Al2O3-SiO2 glass (m-K-Al), a total of 38 pieces; the other group with similar mass fractions of Al2O3 and CaO and low Rb/Sr is m-K2O-CaO-Al2O3-SiO2 glass (m-K-Ca-Al), with a total of 4 pieces. Figure 4 shows the ratio of TiO2/Al2O3 and Al2O3/SiO2 of glass Jue samples. The m-K-Al glasses are significantly centralized.
SEAG-036 is a mineral alkali soda-alumina glass (m-Na-Al) (Dussubieux and Walder 2022). The mass fraction of Na2O in SEAG-036 is 16.56%, which suggests that Na2O was used as the flux in this glass Jue. The Al2O3 mass fraction is 5.84% and the MgO mass fraction is 0.89%.
The SEAG-031 can be classed to the potash-lead glass (Liu et al. 2019). As shown in Table 5, only one sample, SEAG-031, was found to have high level content of PbO. SEAG-031 has a thick weathered layer on the surface, which can be divided into white and brown areas. The white areas are easy to form white powder. It can be seen from Table 4 that the brown part of the surface of SEAG-031 has the highest mass fraction of CaO and PbO, and the lowest mass fraction of SiO2. The white area is suspected to be formed after the brown weathered layer falls off. Compared with the brown weathered layer, the mass fraction of SiO2 is higher, and the mass fraction of CaO and PbO is lower. Removing the white weathered layer on the surface and analyzing its interior, it was found that the mass fraction of K2O increased to 10.20% and the mass fraction of PbO decreased to 37.12%.
3.3 Glass-making techniques
The internal physical structure characteristics of glassware, including the morphology and distribution characteristics of inclusion particles, opacifier crystals, bubbles, etc., as well as the surface micro-morphology characteristics of glassware, have important indicative significance for the glass-making techniques. Based on the obtained internal physical structure characteristics and surface morphology characteristics of the objects, it is considered that there are three processing techniques used for those glass Jue samples: drawing, casting and cold-working.
The first technique method is drawing. Figure 5 shows the OM images and two-dimensional OCT images of SEAG-001, SEAG-002, and SEAG-003. It is obvious that the elongated large bubbles can be observed, and the long axis direction is parallel to the ring edge. It can be inferred that the drawing-process is used to draw the glass into Jue shape while it is hot formed.
Casting can make Jue of various shapes. The Jue with rectangular or trapezoidal section is almost made by casting. The casting method is to inject the molten glass into the mold and then mold it, so there will also be internal bubbles in the shape of long strips under pressure. Some of the samples are rough, with a lot of bubbles inside and pits on the surface. These pits are also bubbles formed when the surface is cooled. Figure 6 shows the OM images and two-dimensional OCT image of SEAG-004. A large number of bubbles and pits on the surface can be observed.
Cold-working techniques are applied to most of Jue samples. The processing of those Jue can be divided into two steps. The first step is the casting, and then the glasses are made into the shape of Jue through cold-working, such as polishing, cutting and drilling. The typical one is SEAG-016 (Fig. 7). SEAG-016 has a small number of elliptical bubbles inside and a smooth surface. And its gap section is very flat, even like being cut by a knife. It is likely to process the gap by cutting. The weathered white spots and flat surface also indicate that the surface may have been polished. And the same cutting and polishing process is also used for other Jue, including the Jue of ‘type 7’ and some of ‘type 8’ (listed in Table 3).
In terms of glass-coloring process, except for SEAG-031, the colors of glass samples are blue, green, or blue-green. From the perspective of coloring characteristics, most potash glasses are colored by iron ions and copper ions, a few are mainly colored by iron ions, and some samples also contain a small amount of tin. The mineral alkali soda-alumina glass SEAG-036 is mainly colored by iron ions. And the white-yellow opaque potash-lead glass SEAG-031 is mainly colored by lead and tin. Raman spectroscopy testing was conducted on the yellow crystal on the surface of SEAG-031, and strong characteristic peaks were obtained near 134cm-1 and 266cm-1 (Fig. 8), which is basically consistent with the Raman peak of lead tin yellow (PbSn1-xSixO3/PbSnO3) (Zhao 2014; Wang et al. 2001). During the processing of SEAG-031, lead stannate may have been added as an opacifier and colorant.
3.4 Possible provenance of glass Jue
Potash glass is one of the most widely distributed ancient glasses in Asia. Potash glass uses K2O as a flux and is divided into three subgroups: low lime-high alumina-potash glass (m-K2O-CaO-SiO2 glass/m-K-Ca), low alumina-high lime-potash glass (m-K2O-Al2O3-SiO2 glass/m-K-Al) and a moderate lime and alumina-potash glass (m-K2O-CaO-Al2O3-SiO2 glass/m-K-Ca-Al) (Liu et al. 2013; Dussubieux and Walder 2022). In this study, there are thirty-eight m-K2O-Al2O3-SiO2 glasses and four m-K2O-CaO-Al2O3-SiO2 glasses. The subgroup of m-K-Al has been found in the Dong Son Culture site in Vietnam, Khao Sam Kaeo in Thailand, northern Myanmar, and Guangxi in China. It is generally believed that there may be potash glass producing or making centers in India (north and south), Southeast Asia and the surrounding areas of Jiaozhi County in Han Dynasty China (Lankton and Dussubieux 2013; Li et al. 2019). Potash glass appeared from the 4th century BCE to the 5th century CE, and its number began to decline sharply in the 3rd century CE, which seems to be replaced by soda-high alumina glass (Li et al. 2019). The m-K-Ca-Al and m-K-Al glass Jue analyzed in this paper may be made in Southeast Asia. The producing center was most probably in the Jiaozhi County(交趾郡) and its adjacent areas during Han Dynasty of China.
The mineral soda-high alumina or m-Na-Al glass is one of the most abundant glass types found in Southeast Asia and South Asia. This is a soda glass with high alumina concentrations (>5%). Its high concentration in India convinced Brill (1987) that this glass had been manufactured there (Dussubieux 2021). There are least 12 sub-groups of the mineral soda-alumina glass, namely m-Na-Al 1 to 12(Dussubieux and Walder 2022). The m-Na-Al 1 glass is the most abundant glass in South India and Sri Lanka from the 4th century BCE to the 11th century CE. Giribawa in northwestern Sri Lanka is an important glass-working place of m-Na-Al 1 glass. Some sites in Southern India and Mantai in Sri Lanka may have also been the glass-making places. The m-Na-Al 3 glass probably produced in northern India (Dussubieux 2021). And other known types of m-Na-Al glass appeared later than 9th century CE and will not be discussed here. SEAG-036 belongs to the m-Na-Al glass (may be m-Na-Al 1 glass), of which the raw materials may come from South Asia, and then enter Southeast Asia for secondary processing.
The sample SEAG-031 is a traditional type of Jue in China. Its internal PbO mass fraction is 37.12% and K2O mass fraction is 10.20%. There are some potash-lead glass beads with similar mineral composition excavateded from the Han tombs in Guangdong and Guangxi (Liu et al. 2019). During the Han Dynasty, Pb-Ba glass prevailed in China, while potash glass was produced in Guangdong and Guangxi provinces in the south China (Gan et al. 2016). SEAG-031 was probably produced in Jiaozhou province (交州刺史部) including jiaozhi, Jiuzhen, Hepu and Rinan of the Han Dynasty.