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Degradation of emerald green: scientific studies on multi-polychrome Vairocana Statue in Dazu Rock Carvings, Chongqing, China

Abstract

The spontaneous degradation of pigments in painting may occur depending on environment, especially the surrounding condition of high humidity and soluble salts. Even some of these are well studied, more investigations are still in need for heritage science. Paint cross sections from Vairocana Statue in Dazu Rock Carvings, one of World Cultural Heritage, Chongqing, China are studied by optical microscopy (OM), Raman spectroscopy (Raman) and mapping, and scanning electron microscopy coupled with energy dispersive X-ray analysis (SEM–EDS). Ultramarine blue, emerald green, synthetic atacamite, vermilion, red lead, gold foil, orpiment, cerussite, gypsum and barite are identified as pigments. Moreover, lavendulan (NaCaCu5(AsO4)4Cl·5H2O) and mimetite (Pb5(AsO4)3Cl) are degradation products of emerald green (Cu(C2H3O2)2·3Cu(AsO2)2) and cerussite(PbCO3) originally used as green pigment with mixture. These secondary products are formed via multistep progresses as degradation of emerald green and cerussite, oxidation of arsenite ((AsO2)), migration of arsenate ((AsO4)3−) and precipitation reaction of these ions with other necessary ions from environmental conditions. Based on the pigment and paint layer stratigraphy analysis, the paintings of the statue have been executed at least four times and the most recent may be after 1850s. The formation of lavendulan give rise to a highlight for identification of green copper-arsenic containing pigments and characterization of degradation in complex conditions.

Introduction

Degradation phenomena occur in the paintings where original pigments, binding media, ground layer and substrate to undergo chemical and physical transformations, leading to discolouration or deterioration of materials. These processes can be initiated by internal factors, for example the characteristics of pigments with organic binders and other materials, or by external factors, which suffer from environmental conditions (relative humidity, illumination, temperature, etc.), biological activity, pollution or human interventions, or several of these together [1, 2]. Degradation of pigments can be visually perceived as color changes or confirmed as structural modifications by employing modern analytical or micro-analytical methods.

Studies on degradation processes and products of pigments inside museum on oil paintings, manuscripts and in an outdoor environment on polychrome statue and wall paintings are well known and documented. Azurite (2CuCO3·Cu(OH)2) and malachite (CuCO3·Cu(OH)2), as the best representatives of basic copper salts (carbonates, chlorides, sulphates, etc.), are widely used as mineral blue and green pigments. In the case of artifacts, the published data indicates the transformation of azurite and malachite into green basic Cu chlorides in the presence of chloride and humidity [3,4,5]. Arsenic-based pigments such as orpiment (As2S3) and realgar (As4S4) are highly appreciated in China for yellow and red to red–orange tones. Arsenic sulfide pigments are bound to shift color exposed to visible light and realgar undergoes photo-induced polymorphism and becomes friable, assuming hues from bright yellow pararealgar (As4S4) to colorless arsenolite (As2O3) whereas the photo-oxidation of orpiment results in arsenolite [6,7,8]. Lead pigments e.g. lead white (2PbCO3·Pb(OH)2), red lead (Pb3O4) are employed owing to bright colors and high covering power in paintings. Lead pigments turn black caused by reaction with sulphur-containing compounds to black galena (PbS) and oxidation to the black-brown plattnerite (PbO2) [9, 10]. Vermillion (HgS) is extensively used as bright red pigment. It darkens attributed to the formation of a black compound, metacinnabar (β-HgS) when exposed to light and HgCl2 when Cl ions present in the pigments [11, 12].

A popular man-made brilliant green pigment, emerald green (Cu(C2H3O2)2·3Cu(AsO2)2), containing copper and arsenic is found to be unstable in paints. Emerald green darkens as it mixed with sulphur-containing compounds from the atmosphere to form brown copper sulfides (CuS) [13]. Emerald green degrades in oil paintings rich with a relatively high concentration of monoacids, diacids and resin acids, forming copper soaps (4Cu(FA)2) (FA = fatty acids) and arsenic trioxide (As2O3), leading to transparent discolored brown layers [14]. Emerald green is also found to transform to mineral lammerite (Cu3(AsO4)2) in wall paintings as a result of the migration of arsenic [15]. Recently, rare lead arsenate mineral, mimetite (Pb5(AsO4)3Cl), is shown to be degradation product of multistep alteration pathway of pigments orpiment and realgar and arsenate ions ((AsO4)3−) to precipitate with Pb2+ ions [16,17,18].

Lavendulan (NaCaCu5(AsO4)4Cl·5H2O), an uncommon copper arsenate mineral, was originally described by Breithaupt in 1837 from Annaberg. It was first found by Vogel in 1853 at Joachimsthal, and then by Goldsmith in 1877 from San Juan, Chile [19]. The identification of lavendulan specimen is confirmed by single crystal X-ray diffraction techniques [20]. Raman spectroscopy has also reliable performance to characterise lavendulan, and infrared spectra reported [21]. This mineral was found as alteration products in ancient slag heaps and used for colourant effects in cosmetics of ancient Egyptians [21]. The discovery of lavendulan in Chinese painting is seldom reported. It is detected in the wall painting of Cave 11 of Yungang Grotto (云冈石窟), Shanxi Province and colored drawing on timber structure of Kumbum Monastery (塔尔寺), Qinghai Province [22]. Lavendulan is also found in paint layers of statues from Anyue Grotto (安岳石窟), Sichuan Province [23]. We find lavendulan on paintings of Maidservant figures in the Saint Mother’s Hall of Jinci Temple (晋祠), Shanxi Province. In these papers, it is still unclear that lavendulan may be formed by the degradations of other pigments containing Cu and As.

Naturally, taking physical and chemical conditions of their usage and storage into account, pigments in wall paintings and polychrome statues are much more subjected to the environment, even in complex conditions including high humidity or dissolved salts. Even some of these are well studied above, more tracking and new investigations are still needed and crucial for the conservation field.

In 2016, China’s National Cultural Heritage Administration launched a large-scale perseveration demonstration projects for the Buddhism Grottoes in Sichuan Province and Chongqing Municipality. At that time, a subproject aiming to conserve and restore the Niche of Sakyamuni Entering Nirvana Statue in Great Buddha Bend (Dafowan, 大佛湾) and Polychrome Statues in Little Buddha Bend (Xiaofowan, 小佛湾) at Dazu Rock Carvings (大足石刻) was undertaken by the Chinese Academy of Cultural Heritage. Located outdoors in a long time, the statues have been inevitably suffering from surface weathering, water seepage, rock instabilities, biological erosion, salt corrosion, etc., so the scientific investigation and conservation is becoming urgent. The first step is to investigate the characteristics of the paintings on caved sandstone surface for determining the appropriate intervention treatment. Therefore, the polychrome statue Vairocana Statue in Little Buddha Bend at Dazu Rock Carvings of Chongqing municipality was chosen as a demonstration example.

In this study, a coupling of Raman spectrum and mapping, OM, and SEM–EDS have been applied to identify the composition of original pigments and signs of their degradation in cross sections of color layers from paintings of polychrome statue Vairocana Statue. The information obtained can accelerate a better understanding of the transformation processes which affect the history and stability of paints. Material identification of layer stratigraphy can confirm the date of paintings executed.

Materials and methods

Materials

Outstanding as the pinnacle of Chinese cave temple art from the 9th to 13th centuries, Dazu Rock Carvings were listed as World Cultural Heritage by UNESCO in 1999. The sites located in Dazu District, Chongqing, China, are comprised of the cliffside carvings at Baodingshan, Beishan, Nanshan, Shizhuanshan and Shimenshan. Dazu Rock Carvings are remarkable for their aesthetic quality, their rich diversity of subject matter, both secular and religious, and the light that they shed on everyday life in China during this period. They provide outstanding evidence of the harmonious synthesis of Buddhism, Taoism and Confucianism [24].

The culmination of carvings is found on Mount Baoding, consisting of two groups from the late 12th to the mid 13th century, namely, Great Buddha Bend and Little Buddha Bend.

The Vairocana Buddha Statue (measuring 1.92 × 1.57 m) is the Lord Buddha of whole Little Buddha Bend statues. The paintings have been re-painted several times observed by naked eyes and seriously damaged. For examples, they are seen as the numerous colour losses, cracking and crumbling of the pictorial layer. Some paintings become powder-like substances. Dust is deposited on the paint surface, and the cracked areas easily gather the dust from the environment. Sixteen micro samples including blue, green, red, gilding, black and white color are collected from the painting of this statue (Fig. 1).

Fig. 1
figure1

Vairocana Buddha in the Little Buddha Bend at Dazu Rock Carvings. The sample location for (1–4) blue, (5–8) green, (9–12) red, (13–14) gold, (15) black, and (16) white pigments on the painting

Methods

Paint sample preparation

Sixteen samples, including different paint layer and ground layer, are collected alongside damages. Sample locations are illustrated in Fig. 1. All the samples are mounted as cross section (CS). For cross section preparation, the minute pigments are embedded in epoxy resin (Buehler Epo Thin) and polished with dry abrasive papers down to 0.5 μm to obtain sufficiently polished surface. Each layers of these samples are analyzed by Optical microscope (OM), micro-Raman spectroscopy (Raman) and scanning electron microscopy coupled with energy dispersive X-ray spectrometry (SEM–EDS).

Cross section sample analysis

The samples are observed using a Leica 4000 M optical microscope.

A Horiba Jobin–Yvon Xplora spectrometer coupled with 100× objective of an Olympus BX-41 microscope is employed for identification of pigments in each painting layers. The 532 nm green and 785 nm red laser is used and the spectra is recorded with a resolution of 2 cm−1. The spectra of pigment particles are representative and chosen from at least three different points. Moreover, identifying green pigments, a 532 nm laser is used and the power is reduced using 1% filter, to avoid the thermal photodecomposition. The exposure time is 10 s with 20 accumulation.

The cross section samples are coated with carbon and studied under a TESCAN VEGA3 scanning electron microscope, equipped with Bruker XFlash 610M energy dispersive X-ray at an accelerating voltage of 20 kV.

Results and discussion

Paint layers

The structure and materials of the Vairocana Statue are very complex, including sandstone substrate, gilding and paintings. The components of non-degraded sandstones of the rock carving are feldspar, quartz, plagioclase, calcite, and a small amount of clay [25]. OM and SEM results of multi-layered paint CS1, CS5, CS10, CS11, CS13 and CS16 show delamination phenomena in the paintings, the visible layers are numbered 1–7 or 8 from the surface to base layer in Fig. 2. Table 1 summarizes multi-paint stratigraphy and layer composition of these samples examined by Raman and EDS.

Fig. 2
figure2

OM and BSE images of cross section samples revealing paint stratigraphy. Perceived surface colors of samples: CS1 blue, CS5 green, CS10 red, CS11 red, CS13 gold, CS16 white

Table 1 Layer stratigraphy and components of cross sections in Fig. 2

OM and BSE images of single-layered paint CS2–4, CS6–8, CS9, CS12, CS14 and CS15 are reported in Additional file 1: Figure S1. Two layers of these ten samples are distinguished along the paint surface to base layer: paint layer close to ground layer. The ground layer is composed of gypsum (CaSO4·2H2O), calcite (CaCO3), quartz (SiO2) analyzed by Raman and clay by SEM–EDS as the presence of elements e.g. Na, Mg, Al, Si, S, Ca and Fe consistent with XRD analysis results [26]. Blue pigment of CS2–4 is mainly identified as ultramarine blue (Na8[Al6Si6O24]Sn). Green layer of CS6–8 is mixture of lavendulan, mimetite, cerussite (PbCO3), barite (BaSO4), whewellite (CaC2O4·H2O) and gypsum. Red layer of CS9 and CS12 is composed of vermilion, and black layer of CS 15 contains carbon (C).

For CS13, the ground layer used to bond gold layer are defined as the base layer close to the sandstone substrate. This layer could be subdivided into three sub-layers, corresponding to red layer 2, black layer 3 and gray layer 4 in Fig. 2 CS13. The layer is composed of organic binding media and inorganic materials. The binding media is confirmed as a mixture with Chinese lacquer by using infrared spectrometry (IR) and tung oil by gas chromatography–mass spectrometry (GC/MS) [27]. Vermilion is added into the binding media in red layer to high the gold gloss. Black-gray lacquer layer mixed with quartz and clay aim to smooth the adhered surface of sandstone.

Green copper arsenite pigments

To highlight the representativeness of the results, four green pigment samples of CS5, CS6, CS7 and CS8 are selected. These samples cover the important units of green pigment usage in the statue. For each sample, Raman analysis focused on the green layer to identify the components.

The spectra taken from CS5 are shown in Fig. 3, the positions and the vibrational assignments of the main bands listed in Table 2. The characteristic bands of emerald green particles are detected at 154, 175, 217, 242, 294, 325, 371, 429, 492, 539 and 950 cm−1 (Fig. 3a). The feature assigned to the acetate group is evident at 950 cm−1 corresponding to C–C stretching, and low wavenumber is due to the arsenite moiety [28]. The spectra exhibit the characteristic bands belonging of lavendulan located at 178, 226, 278, 342, 410, 544, 853 cm−1 (Fig. 3b). The spectra consists of ν1 (AsO4) at 854, ν2 at 345 and ν4 at 545 cm−1 [21]. The As-containing phases in green layer are mimetite and cerussite. The mimetite is indicated by a strong band corresponding to ν1 modes of AsO4 at 813 cm−1 (Fig. 3c) and cerussite by a strong band corresponding to ν1 modes of CO at 1054 cm−1 (Fig. 3c, d) in the Raman spectra [29]. The main characteristic bands of whewellite are observed at 1464 with a second band at 1491 cm−1 assigned to the CO stretching mode and 897 cm−1 to the C–C stretching mode (Fig. 3d) [30]. Raman signal also display the occurrence of gypsum and baryte (Fig. 3c, d).

Fig. 3
figure3

Raman spectra from green layer of CS5: ad show characteristic peaks for emerald green, lavendulan, mimetite, baryte, cerussite; whewellite and gypsum. Black reference spectrums from RRUFF open database

Table 2 Main Raman characteristic bands for phases of CS5 green layer

All four cross sections show that green layer is mainly composed of lavendulan, together with mimetite, cerussite, gypsum, barite and whewellite. A small quantity of emerald green particles are present only in the lower part (layer 2, Fig. 2 CS5) of green layer. Apart from lavendulan and emerald green, no other copper-arsenic containing pigments are detected in these cross sections.

The finding of lavendulan and mimetite is of an exceptional importance. Especially, there is a complete lack of historical evidence of lavendulan used as pigment. The crucial question is whether the lavendulan represents an intentionally used pigment or a secondary phase formed by degradation of other Cu–As-containing pigments, such as emerald green.

To explore this issue, CS5 is carefully selected from the previously mentioned green samples, hope to obtain accurate information regarding the morphology and distribution of the residual emerald green and lavendulan particles.

Further observations with OM and SEM–BSE for CS5 show the upper part (layer 1 in Fig. 4a) of the green layer losing the green coloration hue comparing with the lower part (layer 2 in Fig. 4a) caused by the absence of emerald green. The lavendulan particles show single plates radiating from center to edges with a diameter of ~ 10 μm and spherulites formed by the plates overlapping or intersecting at the center in Fig. 4b, c. Although lavendulan particles occur with color of pale blue (Fig. 4b), their general crystal habit and structure is consistent with that of emerald green [13]. Nevertheless, the natural lavendulan forms bright blue crusts, spherules and thin rectangular platelets which are flexible and have a low Mohs hardness (2.5) and excellent cleavage parallel to the platy face [20]. These results suggest that lavendulan is a degradation product of emerald green. The elemental maps of the green layer corresponding to BSE image (Fig. 4d) show the distribution of copper, arsenic, sodium, calcium and chlorine (Fig. 4e–i). The arsenic is not confined to the green particles, and migrates throughout the whole green layer, while the copper distribution is limited to particles. This is similar to observation of the migration of arsenic from the arsenic-containing pigments to paint layers [31, 32]. Furthermore, the absence of arsenic in the blue, gold, red and black samples and paints excludes the possibility of arsenic introduced from the surrounding environment to the green paint. An explanation for the presence of arsenic in the green layer could be deriving from degraded emerald green. The distributions of Na, Ca and Cl in green layer also suggest these elements introduced from the surrounding environment and then react with Cu and As to form lavendulan.

Fig. 4
figure4

Green layer (layer 1 and layer 2, Fig. 2 CS5): a optical microscopic image of green layer, b optical microscopic image of particles show the loss of green coloration of emerald green degraded into lavendulan, c SEM–BSE image of lavendulan particles, d SEM–BSE image of green layer, and elemental maps of e copper, f arsenic, g sodium, h calcium and i chlorine show that arsenic migrated out the particle and diffusion within the whole green layers while the occurrence of copper is limited within green particles

Based on the preliminary OM and Raman results, the residual emerald green particles are identified in small quantities at the lower part (layer 2, Fig. 2 CS5) of green layer. A representative subarea is selected and analyzed by using Raman mapping. Distributions of crystalline phases of this area show more details in Fig. 5. Emerald green is confirmed as green pigment and surround by cerussite as shown in Fig. 5a, b. Next to emerald green (point 1), distributions of lavendulan (point 2, 3 and 4) are quite different (see Fig. 5c). Mimetite is found in the vicinity of green particles and shows a higher abundance in the areas around lavendulan particles (especially point 3) than that around emerald green (see Fig. 5d). These results suggest arsenic derived from the degraded emerald green particles must have reacted with cerussite to form mimetite as secondary products.

Fig. 5
figure5

Raman mapping of a sub area (see rectangle) in the lower part of CS5 green layer: a emerald green and b cerussite, assumed to be originally present in green layer; c lavendulan and d mimetite as to secondary minerals, formed in situ

Green copper hydroxychloride pigments

Regarding the green layer of CS16, layer structure and composition are investigated by Raman, OM and SEM–EDS.

Raman analysis (Fig. 6) shows the existence of atacamite and malachite in the green layer (layer 6, Fig. 2 CS16). The positions and the vibrational assignments of the main bands for atacamite are listed in Table 3. The presence of atacamite can be concluded from Raman characteristic bands in the range of 145–972 cm−1 and 3328–3433 cm−1 which coincide with the published literature [33], three intense bands at the identical positions are observed at 972, 902 and 818 cm−1, the bands between 800 and 1000 cm−1 attributed to Cu–OH and OH bends; the intense band occurs at 511 cm−1, the bands below 600 cm−1 assigned to O–Cu–O and Cl–Cu–Cl modes; three bands at 3328, 3349 and 3433 cm−1 assigned to OH stretches.

Fig. 6
figure6

Raman spectra from green layer of CS16: a atacamite and b malachite. Black reference spectra from RRUFF open database

Table 3 Main Raman characteristic bands for atacamite of CS16 green layer

Figure 7a, b and c mainly show that numerous atacamite particles appear as aggregates or masses, while malachite particles sporadically occur in the layer. The synthetic atacamite particles are found to be spherical with dark spots in the center under the PLM [34, 35]. Figure 7b–d and g reveal nearly spherical particles, typical for synthetic atacamite. Malachite could be obtained as a by-product of preparation of synthetic atacamite. Artificial copper trihydroxychlorides could be the most popular green pigments for wall painting and architecture from North Dynasty (386–581 CE) until late Qing Dynasty (1840–1911 CE) [36]. In addition, the element maps of chlorine associated with copper (Fig. 7e, f, h, i) show delamination phenomena in the green layer is invisible, suggesting the green layer was painted only one time other than repainted using the two kinds of green pigments.

Fig. 7
figure7

Microscopic images of green layer (layer 6 in Fig. 2f) of CS16: a OM, b SEM–BSE, c BSE image enlarged rectangle 1 in g, atacamite obviously seen with black arrows and malachite with white arrows, d BSE image (see rectangle 1 in b) and elemental maps of e copper and f chlorine, g BSE image (see rectangle 2 in b) and elemental maps of h copper and i chlorine show the occurrence of malachite (white arrows)

Discussion on dating

Emerald green is a brilliant green pigment first synthesized by Willem Sattler in 1814. Emerald green particles exist in a great variety of crystalline assemblages that are organized as agglomerates of crystal platelets in the form of rosettes or spherulites [13]. It was widely used in China as watercolor in pith paper works and in scroll paintings from the 1850s onwards [37]. Ultramarine blue shows rounded anisotropic particles of homogeneous sizes (≈ 2 μm), suggesting the artificial origin of lapis lazuli [38] are used in the out layer of the painted statues. Artificial ultramarine blue was invented by Guimet in 1828 and its commercial production evolved soon after 1830 [39]. Then ultramarine blue was introduced from Europe into China in late Qing Dynasty (1840–1912 CE), and the importation lasted until 1927 when Chinese chemists Dai A and Ling Z synthesized this pigment [40].

The statues in the Little Buddha Bend at Dazu Rock Carving were excavated during the Southern Song Dynasty (1127–1279 CE) [41]. Religious paintings in China usually undergo heavy repairs and even re-painting in different period. As the layer stratigraphy shown (Fig. 2), for more than 800 years so far, the Vairocana Buddha statue has been painted at least four times. Concerning these documents above, the most recent painting of the statue may be executed after late 1850s, based on the date of the wide use of emerald green.

Because the date of the invention and wide use in China of emerald green and ultramarine blue were nearing, they appeared co-localized in Chinese paintings. In addition, consistent with the recent literature on this topic [16,17,18], the rare nature of mimetite minerals strongly suggests that they are secondary products. Once more this information suggests emerald green was used as original pigment other than lavendulan (secondary products).

Degradation progress of emerald green

The Vairocana Buddha statue locates in the Holy Longevity Sites, where the air circulation is poor because of the semi-closed building structure. Relative humidity in the Dazu Rock Carvings is very high and can reach above 85% from July to September, even oversaturated to form condensation water with pH scale at 6 on the surface of statues [42]. When exposed to such conditions, degradation phenomena of pigments can occur, namely transformation from emerald green to lavendulan in the paint surface. It can be explained as follows:

The degradation of emerald green can occur under acidic conditions provided by the environment [15]. Emerald green (Cu(C2H3O2)2·3Cu(AsO2)2) can release acetic acid (CH3COOH) together with arsenite (HAsO2) and copper ions (Cu2+) in the slightly acidic environment (Eq. 1). In the next step, the arsenite ions ((AsO2)) are oxidized to arsenate ions ((AsO4)3−) (Eq. 2) [14, 43]. The chemical transformation to the arsenate from arsenite clearly is an oxidation process since the As(III)-species are originally in emerald green that change to As(V)-species. Standard reduction potentials (E0 values) at 298.15 K, pressure of 101.325 kPa (1 atm) for half-reactions of this redox reaction are as follow: E0 = 0.40 V for O2 + 2H2O + 4e → 4OH [44] and E0 = − 0.67 V for (AsO4)3− + 2H2O + 2e → (AsO2) + 4OH [45]. This suggest oxygen has the plenty thermodynamic potential to oxidize (AsO2) to (AsO4)3−. The last step involves the reaction of (AsO4)3− and Cu2+, Na+, Ca2+ and Cl which triggers the formation of lavendulan (NaCaCu5(AsO4)4Cl·5H2O) (Eq. 3). The formation of lavendulan needs acid environment [46], this could be supplied by pollution air and acid rain surrounding the grotto.

$${\text{Cu}}\left( {{\text{C}}_{ 2} {\text{H}}_{ 3} {\text{O}}_{ 2} } \right)_{ 2} \cdot 3 {\text{Cu}}\left( {{\text{AsO}}_{ 2} } \right)_{ 2} + {\text{ 8H}}^{ + } \to 4 {\text{Cu}}^{ 2+ } + {\text{ 6HAsO}}_{ 2} + {\text{ 2CH}}_{ 3} {\text{COOH}}$$
(1)
$$2\left( {{\text{AsO}}_{ 2} } \right)^{ - } + {\text{ 2H}}_{ 2} {\text{O }} + {\text{ O}}_{ 2} \to { 2}\left( {{\text{AsO}}_{ 4} } \right)^{ 3- } + {\text{ 4H}}^{ + }$$
(2)
$$5 {\text{Cu}}^{ 2+ } + {\text{ Na}}^{ + } + {\text{ Ca}}^{ 2+ } + 4\left( {{\text{AsO}}_{ 4} } \right)^{ 3- } + {\text{ Cl}}^{ - } + {\text{ 5H}}_{ 2} {\text{O}} \to {\text{NaCaCu}}_{ 5} \left( {{\text{AsO}}_{ 4} } \right)_{ 4} {\text{Cl}}\cdot 5 {\text{H}}_{ 2} {\text{O}}$$
(3)

Cerussite is identified as extender mineral added to the paint, which enwraps the emerald green by using Raman mapping. The dissolution of cerussite (PbCO3) occur in the aqueous phase which can be enhanced in acidic solution and releases the Pb2+ ions. The acidic groups from environment are sufficient to promote the dissolution process [47], with consume of free protons and release of CO2 (Eq. 4) [16]. The solvated arsenate ions ((AsO4)3−) that are supplied from the hydrolysis of emerald green migrating toward Pb2+ ions react with Cl ions to produce the precipitation of mimetite (Pb5(AsO4)3Cl) (Eq. 5). Results of X-ray diffraction analysis show the content of NaCl in the weathered products from the sandstone of Dazu Rock Carvings is about 2.36 wt% and the groundwater types in this area include Ca·Mg–HCO3·SO4 or Ca·Na–HCO3·Cl [48]. These chloride ions in the weathered products and groundwater are available for the formation of mimetite.

$${\text{PbCO}}_{ 3} + {\text{ 2H}}^{ + } \to {\text{ Pb}}^{ 2+ } + {\text{ CO}}_{ 2} + {\text{H}}_{ 2} {\text{O}}$$
(4)
$$5 {\text{Pb}}^{ 2+ } + {\text{Cl}}^{ - } + 3\left( {{\text{AsO}}_{ 4} } \right)^{ 3- } \to {\text{Pb}}_{ 5} \left( {{\text{AsO}}_{ 4} } \right)_{ 3} {\text{Cl}}$$
(5)

Simultaneously, calcium oxalate, e.g. whewellite CaC2O4·H2O, is also founded together with lavendulan by Raman (Fig. 3d). Oxalate salts are formed by calcium ions reaction with oxalate ions over a wide pH range, and commonly occur in art objects. The source of oxalate may be considered as chemical result [49, 50], a product of the oxidative degradation of organic binders [51, 52].

In this study, emerald green has low permanence in the environment of high moisture and soluble salt. This work may help the scholars draw attention to the existence of degradation phase when investigating pigments in complex environment system, e.g. emerald green in damp and salt containing conditions. It also helps scholars rethink about rare minerals as original pigments or degradation products. Because of wide application of emerald green in China, rare copper-arsenic containing minerals could have a high propensity to be identified as degradation products in the paintings after the late Qing Dynasty. Synthetic pigment is crucial for interpreting the historical context of cultural objects, especially for the dating.

Conclusion

In the conservation field of heritage science, study on degradation or corrosion of paint materials e.g. pigments play a vital role in solving key questions of conservation, restoration and storage. In this study, secondary arsenate minerals, namely lavendulan and mimetite, are formed due to the degradation of emerald green and cerussite in the slightly acid and highly humid conditions. This processes appear to: formation of arsenate and copper ions as a result of degradation of emerald green; migration of these ions including partially arsenate ions towards the surrounding area where dissolution of Pb2+ ions from cerussite and Cl ions from environment to product precipitation of mimetite; copper ions remaining in their original place together with arsenate ions and Na+, Ca2+, Cl to form lavendulan.

The formation of lavendulan gives rise to a highlight for green copper-arsenic containing pigment identification as once generally considered to be emerald green and in turn remind the scholars rethink about the rare minerals discovered in the painting as pigments or degradation products.

Obtained from identification of painting layer stratigraphy, the information is crucial for understanding the context of cultural heritage objects regarding relative date of creation, painting technique and artists’ savoir faire. The analysis of paint cross sections from Vairocana Statue in Dazu Rock Carvings, Chongqing, China reveals an example of discrimination the paint dating via material research results. Ultramarine blue, emerald green, synthetic atacamite, vermilion, red lead, gold foil, orpiment, cerussite, gypsum and barite are identified as pigments. Based on the pigment analysis and historical documents, the paintings of the statue have been executed at least four times and the most recent may be after 1850s.

It also demonstrates that Raman spectroscopy mapping and element mapping corresponding with the layer stratigraphy on paint cross section have reliable performance for identification of the components and discrimination between products resulting from degradation processes, especially in the characterization of pigments in complex conditions.

Availability of data and materials

The datasets used during this study are available from the corresponding author on reasonable request.

Abbreviations

UNESCO:

United Nations Educational, Scientific and Cultural Organization

Raman:

Micro-Raman spectroscopy

OM:

Optical microscopy

SEM–EDS:

Scanning electron microscopy with energy dispersive X-ray analysis

CS:

Cross section

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Acknowledgements

The authors wish to express their great gratitude to Miss Fengdan Hu at the Chinese Academy of Cultural Heritage, Professor Yanxiang Li and Mr. Feng Wang at the University of Science and Technology Beijing for their kind support and assistance with this research. Authors would like to thank the peer reviewers and editors for providing valuable feedback.

Funding

Chinese Ministry of Finance’s Special Fund for the Basic Research by Non-Profit Public Research Institutes of Chinese Academy of Cultural Heritage

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QM provided support and guidance for this study. ZL performed the analysis. ZL, LW and HC carried out literature. All authors read and approved the final manuscript.

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Correspondence to Qinglin Ma.

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Supplementary information

Additional file 1: Figure S1.

OM and BSE images of single-layered paint cross sections. Perceived surface colors of samples: CS2  4 blue, CS6  8 green, CS9 red, CS12 red, CS14 gold, CS15 black.

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Li, Z., Wang, L., Chen, H. et al. Degradation of emerald green: scientific studies on multi-polychrome Vairocana Statue in Dazu Rock Carvings, Chongqing, China. Herit Sci 8, 64 (2020). https://doi.org/10.1186/s40494-020-00410-2

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Keywords

  • Dazu Rock Carvings
  • Pigment
  • Degradation
  • Raman mapping
  • Emerald green
  • Lavendulan
  • Mimetite