1 Introduction

Archaeological ceramics are, from an historical point of view, very relevant materials as the information they possess help historians to understand the societies from the past. In this way, archaeological ceramics provide data regarding the technological development of these societies. This includes information about the raw materials used, how they were prepared, how and by whom they were modelled, how they were fired (temperature and atmosphere), and what they were used for (cooking, food storage, rituals…) [1]. Besides, the physical and chemical features make archaeological ceramics very resistant materials, in comparison with glass or organic materials such as wood [2]. However, they can present several alterations: material loss, cracking, decoration loss, etc. Among them, soluble and insoluble salts deposits are the most common ones, both in buried and underwater finds. Indeed, calcareous deposits not only appear on buried ceramics, as underwater materials also present deposits from calcareous shells of marine animals [3]. Whereas soluble salts are easy to remove by immersion in water, the removal of insoluble salts implies the use of chemical products that soften the deposits. For example, calcium carbonate is very difficult to remove mechanically or dissolve in water due to its low solubility (CaCO3 kps = 4.8 × 10–9) [4]. Even though current trends in the conservation–restoration field are more respectful and tend to leave them under controlled ambient conditions [5], sometimes, their removal becomes necessary. For example, if the deposits imply an information loss, by covering a piece of decoration or some writing. Also, if the pieces are going to be exhibited, their aesthetic values become fundamental and the deposits might interfere with their appreciation.

For the removal of these deposits, since the 70s, conservators have developed and performed several treatments, based on acid and basic solutions to soften the deposits, followed by a mechanical action [1, 6]. Regarding the application methods, direct, as immersion, and indirect, as poultices, are the most common ones [7,8,9,10]. Indirect application methods are, in general, easier to control, as they release the product contained in a more gradual way. They are also meant to be safer than direct ones, as more specific areas can be treated. For this reason, other products were developed from the 80s onwards for indirect methods: the thickening agents. Since then, they became quite common in the conservation–restoration field. However, they are still not usual in the conservation of archaeological objects [11,12,13,14,15]. Within this research project, a survey among 54 Spanish conservators was conducted in 2018 in order to know more about current treatments. According to the data obtained, poultices (70.4%), gels (37%) and static baths (22.2%) were the three most common application methods used for the removal of calcareous deposits, among others. Poultices can be made of clay, cellulose or cotton, whereas gels consist of agarose, polyacrylic acid, xanthan gum or other polymers. On the other hand, static baths consist of the immersion of the pieces in the selected product without adding movement. Regarding products, acids (55.6%) and chelating agents (74.1%) resulted the most usual ones. Finally, for the removal of the possible remains, or neutralisation process, the most common method is the immersion or static bath in distilled or deionised water, alone (70.9%) or combined with other products (buffers, basic solutions, etc.) (16.4%) [16].

It is important to bear in mind that, in the same way that the products applied to remove insoluble deposits are effective, they might be also altering the minerals contained in the ceramics matrixes. More specifically, carbonates, such as calcium carbonate (CaCO3) or dolomite [CaMg(CO3)2], might be dissolved by the effect of acid and chelating agents. Even though some studies proved that acid products may affect the original composition of the ceramics, they are still in use [17,18,19]. In order to guarantee the safety of the ceramic pieces treated with these products, it becomes essential to analyse their effects on these materials, as they might be harmful and imply severe and irreversible consequences to the conservation of the ceramics.

This research aims to study the efficacy and safety of acid products applied by immersion in the removal of calcareous deposits, by determining the mineralogy composition by XRPD and the quantification of calcium carbonate by TG-DSC. For this purpose, a methodology for the elaboration of ceramic specimens and the growth of calcareous deposits has been developed.

2 Materials and methods

2.1 Ceramic specimens

Four groups of ceramic specimens, fired at four different temperatures, were elaborated in order to simulate archaeological ceramics with different properties [20]. A red commercial clay Sio-2® ARGILA (Ceramica Collet S.A.) was used for its similarity with red natural clays, one of the most common clays used for ceramics since ancient times, due to its easy accessibility and natural plastic properties [21, 22]. No tempers or water were added during its manipulation. Its chemical composition established by XRF was provided by the supplier enterprise J. L. Vicentiz, S. L. According to the results expressed in oxides (Table 1), the main components of the red clay used are silicon oxide (SiO2) and aluminium oxide (Al2O3), in minor concentration iron, calcium, potassium and magnesium oxides were detected (Fe2O3; CaO; K2O; MgO; respectively). Other components were also found: titanium, sodium and manganese oxides (TiO2; Na2O; MnO). These results were verified and completed, so they could be used as a reference in the research. Besides, its mineralogical composition was established by XRPD and oriented aggregates patterns (OA) (see "Results and discussion" section).

Table 1 XRF results expressed in oxides of the red commercial clay used for the elaboration of the ceramic specimens. L.O.I.: Loss on Ignition. Analysis provided by J.L. Vincentiz S.L
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Layers of 1 cm thick of clay were cut and flattened using a rolling pin, without hand modelling, and later cut into approx. squares of 5 cm side (Fig. 1a, b). The specimens were let dry in a climatic chamber (Vötsch Indusrietechnik VCL 4010) at a temperature of 20 °C and 50% of relative humidity (RH) (Fig. 1c). After 5 h, they were turned around to allow a homogeneous drying process, and 72 h later, the specimens were introduced into a muffle furnace (SNOL 30/1300 L) and fired up to 120 °C at a heating rate of 2 °C/min and 5 min soak to eliminate hygroscopic water [23].

Fig. 1
figure 1

Elaboration of the ceramic specimens, including the modelling of the clay (a), the shaping of the specimens (b), their drying in climatic chamber (c), the firing process (d) and the final specimens (e)

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Afterwards, the specimens were introduced again into the climatic chamber at 20 °C and 50% RH to cool them down. In order to reproduce archaeological firing temperatures, the specimens were fired up to 650, 800, 1000 and 1100 °C at a heating rate of 2 °C/min and 3 h soak (Fig. 1d). Once cooled down in the muffle furnace under 100 °C, they were introduced into the climatic chamber at 20 °C and 50% RH for 24 h (Fig. 1e).

2.2 Artificially growth of calcareous deposits

Subsequently, to favour the growth of calcareous deposits on the ceramic specimens’ surfaces, a specific methodology was developed. A lime putty of four years maturation time (supplied by Proiescon S.L.) and limewater obtained from it were used for the growth of calcium carbonate deposits on the surface of the specimens, together with dried and sieved soil (250–63 µm) from the archaeological site of Guarrazar (Toledo, Spain). Its mineralogical composition was studied by XRPD and oriented aggregates (see “Results and discussion” section). In first place, the fired ceramic specimens were introduced into a lime water bath (3:1 vol.) for 7 days (Fig. 2a). Afterwards, a layer 2–3 mm thick of lime putty mixed with the sieved soil (3:1 vol.) was applied on the surface (Fig. 2c). To end with, the pieces were introduced for 10 days into a climatic chamber (Dycometal CCK -25/81) at 20 °C, 60% RH and 1600 ppm CO2, conditions that favoured the carbonation process of the deposits previously applied (Fig. 2d). The resulted deposits presented more adherence in the pieces fired up to higher temperatures (1000 and 1100 °C) than those fired to lower ones (650 and 800 °C) (Fig. 2e). For these last lower temperatures, a white veiling accumulation appeared underneath the lime putty deposit because of the immersion in lime water that hampered a high adhesion of the lime putty to the ceramic surface (Fig. 2b). Due to this lack of adhesion, some of the growth deposits shown craquelure on their surfaces (Fig. 2e).

Fig. 2
figure 2

Artificially growth of the calcareous deposits on the surfaces of the ceramic specimens. First the immersion in limewater (a, b), followed by the application of the mixture of lime putty and sieved soil (c), the carbonation process in the climatic chamber (d) and the deposits obtained (e)

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2.3 Cleaning treatments

In order to remove the artificially grown calcareous deposits, two acids, the most used in archaeological ceramics, according to the survey conducted, were tested: acetic acid (CH3COOH, AA for short), a weak acid, and nitric acid (HNO3, NA for short), a strong one. Acids react with calcium carbonate and transform it into the soluble salts: calcium acetate and calcium nitrate, respectively. After that, the deposits are easily removed by mechanical means. The occurring chemical reactions during this process are the following:

$$\text{CaCO}_{3}+ {2 \text{CH}}_{3}\text{COOH} \to \text{Ca(CH}_{3}\text{COO)}_{2}+\text{CO}_{2}+\text{H}_{2}\text{O}$$
$$\text{CaCO}_{3}+ {2 \text{HNO}}_{3} \to \text{Ca(NO}_{3})_{2}+\text{CO}_{2}+\text{H}_{2}\text{O}$$

According to the Spanish standard UNE 41806-2 IN: 2009 [24], minimum concentration of the products and shortest treatment were set as basic criteria for the cleaning treatments. For this reason, solutions of the acids were prepared at 1% vol. in deionised water. The pH values were set as 2.76 ± 0.01 for acetic acid and 1.16 ± 0.01 for nitric acid (measured with a Seven Compact pH meter S220 METTLER TOLEDO, sounding line InLab® Expert Pro-ISM). After several tests, 30 min was set as the minimum time for the treatments to be effective. One ceramic specimen of each firing temperature (650, 800, 1000 and 1100 °C) was introduced in 300 mL of each acid solution for at least 30 min. Afterwards, the existing remains of the deposits were mechanically removed with wooden sticks. Table 2 shows the samples obtained at various temperatures and tested with different acid solutions to clean the calcareous deposits. Three of the specimens (C800 NA, C1100 AA, C1100 NA) needed additional time to soften the deposits, so the chemical treatment was repeated for 10 more minutes (Table 2). Specimens after the cleaning treatments are shown in Fig. 4. As can be noticed, the possible remains of the deposit no longer interfere in the appreciation of any of the ceramics (Fig. 3).

Table 2 Characteristics and conditions of the acid treatments, both acetic acid and nitric acid at 1% vol., applied by immersion to the ceramic specimens
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Fig. 3
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The appearance of the pattern specimens’ surface (PAT), carbonated specimens (CAR), treated specimens with acetic acid (AA) (c) and treated specimens with nitric acid (NA) (d)

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After the treatments, it was necessary to neutralise their effect and remove the soluble salts resulted from them. The neutralisation process was made by immersion in deionised water (pH ≈ 6–7), in an approximated ratio of 1:15 g/ mL [25]. To monitor this neutralisation process, conductivity measures (K) were recorded with an electrical conductivity meter (Delta-Ohm HD2156.2) at 0, 5, 10, 15, 30, 60, 120, 180 min. To establish the endpoint of the neutralisation process, the variation in Knorm was monitored, as it considers the change in conductivity, regarding the water volume, time and mass of the specimen as follows [25, 26]:

$${K}_{\mathrm{norm}}=\frac{\Delta K\times L}{\Delta t\times g}$$

where \(\Delta K\) is the variation in conductivity, L is the water volume in litres, \(\Delta t\) is the time passed since the beginning of the process in days, and g is the mass of the specimen to be neutralised in grams. According to White et al. [26], the process ends when the values of Knorm are below or equal 2 (Knorm ≤ 2) (Fig. 4). However, in this case, these values were reached much earlier, probably because the amount of salts was lower, so it was decided that the variable Knorm should reach 2 twice, after renewing the water when the variable reaches 2 for the first time (Table 3). When this process ended, the ceramic specimens were introduced again into the climatic chamber at 20 °C and 50% RH to let them dry for 24 h. In Table 3 and Fig. 4 are gathered, as an example, the values of the neutralisation process of the specimen C650 treated with acetic acid (AA).

Fig. 4
figure 4

Monitoring of the neutralisation process in specimen C650 AA (see Table 2), treated with acetic acid by immersion. Variation in time of the variable Knorm

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Table 3 Monitoring of the neutralisation process in specimen C650 AA (see Table 2), treated with acetic acid by immersion
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2.4 Chemical and mineralogical composition

The chemical composition of the clay was determined by X-ray fluorescence (XRF) with a Panalytical Zetium equipment, and the results obtained were analysed with the software Omnian® (Panalytical). The analysis of oriented aggregates (OA) of the clay was pursued with a Bruker D8 ADVANCE equipment in Bragg–Bretano θ–θ configuration (Cu Kα radiation, 40 kV, 40 mA, angular range 2°–35° (2θ) with a step of 0.02° and 0.8 s counting time). However, mineralogical changes were determined by XRPD.

One ceramic specimen of each firing temperature (650, 800, 1000, 1100 °C) was chosen as patterns and analysed before the carbonation process. The ceramic specimens cleaned with the treatments tests were also analysed. Their mineralogical composition was studied by X-ray powder diffraction (XRPD) with a Panalytical X’Pert MPD equipment in Bragg–Bretano θ–θ configuration (Cu Kα radiation, 45 kV, 40 mA, angular range 5°–70° (2θ) with a step of 0.02° and 1 s counting time). For this purpose, fragments of the ceramics were finely grinded with an agate mortar. The phase identification was conducted using the PDF-2 2002 ICDD database using the HighScore Plus® software. Besides, mineralogical composition of the soil used for the carbonation process was also determined with XRPD and OA techniques.

Thermogravimetric (TG-DSC) analyses were also carried out to establish variations in the content of the calcium carbonate (CaCO3) after the carbonation process and after the cleaning treatments, in comparison with the non-treated patterns. A simultaneous thermal analysis equipment SDT Q600 (TA® Instruments) was used; 10 mg of powder samples was analysed in platinum capsule at a heating rate of 10 °C/min, from room temperature to 1000 °C in nitrogen atmosphere with a 100 mL/min flow. The results obtained were analysed with TA Universal Analysis® software.

3 Results and discussion

3.1 X-ray fluorescence of the commercial clay

The XRF results provided by the supplier enterprise J. L. Vicentiz, S. L. (Table 1), were verified and completed. The data obtained shown high similarity, as the main components and quantities agreed. However, a semiquantitative analysis was conducted and its trace elements were identified. Table 4 shows the results obtained both of the major and minor components and trace elements.

Table 4 XRF results expressed in oxides and ppm of the red commercial clay used for the elaboration of the ceramic specimens
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3.2 X-ray powder diffraction

The XRPD pattern of the clay used for the ceramic specimens is shown in Fig. 5. Significant amount of quartz, (SiO2) [JCPDS 01-086-1629] has been identified, together with phyllosilicates (muscovite (KAl3Si3O10(OH)2) [JCPDS 01-076-0929] and/or illite KAl2(Si3Al)O10 (OH)2 [JCPDS 00-043-0685] and clinochlore ((Mg,Fe)6(Si,Al)4O10(OH)8) [JCPDS 00-029-0701]), feldspar (albite Na(AlSi3O8) [JCPDS 01-071-1150] and orthoclase (K(AlSi3O8)) [JCPDS 01-076-0749]), and other minerals as hematite, (Fe2O3) [JCPDS 01-085-0599] (Fig. 5). Some amount of calcite (CaCO3) [JCPDS 01-072-1651]) and dolomite (CaMg(CO3)2) [JCPDS 01-073-2361], were also detected. Among phyllosilicates, the main components were determined by oriented aggregates patterns (OA). According to the results, mica-illite (60%) and smectite (25%) were the main phases, along with chlorite (8%) and kaolinite (7%) in minor concentration.

Fig. 5
figure 5

Diffraction patterns of specimen patterns of the unfired clay and specimens fired at five temperatures (120, 650, 800, 1000 and 1100 °C). Ab: albite; An: anorthite; Cal: calcite; Clc: clinochlore; Dol: dolomite; Hem: hematite; Mica: muscovite and/or illite; Or: orthoclase; Qz: quartz

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Besides, the XRPD patterns of the ceramic specimens fired at different temperatures are also included in Fig. 5. The peaks corresponding to phylosillicates (muscovite and/or illite) decreased with the rise in temperature and disappear at 1000 °C. Orthoclase main peak (26.9°) reduces its intensity and disappears at temperatures above 800 °C. Clinochlore disappears before reaching 650 °C. Anorthite is detected at 1000 °C and increases its diffraction peaks at higher temperatures [27, 28]. In the same way, the maximum peaks of hematite became more intense and narrow as the firing temperature increased, probably due to a crystalline growth [7]. The decomposition of calcite begins above 650 °C and disappears above 800 °C. Quartz remains the most abundant phase at all temperatures. The existence of an amorphous phase is evidenced by the increased background noise at temperatures above 800 °C, which suggests that samples are undergoing vitrification.

Besides, the mineralogical composition of the soil from Guarrazar used for the growth of the artificial deposits was analysed. In the XRPD patterns, quartz [JCPDS 01-089-1961], calcite [JCPDS 01-081-2027], phyllosilicates as dickite [JCPDS 01-074-1758] and clinochlore [JCPDS 01-079-1270] were identified. Also plagioclases as anorthite [JCPDS 01-086-1707] and albite [JCPDS 01-076-0898] were detected. The analysis of oriented aggregates of the phyllosilicates (OA) determined its composition by: mica-illite (78%), smectite (12%), chlorite (5%) and kaolinite (5%).

All the clay specimens were studied again after the cleaning treatments, showing no differences in any of the mineralogical phases detected (Fig. 6). Indeed, calcite peaks are detected, in both C650 and C800 specimens, which suggest that the acid treatments did not dissolve the carbonates from the ceramic. However, the semi-quantification of calcium carbonate content was made by the thermogravimetric analysis.

Figs. 6.
figure 6

Diffraction patterns of ceramic pattern specimens (PAT) and treated specimens (AA and NA) fired at the four temperatures: a 650 °C, b 800 °C, c 1000 °C and d 1100 °C. Ab: albite; An: anorthite; Cal: calcite; Dol: dolomite; Hem: hematite; Mica: muscovite and/or illite; Or: orthoclase; Qz: quartz

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3.3 Thermogravimetric analysis

TG–DSC curves were evaluated considering both the mass loss expressed as percentage and the heat flow of samples as a function of temperature.

In all the thermograms, there was an endothermic peak at 573 °C, which did not imply a weight loss, related to the polymorphic inversion of α quartz [29].

Another endothermic peak raised at ~ 400 °C, both in pattern (Fig. 7a) and carbonated specimens (Fig. 7b). This peak is ascribed to the loss of structurally bound water [30,31,32]. In the pattern samples, this peak is observed only in samples fired at low temperature (C650 and C800) and is linked to a small weight loss. Together with the results of XRPD data, this peak is ascribed to dehydroxylation of muscovite [33]. On the other hand, at this temperature range (380–430 °C), another endothermic peak is observed in all the carbonated samples, no matter the firing temperature (Fig. 7b). From the derivative curve, within this temperature range, it is possible to observe two overlapped peaks in the samples fired at low temperature (C650 and C800), and only one in the samples fired at high temperature (C1000 and C1100), both linked to a weight loss. The first one can be ascribed to the dehydroxylation of calcium hydroxide [34], present in all samples, whereas the second one, to the dehydroxylation of muscovite [33], as determined in pattern samples and according to XRPD data. This would mean that during the carbonation process, not all of the calcium hydroxide (Ca(OH)2) applied was transformed into calcium carbonate (CaCO3). The endothermic peak at ~ 400 °C in the treated samples was only present in the specimens fired at low temperature (Fig. 8a, b) as happened in the pattern samples (Fig. 7), so that peak can be ascribed to the dehydroxylation of muscovite alone, meaning that the cleaning treatments were effective in the removal of the Ca(OH)2 present in the carbonated specimens. In DSC curves of pattern specimens C650 and C800 (Fig. 7a), an important endothermic peak appeared ~ 655 °C together with a weight loss around 500–750 °C, related to the decarbonation of calcium carbonate [30, 32], which was in agreement with the XRPD results. On the other hand, pattern specimens fired at 1000 and 1100 °C, did not show any transformation within this temperature range (Fig. 7a), confirming the absence of calcium carbonate in these samples, in consonance with XRPD results. Besides, all the carbonated specimens showed such peaks due to decomposition of calcium carbonate from the carbonation process (Fig. 7b). However, the weight losses linked to this peak were higher for C650 and C800 than those detected in C1000 and C1100 (Fig. 7b).

Fig. 7
figure 7

On the left (a), thermograms of pattern specimens (PAT) and on the right (b), thermograms of carbonated specimens (CAR) for all the firing temperatures. In pink the heat flow (W/g) curve, in green the weight (%) and in blue the derived of the weight (%/°C). The dehydroxylation of muscovite is detected ~ 400 °C, whereas the decarbonation process takes place ~ 655 °C. The differences in the weight loss depend on the firing temperature specimens

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Fig. 8
figure 8

Thermograms of all the specimens after the cleaning treatments, with acetic acid (AA) and nitric acid (NA): a 650 °C, b 800 °C, c 1000 °C and d 1100 °C. In pink the heat flow (W/g) curve, in green the weight (%) and in blue the derived of the weight (%/ °C). The thermograms show important differences regarding the firing temperature of the specimens. The decarbonation process is detected in C650 and C800 specimens both before and after the cleaning treatments. In the same way as that the dehydroxylation process

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On the other hand, in thermograms of cleaned specimens (Fig. 8), features related to the decomposition of calcium carbonate were detected in all of them, but with lower magnitude as the firing temperature increases, with the exception of the highest firing temperature (C1100). In the specimen C650 AA a weight loss of 3.9% between 532.6 and 738.4 °C was detected. In a similar way, another weight loss of 4.0% between 515.1 and 723.6 °C was also detected in the specimen C650 NA (Fig. 8a). These weight losses detected at the temperature range 500–740 ºC are higher than the weight loss detected in the pattern sample C650 PAT at the same temperature range (2.7 %) (Fig. 7a). The same occurs for C800 treated samples, as after both treatments (AA and NA), a weight loss of 1.3% is detected between 502.4 and 675.2 °C for C800 AA and 525.9–677.8 °C for C800 NA (Fig. 8b). Also, for the specimens C1000 AA and 283 NA, a small weight loss of 0.3% is detected between 522.5 and 650.3 °C for AA, and between 517.1 and 640.9 °C for NA. However, the weight loss due to the decarbonation process is not detected in C1100 AA and NA specimens after the cleaning treatments (Fig. 8c, d), meaning that, for lower firing temperatures specimens (C650 and C800), the treatments were effective as they removed the artificial deposits, although there were still remains. Whereas for the highest firing temperature specimen (C1100), the cleaning treatments have been more effective, as no remains of calcium carbonate were detected. On the other hand, the endothermic peaks related both to the dehydroxylation of muscovite and calcium hydroxide were noticeable after both acid treatments for the specimens fired at lower temperatures (Fig. 8a, b). However, it was not found in the thermograms of specimens fired at higher temperatures (Fig. 8c, d). So then, the cleaning treatments were effective in the removal of calcium hydroxide, and the peak found in specimens fired at lower temperatures was linked to the muscovite [32].

In addition, according to the results obtained from the thermogravimetric analysis, the approximate calcium carbonate content was calculated regarding the weight loss and the following reaction:

$$\text{CaCO}_{3}\left(100.01 \,\text{g}\right)+\text{Q} \left(\text{J}\right)\to \text{CaO} \left(56.07 \,\text{g}\right)+\text{CO}_{2}(44.01 \,\text{g})$$

The results gathered in Table 5 determined that the calcium carbonate content in pattern specimens was higher for the lower firing temperatures, in agreement with XRPD data. Besides, the carbonation process was effective in the specimens fired at the four temperatures as the calcium carbonate content increased in all of them. However, this content decreased as long as the firing temperature increased. Besides, the calcium carbonate content did not decrease after the cleaning treatments in comparison with the pattern specimens. Indeed, there was a small increase in all cases with the exception in the specimen C1100. This increase might be due to the remains of the calcareous deposits generated after the carbonation process that were not completely removed by the cleaning treatments. However, they were not noticeable to human eye and do not interfere with the aesthetical values of the specimens.

Table 5 Weight loss and content of calcium carbonate in specimens at the four firing temperatures, pattern (PAT), carbonated (CAR) and after the treatments (AA, acetic acid; NA, nitric acid)
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From the data obtained, the remains of the calcareous deposits were established, calculated as the difference between the calcium carbonate content in carbonated and treated specimens. These contents were attached to the firing temperatures, as for both the acetic and the nitric acid treatments, the values were higher for C650 specimens and decreased along with the specimens fired at higher temperatures (Table 6). Besides, the efficacy of the treatments was calculated taking into account the removal of the artificial calcareous deposits after the acid treatments. For the sample fired at the lowest temperature, the largest deposit was observed (4.1% CaCO3), and the efficacy resulted the lowest (33.3% with AA and 27.8% with NA). As long as the deposit decreased, the efficacy of the treatments increased, reaching 100% efficacy in specimen C1100, both for acetic and nitric acid. Although 100% efficacies were not reached in all the cases (Table 6), they were enough to make the remains unnoticeable to human eye. It is also important to point out that the efficacy of the treatments was very similar, even equal, for both acids tested.

Table 6 Relative variation in the CaCO3 content (%) in the specimens fired at the four temperatures. Calculated efficacy of acid treatments
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4 Conclusions

According to the results, on one hand, the process followed for the elaboration of the specimens was a success, as well as the artificially growth of the surface deposits, as they both simulate archaeological ceramics characteristics. Regarding the carbonation process, calcium hydroxide (Ca(OH)2) was detected by TG-DSC, in all the carbonated specimens, meaning that the carbonation process was not concluded, as the calcium hydroxide applied on the ceramic surface was not completely transformed into calcite (CaCO3). In addition, a correlation between the firing temperature and the growth of the deposits was found: the lower the firing temperature, the larger the deposit.

Besides, both acid treatments employed for the removal of calcareous deposits on ceramic specimens were effective, since the deposits were successfully removed as they are no longer noticeable to human eye. Even though, their efficacy varied and was linked to the amount of the deposit. For larger deposits, the efficacy decreased. However, it was proved that even with low efficacies (~ 30%), the deposits are not visible. For this reason, they would no longer interfere with the aesthetic values of the specimens. Besides, calcium hydroxide is not detected after the cleaning treatments, and due to the stability of calcite, the conservation of the specimens would not be jeopardise.