3.1. Effects of leather burial on collagen shrinkage activity by MHT method
The MHT method provides the shrinkage activity of collagen fibres which is described by a sequence of temperature intervals: no activity − A1 − B1 − C − B2 − A2 − complete shrinkage [32]. In the first two intervals, A1 and B1, shrinkage discretely occurs in individual fibres, but shows a more intense activity (i.e. higher amount of shrinkage per unit of time) in the B1 interval. Most of the fibre mass shrinks in the main interval ΔC called the main shrinkage interval whose starting temperature is considered as the shrinkage temperature, Ts. Generally, the shrinkage in the ΔC is short and intense, and levels off through B2 and A2 intervals. The shrinkage interval is delimited by Tf, the temperature at which the very first motion is observed, and Tl, the temperature of the very last observed motion. The total shrinkage interval is thus calculated as ΔT = Tl ̵̶ Tf.
Table 1 List of the buried leather samples, with their symbols, animal origin and burial time
Animal species
|
Tannin type
|
Burial time (years)
|
Symbol
|
Calf
|
Hydrolysable
|
0
|
CH0
|
|
|
1
|
CH1
|
|
|
2
|
CH2
|
Calf
|
Condensed
|
0
|
CC0
|
|
|
1
|
CC1
|
|
|
2
|
CC2
|
Sheep
|
Condensed
|
0
|
SC0
|
|
|
1
|
SC1
|
|
|
2
|
SC2
|
Cattle
|
Condensed
|
0
|
CaC0
|
|
|
1
|
CaC1
|
|
|
2
|
CaC2
|
|
|
4
|
CaC4
|
Shrinkage behaviour of new, undamaged vegetable tanned leather was shown to depend on the tannin type, animal species and processing method [8, 11]. As vegetable tanned leather ages and deteriorates its shrinkage activity changes specifically depending on the mechanism of damage. Consequently, the shrinkage temperature has been widely used as a metric for leather damage [2, 8, 27–28, 43]. Some of us have also reported how the macroscopic properties of collagen fibres measured by MHT method (i.e., hydrothermal stability expressed as Tf and Ts, and structural cohesivity and heterogeneity expressed as ΔC and ΔT, respectively) correlates with natural or artificially induced ageing pattern [2, 8–9, 16, 44].
For the investigated vegetable tanned leathers, the variation of shrinkage parameters with burial times is reported in Fig. 1. The most important changes we observed were the following:
-
T s increased for all leather samples, regardless of the type of tannin (hydrolysable or condensed) and the duration of treatment, except for CaC4 sample which no longer shows activity in the main shrinkage interval.
-
T f decreased for all samples, but a dramatic decrease occurred for the CH leather tanned with hydrolysable tannin.
-
The shrinkage interval ΔC generally increased except for the CaC4 sample which no longer shows activity in the main shrinkage interval.
-
The total shrinkage interval ΔT generally increased as a result of the increase of both (A1 + B1) and (A2 + B2) intervals. This increase was observed for SC2 sample although it no longer shows activity in the (A2 + B2) interval.
We cand say therefore state that burial experiments led to an increase in the degree of inhomogeneity. For the CH leather samples, the high inhomogeneity is due to a partial surface gelatinisation evidenced by the Tf sharp decrease below 30°C. On the other side, the CH samples show an apparent thermal stabilisation which could be explained by a mechanical strengthening (cementing) of collagen fibres after the prolonged contact with soil minerals. In the case of CC leather samples, the increase of structural inhomogeneity is equally due to the increase in the number of collagen fibres showing discrete shrinkage of individual fibres in the (A1 + B1) and (A2 + B2) intervals. CaC1 and CaC2 leather samples behaves similarly to CC1 and CC2, respectively. SC1 leather sample behaves similarly to CC1, while the SC2’s behaviour is much different in that the (A2 + B2) interval fully disappear and (A1 + B1) interval is greatly diminished. These differences can be attributed to a different burial test resistance over time of the sheep leather compared to calf and cattle leather.
Interestingly, the more coherent collagen fibres (namely those showing shrinkage in the main shrinkage interval ΔC) showed a slight increase of their thermal stability (indicated by the Ts increase) for all leather samples (except for CaC4), while the length of ΔC interval increased. his is in contrast to what was reported so far: Larsen et al. [43] observed that ΔC interval decreased as leather deterioration increased and Carsote and Badea [2] found shorter ΔC intervals in historical leathers compared to new ones and, in some cases, the absence of ΔC interval. A dual behaviour was observed for vegetable tanned leather exposed to gamma irradiation: low-dose irradiation caused an increase of ΔC length, whereas high-dose irradiation led to a progressive shortening of ΔC interval [44]. The authors explained it by distinct deterioration patterns, i.e., the formation of molecular cross-links at low-dose irradiation while the peptide bonds cleavage was promoted by high-dose irradiation. It can be assumed that the mechanical strengthening (cementing) of collagen fibres after the prolonged contact with soil minerals may have similar effects and hence it explains the concomitant increase of Ts value and ΔC interval.
3.2. Effects of leather burial on collagen thermal stability by DSC
The DSC curves for the new leather samples measured in open crucibles and gas flow (Fig. 2) displayed a broad endotherm ranging from room temperature to about 120°C associated with the loss of moisture, followed by two small endotherms in the temperature intervals (135–150) °C and (220–240) °C, respectively (Table 2). The first small peak was related to the thermal denaturation of collagen-tannin matrix, whereas the second peak at T > 220°C was ascribed to the thermal denaturation of the more stable crystalline collagen embedded in the amorphous matrix [26, 41]. These curves are typical for collagenous materials and the two small endotherms are in good agreement with the literature data [26, 45–47]. Budrugeac et al. [28] however, assigned these two endotherms to thermal denaturation of the crystalline collagen embedded in the amorphous matrix. Considering our previous results on parchment thermal behaviour corroborated by the literature data, we are of the opinion that the endotherm at T < 220°C is related to the denaturation of collagen-tannin matrix while the endotherm at T > 220°C is related to the denaturation of crystalline collagen. It is known that crystalline collagen fraction has a much lower degree of hydration being hence much more thermostable.
Table 2
Animal species | Tannin type | Burial time (years) | Symbol |
Calf | Hydrolysable | 0 | CH0 |
| | 1 | CH1 |
| | 2 | CH2 |
Calf | Condensed | 0 | CC0 |
| | 1 | CC1 |
| | 2 | CC2 |
Sheep | Condensed | 0 | SC0 |
| | 1 | SC1 |
| | 2 | SC2 |
Cattle | Condensed | 0 | CaC0 |
| | 1 | CaC1 |
| | 2 | CaC2 |
| | 4 | CaC4 |
DSC and TG/DTG parameters of leather samples before and after the soil burial tests: denaturation temperature of the collagen matrix (Td1), denaturation temperature of the crystalline fraction (Td2) and the rate (V310/%min− 1) of the first process of thermal oxidation. |
The DSC curves for the 1-year buried samples no longer had either of the two small peaks. Such a behaviour was previously observed for parchments exposed to the combined action of polluting gases (50 ppm NOx + SO2) and dry heat (100°C) [26]. This indicates that the burial tests we performed had a strong denaturing effect on collagen, which is somewhat contradictory to the MHT measurements results. We may therefore infer that the increased thermal stability observed by MHT method is due to soil mineral penetration into leather structure having a fibre cementing effect.
3.3. Effects of leather burial on collagen susceptibility to thermo-oxidative deterioration by TG/DTG
It was reported that the non-isothermal deterioration of leather occurs through three processes accompanied by mass loss: (i) water loss at T < 150°C, (ii) pyrolytic thermo-oxidation and (iii) thermal decomposition of the material [27–28]. These processes are evidenced in the DTG curves by the peaks I, II and III (Fig. 3). The rate of the thermo-oxidation process corresponds to the maximum of the thermo-oxidation peak, namely the peak II (Fig. 3). For various collagen-based materials it was shown that the rate d%Dm/dt of the pyrolytic thermo-oxidation process calculated at 310°C well correlates with the collagen matrix cross-linking degree. Accordingly, Budrugeac et al. [28] used this parameter as an indicator of the damage level in historical collagen-based materials relating the high rates of the thermo-oxidation process to not-damaged/well conserved leather, and the lower rates to various damage levels. In fact, the lower the rate the higher the deterioration degree. The rates d%Dm/dt of the pyrolytic thermo-oxidation process for the investigated leather samples reported in Table 2 show a progressive decrease of the oxidation rate as burial time increases. This thermo-oxidation susceptibility increase clearly indicates an increase of the damage level with burial time.
3.4 Effects of leather burial on molecular alteration of collagen-tannin matrix by FTIR-ATR
The following aspects were considered when studying the FTIR-ATR spectra of the investigated samples: the effect of burial tests on the behaviour of the complex spectral bands resulted by the overlapping of collagen and vegetable tannins bands, and identification of added during manufacturing or formed during burial [12, 17, 21].
In Fig. 4, the FTIR-ATR spectra of the buried leather samples (CaC1, CaC2 and CaC4) are illustrated and compared with those of newly manufactured leather (CaC0). For all leather samples, the main infrared absorption bands of collagen were cleary detected: (i) the amide A (AA) at ~ 3300 cm− 1 related to stretching vibrations of the amide N-H bonds; (ii) the amide B (AB) at ~ 3080 cm− 1 attributed to the Fermi resonance overtone of the amide II vibration; (iii) the amide I (AI) at ~ 1633 cm− 1 arising mainly from the C = O stretching vibration; (iv) the amide II (AII) at ~ 1538 cm− 1 attributed to NH in plane bend and CN stretching vibration and (v) amide III (AIII) at ~ 1235 cm− 1 corresponding to the NH bending, CN stretching vibration and small contributions from both CO in plane bending and CC stretching vibration [48–49].
There are FTIR-ATR bands specific of all vegetable tannins (hydrolysable and condensed) detectable at: 1606 cm-1 (νC=C; aromatic ring), 1507 cm-1 (νC=C; skeletal ring), 1445 cm-1 (νC=C; aromatic ring), 1198 cm-1 (νC-OH; aromatic) and 1030 cm-1 (β - CH deformation). The hydrolysable tannins are specifically identified through typical bands occurring at 1721 cm-1 (νC=O; phenolic esters lactones or phenolic esters), 1322 cm-1 (νC-O; lactones), 1080 cm-1 (νsC-O-C; aryl phenolic ester), 872 cm-1 (γOH and γC-H; tetrasubstituted aromatic) and 758 cm-1 (νs skeletal - sugar ring, breathing vibration). On the other hand, condensable tannins also present typical bands at 1282 cm-1 (νC-O; pyran ring), 1159 cm-1 (νsC-O-C; cyclic ether), 1110 cm-1 (νasC-O-C; cyclic ether), 976 cm-1 and 842 cm-1 (γC-H; tetrasubstituted aromatic) [18–19]. Due to the tannin presence, the spectra of leather are characterized by bands overlapping in the amide I, amide II, and amide III regions making it rather difficult to specifically attribute the spectral variation as a result of deterioration.
For example, in Fig. 4 is observed a reduction of the band intensity in the amide I and amide II region suggesting some changes in the structure of collagen–tannin matrix. However, for a more accurate assessment of the alterations that occurred in the secondary structure of collagen, the second derivative of FTIR spectra was calculated in the spectral range of amide I and amide II (Fig. 5). The second derivative of the FTIR-ATR spectra of new leathers were first characterized and we found the followings (Fig. 5):
-
two components of amide I centered near 1660 cm-1 and 1622–1628 cm-1, respectively;
-
two components of amide II centered near 1550 cm-1 and 1502–1515 cm-1, respectively;
-
one tannin band at 1602–1605 cm-1, visible as a shoulder of the second component of amide I;
-
a tannin band that fully overlaps the second component of the amide II.
As a result of the burial tests, both amide I components began to decreased after the first year for CC, SC and CaC leathers. In the same time, the tannin band at 1602–1605 cm− 1 decreased, too, suggesting a loosening of the collagen – tannin interactions. This destabilization led to de-tanning after the second year of the burial tests as indicated by the net separation of the amide I and tannin bands. The loosening and then breaking of collagen-tannin interactions during burial is also suported by the changes in the amide II region characterized by the shift of the component at 1550 cm− 1 towards lower wavenumbers (1546–1538 cm− 1), related to α-helix structure conversion to disordered structures [50], and progressive depletion of the complex band observed at 1502–1515 cm− 1. Interestingly, for CH leather samples, the intensity of the 1660 cm− 1 component decreased while the intensity of the 1628 cm− 1 component increased. This behaviour may be explained by the unfolding of the native left-handed triple α helix into a random coil structure, resulting in the formation of gelatine. It is thus confirmed the gelatinisation of CH leather evidenced by the MHT method. A similar spectral behaviour was previosly explained by Stani et al. [51] through the formation of larger number of water-mediated hydrogen bonds in denatured collagen. They assigned the component near 1630 cm− 1 mainly to the carbonyl stretching of hydroxyproline and of the others amino acids involved in water mediated hydrogen bonds in the native state [52]. Recently, some of us reported an number of these carbonyl moieties in denatured α-chains for collagen (in parchment) exposed to dry-heat ageing, causing the component at 1632 cm− 1 to increase in intensity [40].
The analysis of FTIR-ATR spectra after 1-year burial indicate the bands of fatliquoring oils/ fats at ∼2920 and 2850 cm− 1 (νasCH2 and νsCH2) and at ∼1735 (νasC=O), while the soil aluminosilicates were identified by their specific bands at ~ 1030 cm− 1 (νSi−O), 525 (δAl−O−Si) and 465 cm− 1 (δSi−O−Si) [53] (Fig. 4). Calcium carbonate was identified by its main absorption bands at 1405 cm− 1 (νasCO3) and 874 cm− 1 (δCO3) (Fig. 4). Its presence could be attributed to the leaching of the mineral components driven either by soil humidity or microbial attack [36].
3.5 Effects of burial tests on leather surface morphology by SEM
Collagen structural damage in the fibrillar structure and network documented by SEM imaging on all the buried samples confirmed the above illustrated findings. The newly manufactured leather showed ordered fibrillar networking with the fibrils grouped in bundles (Fig. 6a) and their typical periodic structure cleary visible at higher magnification (Fig. 7a). The buried samples displayed discontinuities and loosening of the fibre matrix cohesion, progresive shrinkage and extended melted/gelatinised areas (Fig. 6b and 6c). The loss of fibrilar structure and massive presence of amourphous and gelatinised structures are already evident at higher magnification after 1-year burial period (Fig. 7b). Bozec and Odlyha [54] related the loss of the repeted periodicity of collagen fibril ultrastructure to collagen entirely structurally denaturated. Collagen structurraly denaturation is in accordance with the DSC results presented above.
In addition, a microbial attack with the leaching of mineral component on the leather surface (most problably calcium carbonate, as indicated by FTIR-ATR results) was observed (Fig. 8). The chains of bacterial spores and filaments resemble the typical structure of some Actinomycetes [36], aerobic spore forming gram-positive bacteria, which are the most abundent organism that form thread-like filaments in the soil and play a major rôle in the cycling of organic matter [55].
3.6 pH variation as a result of the burial tests
The pH value of the new vegetable tanned leathers was in the range 3.5–4.6, depending on the tannin type and manufacturing process. The pH values of the buried leather increased to 6.5–7.3, which is actually the pH value of the soil. In fact, the soil acts as a buffer, so the pH value of the archaeological leather does not depend on the type of damage, but on the type of soil in which it was buried.