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u-Raman, such as plumbonacrite, indicate the need to stabilize chemically these soaps since they are responsible for a continuum of chemical degradation phenomena [5].These chemical reactions also contribute to the physical degradation of the paintings, since the increase of volume of lead carboxylates causes instability in the ground and painting layers, being probably one of the causes contributing to the detachment of these layers from the support.  Figure 2. a) Micro-Fourier transform infrared (u-FTIR) spectrum from the green shadow of the grass, in P2, displaying azurite, kaolinite, oil and metallic carboxylates; b) u-FTIR spectrum from the light green of the grass, in P4, displaying azurite, hydrocerussite, oil and lead carboxylates.  These results prove the evidence of the poor state of conservation of the studied groups, with no exception. Big areas of lacunae were detected in many parts of the paintings, some of them already restored (P1—P2, P5). These lacunae are more evident in the lower part of each painting as confirmed by IRR and IRP results. This fact suggests that a higher amount of humidity was accumulated in this area. Ascensional absorption of the wood canals in the lower part of each painting was the main cause for this degradation, probably being in contact with floor humidity. Also, the high humidity in the air was verified. Relative humidity was controlled in P1 and P2 in summer and winter. In other paintings (P3—P5) climate verification was not possible for this study, since it takes at least one year to analyze climate changes according to seasoning. P3 and P4 were brought from a church to the museum climate during the last year and P5 remained for several years in a museum climate. Results on P1—-P2 climate verification showed that the change in the relative humidity environment varies between 63% and 70% in the dry season (summer). This means a variation of 7% in relative humidity between morning and afternoon, and the relative humidity should not fluctuate more than 10% in 24 hours. It has to be considered that this maximum value of 70% of relative humidity is the value from which it is agreed that the various objects of organic structure, especially painting, begin to change their dimensions, lose their original rigidity, becoming plastic and more vulnerable to the formation of fungus [6,7]. However, in the wet season (winter) an approximate relative humidity of 78%-83% was detected.

Figure 2 u-Raman, such as plumbonacrite, indicate the need to stabilize chemically these soaps since they are responsible for a continuum of chemical degradation phenomena [5].These chemical reactions also contribute to the physical degradation of the paintings, since the increase of volume of lead carboxylates causes instability in the ground and painting layers, being probably one of the causes contributing to the detachment of these layers from the support. Figure 2. a) Micro-Fourier transform infrared (u-FTIR) spectrum from the green shadow of the grass, in P2, displaying azurite, kaolinite, oil and metallic carboxylates; b) u-FTIR spectrum from the light green of the grass, in P4, displaying azurite, hydrocerussite, oil and lead carboxylates. These results prove the evidence of the poor state of conservation of the studied groups, with no exception. Big areas of lacunae were detected in many parts of the paintings, some of them already restored (P1—P2, P5). These lacunae are more evident in the lower part of each painting as confirmed by IRR and IRP results. This fact suggests that a higher amount of humidity was accumulated in this area. Ascensional absorption of the wood canals in the lower part of each painting was the main cause for this degradation, probably being in contact with floor humidity. Also, the high humidity in the air was verified. Relative humidity was controlled in P1 and P2 in summer and winter. In other paintings (P3—P5) climate verification was not possible for this study, since it takes at least one year to analyze climate changes according to seasoning. P3 and P4 were brought from a church to the museum climate during the last year and P5 remained for several years in a museum climate. Results on P1—-P2 climate verification showed that the change in the relative humidity environment varies between 63% and 70% in the dry season (summer). This means a variation of 7% in relative humidity between morning and afternoon, and the relative humidity should not fluctuate more than 10% in 24 hours. It has to be considered that this maximum value of 70% of relative humidity is the value from which it is agreed that the various objects of organic structure, especially painting, begin to change their dimensions, lose their original rigidity, becoming plastic and more vulnerable to the formation of fungus [6,7]. However, in the wet season (winter) an approximate relative humidity of 78%-83% was detected.