3.1. Physical and Chemical Characteristics of Lime and Dregs
Based on the obtained particle size distributions (
Figure 3), it can be stated that the dregs have relatively fine granulometric properties with a unimodal distribution. The size distribution of these particles is very similar to that of lime, thereby allowing for the replacement of its fraction in the cement composite without modifying the pore distribution of the mortar. Since only a fraction of lime was substituted in this research, it is unlikely that the small difference between the granulometric curves changed the properties of the composite. Accordingly, Melo and co-workers [
24] studied the production of lime with calcium-rich biomass ash and reported concentrations of 0.1% and 4% of materials retained in sieves with openings of 0.6 mm and 0.074 mm, respectively. Based on the pulp-and-paper production process, the small particle size attributed to the dregs can be ascribed to the presence of impurities, such as Na
2O, MgO, and SiO
2, which may have been incorporated into the dregs in the recovery of white liquor. Such a unimodal pattern and small average particle size have already been reported in the literature [
25,
26]. According to Novais and co-workers [
26], the granulometry of ground dregs is similar to that of typical mortar pozzolans, such as metakaolin and fly ash.
The levels of loose unit mass, compacted unit mass, and specific mass (
Table 8) are within the limits reported in the literature for similar materials. Maheswaran and co-workers [
27] studied a material they called lime mud, which appears to be equivalent to dregs since it comes from the recausticizing of green liquor. The authors observed density and specific mass values of 0.616 g/cm
3 and 2.381 g/cm
3, respectively, with a moisture content of 52% and 85–90% of the material passing through a 40 μm sieve. It is important to note that the dregs were dried and ground in the present study, unlike the study by Maheswaran and co-workers [
27], which explains the differences between the granulometries. Moreover, Moreira and co-workers [
28] carried out a study on the incorporation of dregs in the clinker for the production of Portland cement and performed the drying, milling, and sieving of the residue, resulting in a specific mass of 2.44 g/cm
3 for a surface area of 1.03 m
2/g and a fineness index of 0.78%.
The diffractogram of the studied dregs (
Figure 4) indicates the presence of a predominant phase of calcite (CaCO
3), which was expected due to the origin of the material; however, along with the presence of calcium ions, contamination from lignin was observed. Similarly, Santos and co-workers [
25] found CaO within the dregs employed in their study, as it was the only compound to form crystalline phases and, therefore, easily detected in the X-ray diffractogram. According to the literature, the CaO content in dregs varies between 30 and 70% [
25,
27,
28,
29]. In addition, some studies reported levels of SiO
2 and SO
3 above 5% [
25,
27,
28]. Several studies also indicated small traces of dolomite (CaMg(CO
3)
2) and cesanite (Ca
2Na
3(SO
4)
3(OH)) in addition to peaks indicating quartz (SiO
2), sodium carbonate (Na
2CO3), pyrsonite (CaNa
2(CO
3)
2.2H
2O), magnesium oxide (MgO), wustite (FeO), and calcium hydroxide (Ca(OH)
2) [
25,
26,
27,
28,
29]. As in the work conducted by Santos and co-workers [
25], in the present study, none of these crystalline structures were identified in the XRD spectra.
Typical compositions of the conventional building materials used in the present study were confirmed (
Table 9). In this regard, it is important to note that the equipment used in this study does not detect the presence of certain elements, including carbon, hydrogen, and oxygen, which certainly conditioned the results obtained. However, the dominant presence of calcium in the lime and cement was verified, as well as the presence of silicon in the sand, which is in accordance with the literature [
24]. The composition of the dregs also presented expected characteristics and was similar to that verified for lime, indicating that the partial replacement of lime by dregs is promising.
Figure 5 shows the FTIR spectra obtained for dregs and lime. The signals at 710–715 cm
−1 (in-plane bending vibration of CO
32− ions), 870–875 cm
−1 (out-of-plane bending vibration of CO
32− ions), 1470 cm
−1 (asymmetrical vibration deformation of CO
32− ions), and 1800 cm
−1 (stretch vibration of C=O bonds) are typically reported for dregs in the literature [
30]. The absence of bands in the range between 1070 cm
−1 and 1080 cm
−1 confirms that calcium carbonate was present in the form of calcite since the bonds representing this compound are inactive with respect to infrared radiation due to the symmetry of the calcium crystals [
25]. The strong band in the region of 3300–3900 cm
−1 observed for lime is associated with the vibration of OH bond stretching and indicates the presence of Ca(OH)
2 [
31].
Regarding the thermogravimetric analysis of dregs and lime,
Figure 6 shows a relatively stable pattern of their mass levels throughout the heating tests up to a temperature of 300 °C. Thus, fluctuations in the mass levels of these materials can be attributed to noise or inaccuracies of the equipment. Starting at 700 °C, the mass of the dregs decayed at an intense and constant level until 800 °C. Lime, on the other hand, showed this behavior between 300 and 400 °C and again between 600 and 700 °C. The 5–10% loss of the initial mass of the dregs occurring up to around 200 °C can be attributed to the water physically adsorbed in the material in addition to the dehydration of CaSO
4 [
28]. Afterward, between 300 °C and 500 °C, an exothermic event occurred, which was likely related to the burning of organic compounds [
32]. Between 500 °C and 800 °C, the observed thermal decomposition of the material may be associated with the decomposition of CaCO
3 and MgCO
3 [
28]. In this regard, it is normal and expected that some elements verified in the dregs from other studies are not identified in the material analyzed in the present study since it is a heterogeneous residue originating from an industrial process with many variations, especially with respect to a comparison between waste from different industries. Between 800 °C and 1000 °C, the dregs experienced a mass loss of approximately 30%, which was probably related to the decomposition of calcium carbonate or calcite (CaCO
3), which transforms into CaO and CO
2 [
27,
28].
3.2. Physical Properties in Fresh and Hardened State
The specimens’ density in the fresh state (
Figure 7a) did not show variation upon the comparison of the types of mortar in this study (0.03% reduction rate), which may be attributed to the density of the dregs and lime being very similar. Regarding the incorporated air content (
Figure 7b), there is no clear pattern of variability as a function of the content of added dregs; therefore, the similarity (3.96% reduction rate) between the average values indicates that the insertion of dregs did not confer any difference in rheological mechanisms that favored the formation of bubbles during the mixing of the mortar components and the consequent presence of pores filled with air. This similarity was desired since incorporated air may enhance the workability of the paste; however, an increase in its content possibly represents a decrease in mechanical properties. All the composites studied showed a density in the fresh state between 1800 and 2200 kg/m
3 and can be classified in the same class according to NBR 13281 [
33] (D5 group), which determines the requirements for the application of coating mortar on walls and ceilings.
Similar to the fresh-state physical properties, the water absorption (0.92% reduction rate), void ratio (0.81% increase rate), and density in the hardened state (0.02% reduction rate) (
Figure 8) of the specimens do not seem to differ when comparing the mortar specimens under study. This behavior is due to the aforementioned similarities between the dregs and the lime, including their density, granulometric characteristics, and chemical composition. The densities of the mortar specimens in the hardened state achieved the limits between of 1600 to 2000 kg/m
3 and can be classified in the same class according to NBR 13281 (M5 group) [
33].
Furthermore, the water absorption via the capillarity coefficient increased (maximum 25.29% increase in 20% dregs) as the content of dregs increased (
Figure 9). However, it is known that the phenomena related to capillarity are different when comparing mortar produced with and without hydrated lime [
16,
17,
34]. In this sense, Marvila and co-workers [
35] affirm that lime acts similarly to sand in relation to capillarity, increasing the absorption coefficient. When lime is used as a binder, capillarity cannot be fully explained based on the porosity of the mortar and the presence of capillary pores [
17,
34]. However, even though an increase in the capillarity coefficient was achieved with the use of the dregs, all the types of mortar studied presented a capillarity coefficient greater than 10 g/dm
2/min
2 and can be classified in the same class according to NBR 13281 (C6 group) [
33], which is a high level of capillarity. This capillarity can reduce the useful life of the mortar due to the carrying of aggressive agents, however, it can allow the entry of CO
2 (CO
2 capture) and increase the mortar’s mechanical resistance due to carbonation [
34].
3.3. Mechanical Properties
When comparing the mortar specimens at 28 and 56 days old, the results (
Figure 10) indicate higher levels of compressive and flexional strength for the 56-day-old mortar specimens. These results were expected and can be attributed to the increase in the hydration level of the employed Portland cement in later ages. Furthermore, according to Bella and collaborators [
36], mortar specimens composed of lime usually have relatively low levels of resistance for up to 56 days, as this resistance depends on the level of carbonation. This carbonation depends on the temperature of the environment, the moisture content in the pores of the mortar, and the concentration of CO
2 in the atmosphere to which the mortar is exposed [
36]. Regarding the addition of dregs, the levels of compressive strength and flexural strength showed a stabilization trend after 28 days. These results again confirm the role of dregs as an agent capable of imitating the role of lime in mortar.
In addition, the pull-out strength obtained in this study was higher than those reported in recent research [
37,
38]. According to Silva and co-workers [
39], the performance of mixed mortar specimens is superior to that of mortar entirely composed of pure cement or pure lime binders. The adhesion of the mortar is afforded by the penetration of the binder paste in the pores and the roughness of the substrate, wherein water retention capacity, consistency, air content, and mechanical strength are factors that interfere with adhesion [
40]. Since the mortar specimens with and without dregs are very similar in terms of these properties, there were no differences between the studied mortar specimens (
Figure 11). Regarding the classification of the mortar specimens with respect to this property according to the current standards, all groups converged toward the highest resistance class (A3) [
33].
3.4. Mortar Specimens’ Chemical and Microstructural Properties
The chemical elements detected using X-ray fluorescence (XRF) via energy dispersive spectroscopy (EDX) for the studied mortar specimens are shown in
Table 10, and their respective spectra are presented in
Figure 12. Regarding the spectra, the detected peaks indicate the presence of typical cement compounds (Ca and Si), which are associated with hydrated silicates such as tricalcium silicate and dicalcium silicate [
26,
41]. There were also significant amounts of Fe and K present, which were associated with tetracalcium iron aluminate and potassium hydroxide, respectively [
41].
Although the elemental compositions of the mortar specimens were strongly affected by the selection of material for analysis, it is possible to observe a reduction in the content of Ca and Fe in addition to an increase in the Si content as a consequence of the incorporation of sand and dregs. These results are relevant since the fractions of CaO and Fe
2O
3 are approximately 40–50% and 0.5–1%, respectively, according to the literature [
29]. These fractions are lower when compared to mortar without the addition of dregs. Accordingly, it is not possible to attribute any difference in composition in terms of the content of dregs incorporated in the mortar specimens. However, the increase in the Si content attributed to the replacement of lime by dregs again indicates the presence of impurities, such as SiO
2, which was mentioned previously in this research.
The aggregate/matrix interface was similar in terms of porosity, and typical compounds (Portlandite and CSH) were visualized (
Figure 13). The similarity between the groups corroborates the mechanical properties and durability indicators, for which no significant variation was identified. In fact, it is known that the interfacial transition zone is the weakest region of a cementitious composite [
42], and, as there was no change, this had an impact on the non-alteration of mechanical properties and durability between the different groups, regardless of the percentage of substitution.
Regarding the hydrated compounds in the cement matrix, once analyzed in the broken section, it was found that calcium hydroxide (Portlandite) was found in the samples at 10, 15, and 20%, and 30% of dregs (
Figure 14 and
Figure 15), while Ref. did not detect Portlandite in the image. It is noteworthy that calcite (CaCO
3) morphologies (
Figure 15) were found in both samples.
In general, it can be considered that the microstructure of Portland cement composites is marked by the formation of pores in the interfacial regions between the fine aggregate and the cement.
Figure 13,
Figure 14 and
Figure 15 confirm the presence of these pores, confirming the growth trend as the dregs content increased. In addition. it can be stated that the presence of dregs did not reduce the formation of hydrated calcium silicate crystals (C-S-H), which determine most of the physical and mechanical properties of Portland cement composites.
Correlating with mechanical properties, adhesion occurs by the mechanical interlocking of the cement hydration products (ettringite and CSH) transferred to the pores of the substrate. Ettringite (3CaO.Al
2O
3.
3CaSO
4.
32H
2O–hydrated calcium trisulfoaluminate) has a long, narrow rod shape of approximately 4–5 µm (
Figure 14 and
Figure 15). It represents 20% to 25% of the volume of solids in a fully hydrated slurry [
17,
34,
43]. The precipitation of ettringite is initiated when Portland cement is mixed with water, wherein gypsum is used as a regulating source of the cement setting time dissolving and releasing sulfate and calcium ions; these ions are the first to enter the solution, followed by aluminate and calcium ions from the dissolution of C
3A in the cement.
Due to the suction or capillary absorption effect induced by the porous base, relevant ions in the solution are transported to more internal regions of the substrate, where they form hydrated calcium trisulfoaluminate (ettringite) inside the pores [
44]. Due to the faster dissolution processes of SO
42−, AlO
4−, and Ca
2+ ions and ettringite precipitation, this product primarily fills capillary pores, which explains its greater abundance in the mortar/substrate contact zone and the surface pores of the base [
17,
43]. CSH, on the other hand, has a morphology that varies from poorly crystalline strands to a crystalline lattice (
Figure 14 and
Figure 15). This phase constitutes about 50% to 60% of the solid volume of the fully hydrated pulp [
17,
34,
43]