3.3.1. Effect of BBC Mortar on Water Permeability in Different Curing Periods
The evaluation of mortar quality is necessary for service life and proper maintenance. In terms of durability, the permeability of mortar is the most important of its performance. Penetration of liquids and gases such as carbon dioxide, chloride ions, and water are the primary causes of harmful effects in mortar. The pore structure of the mortar governs its penetration into the mortar. Thus, water permeability can indicate the ease with which liquid can penetrate the mortar. In this investigation, the resistance of BBC mortar was tested by penetrating deleterious elements. The purpose was to determine the efficiency of BBC mortar to resist environmental conditions. The effects of BBC mortar on water permeability were evaluated in terms of the water permeability coefficient. The water permeability of NC and BBC mortar in different curing media is shown in
Table 8 and the water permeability of the BBC mortar effect is plotted in
Figure 7.
The water permeability of BBC mortar using various curing media was compared to NC mortar cured with the same curing media. The results showed that the water permeability of BBC significantly dropped in 7 days, slowly decreased to 28 days after the water exposure, and remained constant afterward. As described in
Table 11,
Table 12,
Table 13, the permeability decreased as the curing time increased in all curing media for both samples, with different reduction percentages. The respective reduction in water permeability coefficient of BBC mortar cured in distilled water (D.W.) for 3, 7, 28, 56, and 90 days was 14.2%, 31.6%, 33.3%, 37.5%, and 39.1%. The samples cured in deposition medium (D.M.) and run-off water (R.W.) had a very positive effect on water permeability at an early stage, short term, and long term, where the coefficients of water permeability were decreasing in the range of 19.9–25.7%, 34.2–50.7%, 33.3–37.7%, 41.9–56.6%, and 51.4–60.9%, after 3, 7, 28, 56, and 90 days, respectively. It is noticeable that with prolonged curing time, there was a significant decrease in the coefficient of water permeability of the mortars.
Figure 7 illustrate the reduction in permeability of BBC mortar due to the curing period and different curing media. The bacterial metabolic activity produced calcite, which clogs the surface pores, decreasing water permeability. Similarly, as discussed earlier, sufficient nutrients during the bacterial metabolic activities precipitate the CaCO
3, which fills and reduces mortar pores, causing blockage of the water penetration path [
37,
38,
39].
3.3.2. Effect of BBC Mortar on Water Permeability in Different Curing Media
The coefficient of water permeability of BBC mortar in various curing media is shown in
Figure 8. Curing media application directly affected water permeability. Compared to D.W. media, D.M. and R.W. media exhibited a positive water permeability coefficient of BBC mortar at the early stage, short-term, and long-term. Different curing media with different nutrients affected the characteristic of water permeability of BBC mortar. Water permeability coefficients obtained after the 90-day curing period were 1.54 × 10
−12 m/s for BBC-DM, 1.17 × 10
−12 m/s for BBC-RW mortar, and 1.85 × 10
−12 m/s for BBC-DW mortar. Therefore, D.M. and R.W. curing media had the highest water permeability reduction.
In conclusion, using a self-healing agent in cement mortar reduces its permeability. Self-healing occurs after a certain period due to sufficient nutrients for BBC mortar samples. This advantageous effect depends on the amount of CaCO3 precipitation relating to bacterial metabolic activities. The bacteria with higher ureolytic and carbonatogenesis activity curing in media containing nutrients produce more CaCO3 to fill the pores. Self-healing performance improves significantly after seven days of curing, possibly due to additional hydration of the un-hydrated cementitious components. Thus, more precipitation is possible in the early stage as more voids are present, which enhances the minerals and media reactions to produce CaCO3.
3.3.3. Microstructure and Composition
Energy-dispersive X-ray spectrometry (EDX) was used to quantitatively determine the elements with atomic numbers. Using scanning electron microscopy (SEM) for microstructure analysis on BBC mortar with different curing media, selected specimens were compared using scanning electron microscopy (SEM).
Figure 9 shows the surface of BBC mortar specimens with the presence of carbonate crystals after being subjected to different curing media.
Figure 9a shows SEM images of BBC mortar cured in distilled water. The SEM magnification was set between 100 and 20,000 times. SEM could clearly observe the whitish precipitates or organic material through the mixture on sample surfaces. Immobilized
Bacillus sphaericus precipitates were probably an organic compound due to their high organic carbon content. Main elements such as calcium (Ca) 21.91%, oxygen (O) 46.02%, silica (Si) 12.63%, carbon (C) 15.32%, aluminum (Al) 2.74%, and magnesium (Mg) 1.38% were determined through EDX analysis.
Figure 9b shows SEM micrographs of BBC mortar surface particles cured in a deposition medium. The formation of white lumps on the surface was evident, indicating calcite compounds. These new materials, calcite precipitates of BBC mortar rich in organic carbon, filled the pores in the cement matrix. These highly potential nutrient-derived compounds were urea, yeast extract, and calcium nitrate. The formation of these compounds is expected to enhance the strength gained from the
Bacillus sphaericus activity. From the previous studies by Norfaniza et al. [
43], the results are supported by the determination of primary elements, namely calcium (Ca) 45.7%, oxygen (O) 35.48%, silica (Si) 8.22%, carbon (C) 7.86%, aluminum (Al) 11.87%, and magnesium (Mg) 0.87% through EDX analysis.
Figure 9c illustrates a large variety of crystal layers on the BBC mortar surface cured in R.W. Two main shapes of crystalline CaCO
3, namely lamellar rhombohedral and needle-like shapes, were visible on the SEM images. The former shape produces the most stable characteristic of calcium carbonate in calcite [
44]. Meanwhile, the latter was a vaterite type, a metastable form of calcium carbonate [
45]. The absorption of organic and inorganic matter inhibited or altered the crystal growth to certain crystallographic planes of the growing crystal. In addition, crystal morphology differences were probably due to the actual urease activity levels linked to cell activity.
The existence of several crystal types proved the carbonate precipitation of bacterial mediation. The density and strength of the particles can be observed due to the interlocking arrangement of calcite materials. The CaCO
3 precipitate can be observed based on bacteria activity in certain curing media. The results show that
Bacillus sphaericus assisted calcite precipitation in mortar specimens [
46]. EDX analysis supported evidence that the main elements obtained were calcium (Ca) 49.62%, oxygen (O) 32.24%, silica (Si) 9.07%, carbon (C) 6.32%, aluminum (Al) 1.95%, and magnesium (Mg) 0.80%. In conclusion, BBC mortar in R.W. curing media produced more CaCO
3 precipitates than other curing media.
The direct influence of curing media on the amount of calcite precipitation on the surface was very significant, as observed by the SEM micrograph. The results were proven quantitatively by the elements with an atomic number through EDX analysis. BBC mortar in D.M. and R.W. curing media had faster biomineralization than in D.W. The biomineralization that occurred in D.W. was caused by the dissolution of pore solution at atmospheric CO2 and CaCO3 formation from portlandite. However, biomineralization in D.M. and R.W. occurred through microbiology hydrolysis of urea using an external nutrients supply from calcium ions, producing carbonate ions.
Biomineralization is technically a two-component coating system with pore-blocking capabilities [
12]. The incorporation of
Bacillus sphaericus resulted in pores plugging, as evident from water absorption analysis and CaCO
3 formation on the surface. The biological process of calcite formation occurred in a supersaturation condition caused by nutrient supply. Heterogenous CaCO
3 precipitation occurred in the internal pores as specimens were exposed to the solution [
13]. The presence of carbonate crystals on the surface, especially inside the porous matrix, decreased the permeability of BBC mortar.
The MICP procedure was used to identify and categorize the mineralogical changes brought on by the various curing mediums. Furthermore, the mineralogical alterations of BBC and any newly produced mineral due to the different curing media were determined by X-ray diffraction (XRD).
Figure 10 depicts the results of a series of XRD analyses performed to investigate the cement matrix’s mineralogical modification and compound formation in response to exposure to various curing conditions. Different curing media did not appear to add a new peak to the XRD spectrum of BBCM, and they did not alter the peaks’ characteristics of the two theta scales or their relative positions. The results demonstrated the efficiency of various curing media in maintaining the pozzolanic reaction during hydration and the lack of inorganic material in the curing media.
The existence of two prominent peaks, at 18.1° and 23.3°, verified the production of ettringite, which is typically caused by the interaction of C
3A with gypsum in the presence of CaCO
3 during the earliest stage of setting. All samples showed ettringite production, although the BBCM-DM had the most pronounced peak. There was a less prominent peak in the BBC-DW and BBC-RW. The free hydroxyl ions present in the cement matrix after curing in D.M. created a conducive environment for ettringite production [
8]. There were several prominent primary peaks at two theta scales of 21°, 26.8°, 29.5°, 39.2°, 48.4°, 50.1°, and 60° in XRD spectra, indicating the presence of calcite. The strain’s effectiveness in the precipitation of CaCO
3 by producing carbonate ions and using calcium ions was demonstrated by a notable rise in the strength of peaks attributable to calcite for the BBC matrix cured in RW. Minimal calcite precipitation and CH production were observed in the XRD spectra for D.W. curing. X-ray diffraction analysis showed that nutrients played a significant role in cement mortar. D.M. and R.W. curing media appeared more efficient than the others at transforming CH into C-S-H and CaCO
3. The ability of the strain to precipitate a high amount of CH at 27.7°, 40.4°, and 47.2° in the presence of D.M. and R.W. was indicative of the usual reactive chemistry that prevailed in the cement mortar, suggesting that there was enough buffer to facilitate further hydration of the cement.