The utilization of Bacillus sp. for the production of bio-CaCO3 in concrete crack repair and strength enhancement has attracted considerable attention. However, microbial-induced calcium carbonate precipitation (MICP) has yet to be explored as a precedent with activated sludge. Here calcium sourced from concrete slurry waste (CSW) and carbon from sludge microbial β-oxidation under alkaline were used to generate micro/nano CaCO3. The results indicate that the main crystalline form of the generated precipitated particles is calcite, with a particle size ranging from 0.7 to 10 μm. Minimal heavy metals were found in the supernatant following settling. And at the optimum pH of 8.5–9, carbon capture reached 743 mg L−1, and CaCO3 production reached 1,191 mg L−1, and dominant phylum were Proteobacteria and Bacteroidota, with Thauera being a prevalent genus adept in β-oxidation. Mass balance analysis showed that alkali promotes microbial β-oxidation of organisms to produce CO2 and facilitate storage. Thus, the alkaline regulation of metabolism between microbe and CSW provides a novel way of sludge to initiate MICP.

  • Utilizing concrete slurry waste as a calcium source and sludge β-oxidation as a carbon source can successfully produce bio-CaCO3.

  • pH 8.5–9 is the optimal alkaline control for Thauera to be the dominant genus undergoing β-oxidation to produce CO2.

  • Bio-CaCO3 is a 0.7–10 μm calcite particle, which is an excellent material for repairing concrete.

  • There is no risk of heavy metal leakage during operation.

During the concrete production process, a large amount of concrete slurry waste (CSW) is generated, attributed to the washing of concrete trucks, dust reduction, and sphere cleaning operations. Characterized by a pH level exceeding 11.5, CSW is rich in calcium silicate (Xuan et al. 2016). CSW is classified as a corrosive hazardous substance. If disposed of in landfills, it would cause detrimental effects on our surrounding environment and ecosystems due to its high pH value. In addition, sedimentation and post-treatment processes lead to the accumulation of waste slurry particles, contributing to dust pollution in the concrete production environment and overlooking the potential recycling and utilization of significant mineral resources. However, the Chinese national standard (GB/T 14902-2012) mandates the recycling of CSW. Previous research has demonstrated that Bacillus sp. can utilize calcium sources in concrete to synthesize CaCO3 bio-nanoparticles, which are beneficial for repairing concrete cracks and filling pores (Qin et al. 2021b). Consequently, microbial-induced calcium carbonate precipitation (MICP) offers a viable alternative for the recycling of calcium resources in CSW.

CSW is recognized as a potential source of calcium carbonate. Upon introducing CO2 into the aqueous phase, up to 30% of calcium can be extracted from CSW, yielding CaCO3 with a purity exceeding 97% (Iizuka et al. 2012). However, CO2′s low water solubility constrains CaCO3 production (Hui et al. 2022). The adjustment of pH enhances CO2 capture, promotes production, and facilitates the generation of abundant CaCO3 nanoparticles. More importantly, bio-nano-CaCO3, synthesized by urease-producing bacteria and enriched from waste-activated sludge via the MICP method, has various applications including repairing concrete voids, cementing soil, improving soil strength, and suppressing coal dust in coal mines (Yang et al. 2020; Liu et al. 2022). Utilizing urease-producing bacteria to produce micro- and nano-CaCO3 from carbonized sludge and urine for the production of sustainable bio-cement has been explored (Yang et al. 2022). The use of Bacillus pasteurii to produce bio-CaCO3 has been demonstrated to enhance the strength of expansive soils (Tian et al. 2022). Sporosarcina ureilytica ML-2 produces bio-CaCO3 for treating waste sludge and immobilizing heavy metals (Zeng et al. 2023). Nonetheless, it is important to consider that using a single strain and adding calcium sources and urea to generate bio-CaCO3 can significantly increase the costs involved. Breaking down urea can lead to the excessive production and accumulation of ammonia nitrogen, which, in turn, can acidify the water and promote eutrophication (Kumar et al. 2023). There remains a lack of direct research on producing micro- and nano-sized biogenic CaCO3 (bio-CaCO3) using microbial communities from activated sludge and CSW. The biological metabolic mechanisms underlying MICP for nanoparticle production in CSW are not well understood, particularly the impact of pH on biochemical reaction pathways and alkalinity regulation.

For this, a comprehensive investigation was conducted on the system that harnesses CSW as a valuable resource through the bio-metabolism process of activated sludge. Additionally, the impact of pH on the efficiency of carbon capture and the production of CaCO3 was thoroughly examined. At varying pH levels, analyses were conducted based on the bacterial community structure, the relative cell count, and the proportions of polysaccharides and proteins produced. Scanning electron microscopy (SEM) was used to determine the particle size, while X-ray diffraction (XRD) was used to identify the composition and crystalline form of the products. Inductively coupled plasma mass spectrometry (ICP-MS) was employed to verify the heavy metal residues in the supernatant following sludge settling and CaCO3 precipitates. These findings offer novel insights into the recycling of CSW calcium resources and the generation of bio-CaCO3, potentially benefiting the early strength of concrete.

Materials

CSW was obtained from Shaanxi Future Venture Construction Technology Co., Ltd, Xi'an and stored at 4°C before use. Sludge, possessing an 80% moisture content, was procured from the No. 4 Wastewater Treatment Plant (WWTP). Chemical reagents for the experiments were procured from Sigma-Aldrich (MO, USA). Ca2+, pH, suspended solids (SS), and chemical oxygen demand (COD) were determined according to the following national standards (GB7476-1987), (GB11901-89) and (HJ828-2017). Results are presented in Table 1.

Table 1

Characteristics of CSW and the bioavailability of sludge pyrolysates

CSW (mg L−1)
Sludge pyrolysates (mg L−1)
pHCa2+SSCODCODBOD5BOD5/ COD
12–13.5 747.09 6,745 68 7,300 ± 100 4,492.5 ± 3.5 0.62 ± 0.005 
CSW (mg L−1)
Sludge pyrolysates (mg L−1)
pHCa2+SSCODCODBOD5BOD5/ COD
12–13.5 747.09 6,745 68 7,300 ± 100 4,492.5 ± 3.5 0.62 ± 0.005 

Preparation of carbon source for sludge pyrolysis solution

To better adapt microbes to the carbon source in actual wastewater, the hydrothermal pretreatment of sludge organisms was employed as a simulated carbon source. This process breaks down lipids into long-chain fatty acids and volatile fatty acids, and proteins into ammonia and volatile fatty acids (Qin et al. 2021c). There is minimal degradation of long-chain fatty acids in sludge subjected to 90 °C hydrolysis (Charuwat et al. 2018). Consequently, Table 1 shows the biochemical oxygen demand (BOD5) and COD during pyrolysis for 1 h at a pH of 11 and a temperature of 90 °C. The BOD5/COD ratio exceeding 0.6 indicates its bioavailability.

Operation of the bio-CaCO3 generation reactor

About 4 L of sludge microbes were introduced into an 8 L reactor. Intermittent aeration was performed at a rate of 7 L min−1 to maintain dissolved oxygen levels between 2 and 5 mg L−1. Mechanical stirring ensures the uniform distribution of sludge in the reactor. Furthermore, an automatic NaOH syringe pump was utilized to maintain an alkaline pH. The reactor is placed in a water bath system to ensure that a consistent temperature of 25 °C is maintained. Sludge pyrolysate was added to maintain an input COD of 300 mg L−1. The reaction cycle spanned 24 h, comprising 23 h of aerobic reaction. After that, there was 30 min of settling and the supernatant was then combined with CSW to produce nanoparticles, followed by 30 min dedicated to CaCO3 nanoparticle generation. The nanoparticle precipitates were enriched through centrifugation, with the supernatant subsequently discarded. The enriched precipitates were then dried and weighed. After the aerobic reaction, the supernatant following sludge settling was collected, and here and content were analyzed adhering to standards (DZ/T 0064.49—2021). Heavy metals, such as Cr, Cu, Zn, Cd and Pb, were measured in the supernatant following sludge settling and CaCO3 precipitates using ICP-MS (Thermo Fisher iCPA Q USA). Before measurement, the samples undergo acid dissolution treatment. In addition, to fully utilize the CSW and reduce operating costs, a reflux experiment was set up, which differs from the former in that the CSW reflux reactor, after generating calcium carbonate, provides alkalinity.

The generated nanoparticles were analyzed using SEM (SU-8082, Japan) to assess their structure and particle size. XRD analysis (Ultima IV, Japan) was employed to determine the composition and crystalline structure of the nanoparticles. Next-generation sequencing based on 16S rRNA was utilized to analyze the microbial community structure. Sludge microorganisms with pH ranges of 7.5–8.0, 8.5–9.0, and 9.5–10.0 were entrusted to Beijing Kinko Biotechnology Co for testing.

Fluorescence observation of proteins and polysaccharides in dyed sludge

The sludge was immersed in 10 g L−1 of fluorescein isothiocyanate isomer I (FITC) to stain proteins, then in 0.1 g L−1 of concanavalin A-alexa fluor (Con A) to label polysaccharides, and in 1 mg L−1 of 4,6-diamidino-2-phenylindole dihydrochloride (DAPI) to stain nucleic acids. Staining of the sludge was conducted by methodologies previously described (Chen et al. 2007; Yang et al. 2023). Subsequently, the samples were paraffin-embedded, sectioned using a microtome (Leica RM2126RT, Germany), and examined and imaged with a fluorescence microscope (Olympus BX61 + DP72, Japan). The excitation wavelengths for Con A, FITC, and DAPI were 555, 488, and 358 nm, respectively.

To confirm the reproducibility of the experimental results, all experiments were performed in triplicate. The graphs were drawn using Origin (OriginLab, USA, 2018). Values are expressed as mean values ± standard deviations. Image J (NIH, USA) was utilized to calculate the fluorescence area.

Effect of pH adjustment on carbon capture effectiveness and bio-CaCO3 output

In alkaline water, CO2 simultaneously exists in the forms of and (Qin et al. 2021a). With an increase in pH, progressively converts into . Conversely, with a decrease in pH, progressively transforms into , subsequently forming H2CO3 molecules. H2CO3, due to its instability, readily decomposes into H2O and CO2, subsequently escaping into the air. Consequently, pH plays a pivotal role in determining the efficiency of carbon capture. As illustrated in Figure 1 at a pH of 7.5–8, CO2 is present exclusively in the form of , reaching a maximum concentration of 250 mg L−1. During this phase, a considerable volume of CO2, generated via microbial β-oxidation, is released from the water into the air. Upon the pH reaching 8.5–9, CO2 continues to coexist in the forms of and . The combined concentration of and (carbon capture effectiveness) experiences rapid growth over 3 days, eventually stabilizing at 700–800 mg L−1. At pH ranging from 9.5 to 10, the carbon capture effectiveness can ultimately stabilize at approximately 1,000 mg L−1. During the pH elevation from 7.5–8 to 8.5–9 and subsequently to 9.5–10, the carbon capture effectiveness escalates by 193.7 and 34.6%, respectively. The maximum yield of CaCO3 rises from 415.8 to 1,190.7 mg L−1 and subsequently to 1,649.3 mg L−1, representing an increase of 186.3 and 38.5%, respectively. This suggests that the growth rate of the carbon capture effectiveness and the yield of bio-CaCO3 are significantly higher at a pH of 8.5–9 than at a pH of 9.5–10. Typically, for aerobic biological treatment, the pH is recommended to be between 6 and 9. An overly elevated pH can result in the death of some microorganisms, extend the adaptation period, or potentially inhibit microbial activity. Furthermore, with increasing pH, the supernatant of the reactor becomes increasingly turbid, adversely affecting the purity of the produced CaCO3. Moreover, a higher pH entails increased operational costs, and therefore, establishing a pH level of 8.5–9 is considered the optimal alkaline condition for producing bio-CaCO3.
Figure 1

Effect of pH 7.5–8 (a and b), 8.5–9 (c and d), and 9.5–10 (e and f) on carbon capture's effectiveness and bio-CaCO3 output (green for theoretical and orange for actual output).

Figure 1

Effect of pH 7.5–8 (a and b), 8.5–9 (c and d), and 9.5–10 (e and f) on carbon capture's effectiveness and bio-CaCO3 output (green for theoretical and orange for actual output).

Close modal
Figure 2

Effect of reflux (a and b) and no-reflux (c and d) way on carbon capture and bio-CaCO3 output (green for theoretical and orange for actual output).

Figure 2

Effect of reflux (a and b) and no-reflux (c and d) way on carbon capture and bio-CaCO3 output (green for theoretical and orange for actual output).

Close modal

As illustrated in Table 2, following the carbon source calculation resulting from the transformation of sewage organics into CO2, a mass balance pertaining to carbon transformation and capture has been established in reactors with a pH of 9.5–10. The conversion ratio of COD to CO2 has been derived from the existing literature (Bao et al. 2015). During this process, the CO2 concentration supplemented by air in aerobic aeration amounts to 1,467.79 mg L−1, markedly surpassing the carbon capture quantity of 148.63 mg L−1 in the control water and 726.31 mg L−1 in the bio-CaCO3 generation reactor. This demonstrates that a substantial portion of the CO2 entering the reactor during the aeration is released into the air. Additionally, the carbon capture quantity in the reactor exceeds the combined carbon of the control water and the incoming source. This implies that the alkali addition not only enhances the conversion of nearly all soluble COD into CO2 via bio-metabolism but also aids in dissolving some insoluble COD in the sludge pyrolysate, thereby enabling more efficient utilization by microbial aerobic respiration. In addition, an alkaline environment favors carbon capture. The alkali addition facilitates microbial carbon transformation, leading to CO2 production, which is advantageous for storing the generated CO2 in water.

Table 2

Carbon mass balance in the bio-CaCO3 generation reactor

Carbon of incomingCarbon of aerationCarbon capture in control waterCarbon capture in reactor
mgL−1 
291 ± 5.8 1,467.79 ± 23.82 148.63 ± 2.78 726.31 ± 8.75 
Carbon of incomingCarbon of aerationCarbon capture in control waterCarbon capture in reactor
mgL−1 
291 ± 5.8 1,467.79 ± 23.82 148.63 ± 2.78 726.31 ± 8.75 

The impact of reactor operational ways on carbon capture efficiency and bio-CaCO3 output

Owing to the high alkalinity of CSW, which exhibits a pH of 12–13.5 (Xuan et al. 2016), its return to the reactor following CaCO3 production can offer an alkaline environment, facilitating waste resource utilization and diminishing the operational costs of the reactor. As depicted in Figure 2(a) and 2(c), with pH levels of 8.5–9, the carbon capture effectiveness stabilized between 700 and 800 mg L−1 following 3 days of rapid increase. In the no-reflux approach, carbon capture effectiveness nearly peaked at 702.5 mg L−1 on the 2nd day, in contrast to a near peak of 742.6 mg L−1, while reflux reached only 591.2 mg L−1, suggesting a more expedited startup period. During days 3–8, reflux progressively increased from 704.3 mg L−1 to a maximum of 789.7 mg L−1. This increase is attributed to the additional minor carbon source from the reflux CSW (refer to Table 1), while the subsequent decline in carbon capture effectiveness is likely due to the inhibition of cellular respiration from accumulated heavy metals and salts (Hong et al. 2013; Ma et al. 2015; He et al. 2017). In the no-reflux reactor depicted in Figure 2(c), carbon capture effectiveness reached its apex at 742.58 mg L−1 on the 3rd day. Despite a minor decline from days 4 to 10, it remained relatively stable at 650–750 mg L−1, marginally lower than the reflux reactor. Figure 2(b) and 2(d) illustrates that under reflux and no-reflux operation way, the peak production of bio-CaCO3 was 1,376.4 and 1,204 mg L−1, respectively, aligning closely with theoretical projections. Reflux's CSW does not impact the efficiency of carbon capture or the production of bio-CaCO3. In addition, Figure 2(a) and 2(c) exhibits distinct peaks in levels and corresponding valleys in levels on day 5. This observed trend can be attributed to the bulking of sludge that occurred around day 5, coinciding with a sludge settling velocity of approximately 90% (refer to Figure S5). Consequently, certain microorganisms present in the bulking sludge experienced mortality in the highly alkaline environment, leading to the leaching of intracellular lipids. These lipids were subsequently converted into fatty acids (Wilson & Novak 2009), thereby contributing to the reduction in pH levels. Moreover, this conversion process also served as an additional carbon source for the system. In summary, for effective pH adjustment of the reactor and reduced operational costs, the adoption of the CSW reflux way is recommended, as it is more conducive to the production of bio-CaCO3.

Effect of pH on the distribution of microbial polysaccharides and proteins

pH exerts a significant influence on the protein and polysaccharide content in microorganisms (Yu et al. 2017). As evidenced in Figure 3, with an increase in pH, the absolute value of nucleic acids in the sludge microbial community rises, signifying a rise in microbial quantity. Under the premise that all samples have the same cell number in the field of view; to illustrate the relative content changes of proteins and polysaccharides, we utilized the fluorescence area of nucleic acids as a reference (blue). With an increase in pH, the area of nucleic acid continuously approaches 3,600 μm2 at pH 9.5–10, while the area occupied by proteins and polysaccharides both increased and then decreased, reaching approximately 2,100 μm2 at pH 8.5–9. The relative ratio of protein declines from 0.74 to 0.70 and ultimately to 0.52. This phenomenon may be attributed to β-oxidation of proteins, as the degradation of proteins into amino acids, subsequent deamination and decarboxylation, facilitates the formation of fatty acids that undergo β-oxidation. Conversely, the relative ratio of polysaccharides escalates from 0.42 to 0.72 with an increase in pH, subsequently decreasing to 0.49. The increase in polysaccharide content from pH 7.5–8 to 8.5–9 is attributed to the secretion of polysaccharides by microorganisms in response to the alkaline environment (Yu et al. 2017). Further increase in pH reduces the relative ratio of polysaccharides to 0.49, but it remains higher than 0.42 at pH 7.5–8. This could be due to the increased solubility of polysaccharides at higher alkalinity (Wang et al. 2022). In summary, as pH increases, the absolute value of nucleic acids in the sludge microbial community escalates, signifying a rise in microbial quantity. However, the relative ratio of protein per microorganism decreases, suggesting that β-oxidation metabolism of proteins occurs. The relative ratio of polysaccharides increases initially and then decreases. This increase occurs in response to the unfavorable environment at pH 8.5–9.
Figure 3

Effect of pH 7.5–8 (a), 8.5–9 (b), and 9.5–10 (c) on the distribution of microbial polysaccharides (red) and protein (green) composition.

Figure 3

Effect of pH 7.5–8 (a), 8.5–9 (b), and 9.5–10 (c) on the distribution of microbial polysaccharides (red) and protein (green) composition.

Close modal

Analysis of the microbial community structure of sludge at different pH levels

As depicted in Figure 4, at the phylum level, Proteobacteria, Bacteroidota, Patescibacteria, and Acidobacteriota emerge as dominant. With the increase in pH, the relative abundance of Proteobacteria consistently escalates from 47.29 to 77.20%, illustrating its adaptability to an alkaline environment. As the pH progresses from 7 to 9, Bacteroidota's relative abundance increases from 10 to 34%. Nevertheless, upon reaching a pH value of 10, its relative abundance diminishes to 14%. While Bacteroidota can thrive in mildly alkaline conditions at pH 9, it is intolerant to environments that exceed a pH of 9.5. Patescibacteria and Acidobacteriota exhibit a consistent decline in relative abundance with pH elevation, decreasing by 11 and 5%, respectively. At the genus level, Thauera dominates at pH 8.5–9, while Brevundimonas prevails at pH 10, with peak relative abundances of 14 and 16%, respectively. Thauera bacteria, which are prevalent in diverse wastewater denitrification systems, facilitate the removal of nitrogen and phosphorus through denitrification. With the pH elevation from 9 to 10, Thauera's relative abundance diminishes from a leading 14–7%, reflecting its preference for moderately alkaline rather than highly alkaline conditions. Furthermore, Thauera is capable of producing polyhydroxyalkanoate facilitated by the acetyl coenzyme A gene (Andreolli et al. 2022; Raunhan et al. 2023), establishing it as a key genus in β-oxidation at pH 8.5–9. Zoogloea is critical for the settling performance of activated sludge (An et al. 2016). The absence of Zoogloea in environments with pH levels ranging from 8.5 to 9 and 9.5 to 10 poses some inconvenience in the production of bio-CaCO3. In conclusion, Proteobacteria and Bacteroidota, at the phylum level, are predominant in bio-CaCO3 production, while, at the genus level, Thauera, proficient in β-oxidation, excels in bio-CaCO3 production at pH 8.5–9. Correspondingly, Zoogloea's limited viability in alkaline results in ineffective sludge settling and turbid supernatant.
Figure 4

Different pH impact on the microbial communities at the phylum (a) and genus (b) level.

Figure 4

Different pH impact on the microbial communities at the phylum (a) and genus (b) level.

Close modal

Analysis of bio-CaCO3 using SEM and XRD

Figure 5 illustrates that bio-CaCO3 predominantly exhibits a sphere shape, with diameters predominantly in the 0.7–10 μm range, to some extent to the nanometer scale. Owing to their diminutive size, these micro-/nano-sized calcium carbonate particles demonstrate superior dispersibility, markedly enhancing the potential for crosslinking with other materials (Boyjoo et al. 2014). Consequently, micro-/nano-sized calcite-type calcium carbonate emerges as an exemplary material for repairing concrete cracks and augmenting its mechanical properties (Cui et al. 2021). CaCO3 exists in three crystalline forms: calcite, aragonite, and vaterite, with calcite being the most thermodynamically stable. Furthermore, its considerable strength facilitates compatibility with cementitious materials. Figure 5(c) depicts an XRD analysis of the products that are predominantly composed of calcite CaCO3, with trace amounts of Al1Si143N191O1 and KCl. Al1Si143N191O1 is likely derived from cement and its hydration products, whereas Cl is sourced from the dilute hydrochloric acid utilized for pH adjustment in the CSW. Similar to cement, calcite CaCO3 boasts effective sand consolidation properties, and its non-permeable calcite layer offers corrosion protection for steel reinforcement (Ramachandran et al. 2001; Achal et al. 2013; Iswarya & Adalarasan 2020). In conclusion, the synthesized micro-/nano-sized CaCO3 crystals, which are calcite type and highly pure, are well suited for use as concrete repair and reinforcement materials.
Figure 5

SEM analysis (5,000× for (a) and 10,000× for (b)) and XRD characterization of bio-CaCO3 (c).

Figure 5

SEM analysis (5,000× for (a) and 10,000× for (b)) and XRD characterization of bio-CaCO3 (c).

Close modal

Assessment of heavy metal leaching after sludge settling and CaCO3 precipitation

Activated sludge is known to contain heavy metals such as Pb, Cr, Cd, Ni, Zn, and Cu (Dewil et al. 2007), while CSW may accumulate Pb, Cr, and Cd (Xuan et al. 2016). Consequently, assessing the risk of heavy metal leaching during the reactor operation is crucial. Given that activated sludge can immobilize heavy metals, mainly through adsorption from surface functional groups, most residual heavy metals in CSW are likely to be adsorbed by the sludge and eliminated through sedimentation and discharge (Commenges-Bernole & Marguerie 2008; Ramrakhiani et al. 2016; Zhou et al. 2016). ICP-MS analysis (Table 3) reveals negligible amounts of Cr, Cd, and Pb in the supernatant following sludge settling in the no-reflux way, with Zn below 20 μg L−1 and Cu at 36.20 μg L−1. These low concentrations of metal ions should be absorbed by the sludge microbes and removed from the reactor by increasing the hydraulic retention time (HRT) and reducing the sludge retention time (SRT). In the reflux way, concentrations of Cr, Cd, and Pb following sludge settling are negligible in the supernatant. Post-day 9, Zn levels in the supernatant following CaCO3 precipitation drop to just 0.05 μg L−1. A contrast to 5.59 ± 0.28 μg L−1, seen following sludge settling, suggests minimal Zn incorporation into bio-CaCO3. The supernatant after sludge settling still contains a significant concentration of Cu, with levels reaching as high as 53.51 μg L−1. It is worth noting that this concentration falls significantly below the groundwater quality standard (GB/T 14848-2017) stipulated by the Chinese national standard. However, the concentration of Cu in the supernatant significantly decreases to only 19.10 μg L−1 after CaCO3 precipitation. These findings indicate a limited uptake of Cu into the bio-CaCO3. This could be attributed to the mixing of CSW and sludge supernatant in approximately a 1:1 ratio during the production process of CaCO3, resulting in the Cu concentration in the supernatant after CaCO3 precipitation being approximately half that present in the supernatant after sludge settling. Based on this, it can be inferred that the mobility of Cu bound within the activated sludge solution is restricted.

Table 3

Analysis of residue metal in the supernatant after bio-CaCO3 generation

CrCuZnCdPb
Reflux (μg L−1
9th day After sludge settling 0.88 ± 0.02 36.58 ± 0.74 5.87 ± 0.23 0.15 ± 0.01 0.24 ± 0.03 
After CaCO3 precipitation 3.33 ± 0.09 21.71 ± 2.38 0.05 0.14 ± 0.28 0.43 ± 0.27 
10th day After sludge settling 1.01 ± 0.78 53.51 ± 3.75 5.31 ± 0.55 0.12 ± 0.09 0.13 ± 0.02 
After CaCO3 precipitation 2.85 ± 0.45 19.10 ± 2.34 0.05 0.17 ± 0.08 0.50 ± 0.24 
No reflux (μg L−1
9th day After sludge settling 0.05 36.2 ± 3.48 17.4 ± 2.65 0.05 0.05 
After CaCO3 precipitation 0.05 35.3 ± 2.27 10.4 ± 0.94 0.05 0.05 
CrCuZnCdPb
Reflux (μg L−1
9th day After sludge settling 0.88 ± 0.02 36.58 ± 0.74 5.87 ± 0.23 0.15 ± 0.01 0.24 ± 0.03 
After CaCO3 precipitation 3.33 ± 0.09 21.71 ± 2.38 0.05 0.14 ± 0.28 0.43 ± 0.27 
10th day After sludge settling 1.01 ± 0.78 53.51 ± 3.75 5.31 ± 0.55 0.12 ± 0.09 0.13 ± 0.02 
After CaCO3 precipitation 2.85 ± 0.45 19.10 ± 2.34 0.05 0.17 ± 0.08 0.50 ± 0.24 
No reflux (μg L−1
9th day After sludge settling 0.05 36.2 ± 3.48 17.4 ± 2.65 0.05 0.05 
After CaCO3 precipitation 0.05 35.3 ± 2.27 10.4 ± 0.94 0.05 0.05 

Furthermore, the supernatant following CaCO3 precipitation in the reflux way contained slightly more heavy metals than that in the no-reflux way. This increase is potentially attributed to the salt accumulation within microbial cells due to the reflux of the supernatant in the reactor, which inhibits biological activity and diminishes the subsequent adsorptive ability of heavy metals (Hong et al. 2013; He et al. 2017). Nevertheless, these heavy metal concentrations remain well below the thresholds established by the comprehensive sewage discharge standard (GB8978-1996). In summary, the reflux way results in concentrations of Cr, Cd, and Pb in the supernatant that are below 3 μg L−1, while Cu and Zn are somewhat higher, reaching maximum values of 53.51 and 17.4 μg L−1, respectively. By increasing the HRT and reducing the SRT, these heavy metals can be primarily concentrated within the sludge microbes and effectively removed from the system.

Utilizing CSW as a calcium source and sludge β-oxidation products as a carbon source enabled the successful production of bio-CaCO3 under alkaline conditions. The sludge pyrolysate, as a simulated COD, has a BOD5/COD ratio that exceeds 0.6 with good biodegradability.

The ideal pH for CaCO3 production was determined to be 8.5–9, achieving a maximum carbon capture of 742.6 mg L−1 and a CaCO3 yield of up to 1,190.7 mg L−1. Mass balance analysis indicated that the addition of alkali enhances microbial β-oxidation, which degrades COD to produce CO2 and aids in CO2 storage. In addition, the reflux of supernatant in the reactor, providing an alkalinity environment and reducing costs, is recommended. As the pH value increases, the number of microorganisms increases. Concurrently, a decrease in the relative protein content per microorganism was observed, suggesting that protein plays an important role in β-oxidation. Here, polysaccharides initially increase the relative content, followed by a decrease, with the elevation at pH 8.5–9, which serves as an adaptive response to adverse conditions. Simultaneously, Proteobacteria and Bacteroidota emerge as dominant phyla, with Thauera being a prevalent genus adept in β-oxidation. SEM disclosed that the majority of CaCO3 precipitate particles exhibit a sphere shape, with a size of 0.7–10 μm in the range. XRD analysis demonstrated that the primary crystalline form of the precipitate is calcite. ICP-MS analysis indicated minimal heavy metal in the supernatant following sludge setting, and these trace heavy metals could be further removed by sludge discharge.

This methodology presents a novel strategy for waste sludge minimization, CSW reclamation, and the generation of bio-CaCO3. The micro-/nano-bio-CaCO3 production has a promising future, which can be used for concrete crack repair and strength enhancement. The discovery of alkaline regulation has expanded the application of MICP in CSW. Nevertheless, as there may be residual organic matter in the production process of bio-CaCO3, further investigation is warranted to confirm the durability and mechanical properties of concrete integrated with this form of CaCO3. The new operation should involve feeding a small amount of CSW into the reactor to maintain pH and continuously produce bio-CaCO3 for slurry recharge in concrete. Furthermore, it is important to investigate whether the existing CaCO3 in the CSW may agglomerate during prolonged placement, which will influence the particle size of MICP bio-CaCO3.

This work was financially supported by the Natural Science Foundation of China (Grant No. 51808044) and the Qinchuangyuan ‘Scientist + Engineer’ Team Construction Project of Shaanxi Province (2022KXJ-119). Supplementary data associated with this article can be found in the online version.

Jinbo Zhao: conceptualization, writing – original draft, writing – review and editing, methodology, software. Jiacheng Feng: data curation, writing – review and editing, methodology, visualization. Yifan Du: formal analysis, investigation, writing – review and editing. Zhiyang Yan: methodology, supervision, resources, writing – review and editing. Xiaoguang Li: conceptualization, project administration, writing – review and editing. Jinyi Qin: conceptualization, validation, funding acquisition, project administration, resources. Ming Su: supervision, validation. Min Yang: supervision, writing – review and editing.

Data cannot be made publicly available; readers should contact the corresponding author for details.

The authors declare there is no conflict.

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