1 Introduction
During the long-term service of soil structures, water-induced erosion frequently poses a significant challenge [
1]. However, conventional soil stabilization techniques often struggle to achieve a balance between reinforcement effectiveness, ecological sustainability, and minimal environmental disturbance [
2]. Therefore, it is imperative to adopt new efficient measures to enhance the workability of soils, especially their strength and slaking resistance [
3–
5]. To address this technical challenge, microbial mineralization was proposed and has emerged as a promising biogeotechnical solution [
6,
7]. This technique catalyzes the hydrolysis of urea through enzyme or enzyme-producing bacteria, producing
that react with Ca
2+ to precipitate CaCO
3, which acts as a bonding agent between soil particles [
8,
9]. Actually, the precipitated CaCO
3 exists in soils in three modes: cementation mode, coating mode, and pore-filling mode [
10]. The cementation mode refers to CaCO
3 preferentially forming at particle contact points to enhance structural integrity, as well as the coating mode involves gradual accumulation of CaCO
3 on particle surfaces, which may further evolve into the cementation mode. Therefore, promoting the preferential deposition of CaCO
3 at particle contacts and on particle surfaces is crucial for improving the mechanical performance and slaking resistance of biocemented soils.
Locations where a liquid can remain more stably due to the combined effects of surface forces, electrostatic forces, van der Waals forces, and capillary forces are referred to as low-energy sites, such as particle contact points and surface depressions [
11]. According to colloid filtration theory, when polymer-based colloidal solutions migrate through porous media, part of the colloids tends to accumulate at low-energy sites due to filtration effects and adsorption interactions [
12]. Based on this principle, using colloids as carriers to immobilize bacteria or enzyme cannot only enhance their retention on the soil, but also effectively promote the deposition of CaCO
3 at particle contacts and interfaces [
13]. Ma et al. [
14] introduced kaolinite into bacterial solution to construct a microbially immobilized colloid system, which improved bacterial adsorption and retention in coarse sand, leading to a more uniform distribution of CaCO
3 precipitates. As a result, the unconfined compressive strength (UCS) and the impermeability of the biocemented coarse sand were improved. Similarly, other researchers have proposed the addition of polymer such as chitosan, polyvinyl alcohol and milk powder to further strengthen the immobilization of bacteria or enzyme within porous media [
15–
17]. These additives assist in the nucleation and precipitation of CaCO
3, demonstrating considerable potential for practical geotechnical engineering applications.
Moreover, in terms of enzyme-induced calcium carbonate precipitation (EICP), the enzyme exists in a free state and lacks the complex biotic interfacial regulation, which often results in disordered precipitation of CaCO
3, thereby leading to insufficient densification of the cementation and limited mechanical performance [
18,
19]. In contrast, during microbially induced calcium carbonate precipitation, microbial cell walls and their secreted extracellular polymeric substances (EPS) not only provide abundant nucleation sites but also regulate crystal growth, promoting the formation of densely structured, morphologically uniform, and strongly adherent CaCO
3 crystals [
20,
21]. Based on these differences, the introduction of EPS into the EICP system can create a stable immobilized colloidal matrix, which not only enhances the retention of enzyme, but also provides additional nucleation sites for CaCO
3 precipitation, thereby improving the solidification efficiency and mechanical enhancement of EICP-treated soils.
The commonly used EPS in microbial mineralization include chitosan, xanthan gum (XG), and guar gum [
15,
22–
24]. The chains of these polymers interact with soil particles through electrostatic adsorption, hydrogen bonding, or physical filling, thereby enhancing soil strength, increasing particle cohesion, reducing permeability, improving durability, and altering compaction characteristics [
25,
26]. Among them, XG is a natural anionic polysaccharide secreted by Xanthomonas campestris, which exhibits high viscosity, excellent rheological properties, and outstanding freeze–thaw stability [
27]. Meanwhile, XG can fill pores with colloidal phase under saturated conditions, as well as bond soil particle by forming fibrous or network-like structures under dry conditions, thereby substantially enhancing the workability of the soil [
28,
29]. Theoretically, XG can strengthen bonding in soils through a triple mechanism: 1) direct physical adhesion to soil particles; 2) promoting the enrichment and retention of the enzyme at low-energy sites within the soil; 3) providing nucleation sites for CaCO
3 precipitation. These synergistic effects collectively improve the strength and slaking resistance of EICP-treated soils.
Previous studies have indicated that the addition of XG can enhance the workability of soils such as soil mechanical properties and wind erosion resistance due to its intrinsic viscosity [
24,
30,
31]. However, the potential of XG in assisting CaCO
3 nucleation has not been thoroughly investigated, and the influence of XG on the slaking resistance of biocemented soils under water-induced conditions remains insufficiently understood. Therefore, this study employs XG as a carrier to construct an immobilized enzyme colloidal system in sand grouting reinforcement, the reinforcement effectiveness and mechanisms of XG are investigated through a series of laboratory tests. First, the UCS tests were performed to investigate the strength evolution of biocemented sand under various XG concentrations. Subsequently, ultrasonic oscillation (UO) tests were utilized to assess the slaking behavior of particles from different sections of the biocemented specimen in water environments. In addition, calcium carbonate content (
CCC) was measured and the relationships between
CCC, UCS and slaking index (
SI) were established. Finally, scanning electron microscopy (SEM) with energy-dispersive spectroscopy (EDS) and X-ray diffraction (XRD) analyses were conducted to reveal the microstructural distribution and mineralogical composition of CaCO
3. The investigation systematically clarifies the synergistic enhancement effects of biopolymer-based immobilization on CaCO
3 precipitation, UCS and slaking resistance, providing a basis for promoting bio-cementation technologies in applications such as erosion control and hydrological engineering.
2 Experimental details and testing procedure
2.1 Materials
The sand used in this study was sourced from Pingtan, Fujian Province, China, with a specific gravity of 2.65. The particle size distribution of the sand was measured through sieving method according to ASTM D422-63 [
32], as shown in Fig. 1. The SEM observation reveals that the sand particles were relatively uniform in size, with surface depressions and irregular microstructures, which may provide additional attachment sites for EICP. The sand was rinsed with water to remove surface impurities, then oven-dried at 105 °C for 24 h. After cooling, it was stored in sealed containers for later use.
The XG used in this study is a white, powdery biopolymer produced by the fermentation of Xanthomonas campestris (Fig. 2(a)). Its basic physicochemical properties are listed in Table 1. The SEM observations revealed that XG exhibited an irregular granular morphology under dry conditions, with uneven particle sizes and a rough surface texture (Fig. 2(b)).
The enzyme solution (ES) used in the EICP reaction was extracted from soybeans. The powdery soybean was dried at a low temperature, passed through a 10-mesh sieve, and then dissolved in distilled water to prepare a soybean solution with a concentration of 100 g/L. The solution was soaked at 4 °C for 24 h. Subsequently, it was centrifuged at 3000 r/min for 15 min to collect the supernatant, which served as the crude ES. The enzyme activity of ES under different environment was determined using the conductivity method [
33]. As shown in Fig. 3, the enzyme activity increases with the pH increased within the pH range of 3 to 8.3, where the initial pH of the enzyme is 8.3. When the pH is below 4, enzyme activity remained below 5 mmol/(L·min) and increases only slightly. Particularly, when pH ≤ 3.5, the activity drops below 2.5 mmol/(L·min), demonstrating the inactivation of enzyme. At the same time, temperature also has a significant effect on enzyme activity. At 0 °C, the enzyme activity is approximately 6 mmol/(L·min), which is about one-third of that at room temperature (25 °C). With the increase of temperature, the enzyme activity increases and reaches 22.78 mmol/(L·min) at 40 °C. Although the enzyme activity at room temperature (16.73 mmol/(L·min)) is 6.05 mM/min lower than that at 40 °C, the operation under room temperature conditions eliminates the need for external heating, making the process simpler and more practical. Therefore, enzyme under room temperature conditions was used for grouting.
To investigate the influence of the biopolymer on the EICP, XG was added to the ES at the concentration of 0, 0.5, 1.0, 1.5, and 2.0 g/L. The mixtures were stirred thoroughly at 4 °C using a magnetic stirrer to ensure complete dissolution. After that, the ESs with XG were sealed and stored at 4 °C for subsequent use. The cementation solution (CS) used in the EICP consisted of urea and calcium acetate, both of which are white, powdery solids. Before the experiments, equimolar amounts of urea and calcium acetate were weighed, dissolved in distilled water, and stirred continuously for 30 min to form a CS with a molar concentration of 0.5 mol/L.
2.2 Specimen preparation
The specimen preparation process for biocemented sand is illustrated in Fig. 4. The mold consisted of an acrylic tube with an inner diameter of 5 cm, assembled with components including nuts, stainless steel gaskets, rubber stoppers, geotextiles, and exposure film. First, a perforated rubber stopper was used to seal the bottom of the tube, and a layer of geotextile was placed above it to prevent sand loss. Then, sand was placed into the mold in five layers using the layered compaction method. This process produced a cylindrical sand column with a dry density of 1.7 g/cm3, a height of 10 cm, and a diameter of 5 cm. After that, the top of the specimen was covered with another piece of geotextile and sealed with a perforated rubber stopper. Finally, the upper and lower ends of the mold were secured using double-ended bolts.
The grouting system consisted of an air compressor, an air pressure control device, a reaction solution container, a support frame, and a beaker. A two-phase grouting method was employed as the following steps: First, an ES equivalent to 1.2 times the pore volume was grouted from the bottom of the mold under a grouting pressure of 20 kPa. The specimen was then left to stand for 2 h to allow sufficient adsorption of enzyme. As the two-phase grouting method replaces the ES with CS, the reaction efficiency is likely governed more by enzyme adsorption than by the ES-to-CS ratio. Hence, a CS of equal volume to the ES was subsequently injected under the same pressure, ensuring efficient enzyme replacement in soil pores while minimizing material consumption. Subsequently, a CS with the same volume of ES was grouted under the same pressure, and the leachate was collected by the beaker. The specimen was kept at room temperature (25 °C) for 24 h to allow the reaction. After 4 grouting cycles, distilled water equivalent to twice the pore volume was grouted to flush out residual ions and unreacted gel. The specimens were then demolded, and both ends were mechanically ground to obtain cylindrical specimens with regular dimensions and smooth, flat end surfaces. Meanwhile, all specimens were labeled according to the XG concentration. For instance, a specimen with an XG concentration of 2.0 g/L was designated as “XG20”.
2.3 Unconfined compressive strength tests
To evaluate the mechanical properties of the biocemented sand, UCS tests were conducted in accordance with ASTM D4219-11 [
34]. The tests were performed using a universal testing machine, applying axial load at a displacement rate of 1 mm/min until specimen failure occurred. During the tests, axial load and axial deformation were recorded to analyze the compressive strength and deformation characteristics of the specimens. After failure, each specimen was longitudinally divided into three equal sections from top to bottom and labeled as the upper section (U), middle section (M) and lower section (L), respectively. The samples were dried at 60 °C and were subsequently used for
CCC measurement and microstructural analysis.
2.4 Measurements of calcium carbonate content
To evaluate the distribution characteristics of CaCO
3 during the variation of XG concentrations, the acid-washing method was employed to measure the
CCC [
7,
35]. During the test, dried samples from the U, M, and L sections of each specimen were first finely ground, respectively. The powdered samples were then immersed in a HCl solution and allowed to react for 24 h until no bubbles were observed. After the reaction, the residual solids were filtered and thoroughly rinsed with deionized water to remove remaining acid and dissolved products. The samples were then dried in a constant-temperature oven at 60 °C for 24 h. The
CCC was calculated as the percentage of CaCO
3 relative to the EICP-treated sand, as defined in Eq. (1):
where CCC denotes CaCO3 content of biocemented sand (%), m1 and m2 denote the weight of samples before and after acid-washing (g), respectively.
2.5 Slaking resistance
In addition to evaluating the water stability of biocemented sand by measuring the UCS loss rate after immersion, UO tests have been used to evaluate the cementation of CaCO
3 under water-saturated conditions [
8,
36]. First, the dried biocemented samples were shaped into cubic blocks with an edge length of approximately 1.5 cm, then each cube was placed at the center of a black square tray to enhance contrast for image recognition. After that, the samples were immersed in an ultrasonic water bath and oscillations at a frequency of 40 kHz were applied for 10 min. During the test, a camera fixed in a top-down position captured images of the samples every minute to record their morphological changes. The captured images were processed using ImageJ software, as illustrated in Fig. 5. Initially, the images were converted to grayscale, followed by binarization, where the black area represented the sample, while the white area corresponded to the background. The number of black pixels was counted to determine the area of sample at each time point. Slaking resistance was characterized using the
SI according to Xie et al. [
37], as shown in Eq. (2):
where St denotes the area of sample at time t, S0 denotes the area of sample before UO tests. A higher SI indicates a higher degree of slaking of biocemented sand.
2.6 Microscopic analysis
To further reveal the precipitation characteristics mineral composition of the CaCO3 in biocemented sand, a series of microscopic analysis were carried out. Among them, some samples were shaped into cubic blocks with an edge length of approximately 1 cm, and their micromorphology was observed through using a FEI Quanta 250 scanning electron microscope. Simultaneously, the EDS was conducted to analyze the elemental composition and its spatial distribution. Furthermore, the formation patterns of CaCO3 and its interfacial bonding with the soil skeleton particles were examined accordingly. Other samples were powdered and sieved for XRD analysis to identify the main mineral phases. The XRD tests were conducted using a D8-Discover X-ray diffractometer, and the diffraction patterns were analyzed using Jade software.
3 Results
3.1 Unconfined compressive strength tests analysis
Figure 6(a) illustrates the stress–strain curves of biocemented sand with different XG concentrations. It is seen that the specimens exhibit a typical stress–strain response characteristic of stabilized soils, consisting of the compaction stage, elastic deformation stage, plastic deformation stage, and failure stage [
38,
39]. Notably, specimens with higher XG concentrations display a sudden drop in stress after reaching the peak value, showing an obvious brittle failure behavior. Meanwhile, the UCS increases from 121.10 to 231.05 kPa as the XG concentration increases from 0 to 2 g/L, demonstrating the significant role of XG in enhancing the cementation efficiency of EICP. Furthermore, the failure strain exhibits a decreasing trend, further confirming the increased brittleness of biocemented sand [
40–
42]. Using only 0.5 mol/L CS for 4 rounds of grouting is sufficient to significantly enhance the soil strength, indicating good application potential in wind erosion control and soil-water conservation. For soil requiring higher strength, the number of grouting cycles and the CaCl
2 concentration can be further increased. In addition, compared with traditional chemical stabilizers, the EICP-based method provides better injectability, as both the ES and CS exhibit water-like fluidity, allowing them to penetrate soil pores more effectively than cement or lime slurry. Moreover, CaCO
3 is also the main constituent of natural limestone, thereby minimizing environmental disturbance [
43–
45].
The deformation modulus (
E50) is introduced as a representative parameter to evaluate the deformation behavior of different specimens, which corresponds to the secant slope of the stress–strain curve at 50% of the peak axial stress [
46], as shown in Eq. (3):
where denotes the stress corresponding to 50% of the failure strain, denotes the failure strain.
The variation of UCS and
E50 with XG concentration is illustrated in Fig. 6(b). It is seen that the UCS exhibits a two-stage growth trend with increasing XG concentration. When the XG concentration is below 1 g/L, the UCS increases from 121.10 to 152.82 kPa, exhibiting a 26.19% increase relative to the initial strength. In contrast, as XG concentration increases from 1 to 2 g/L, the UCS further rises to 231.05 kPa, exhibiting a 64.60% increase relative to the initial strength. The growth rate in the second stage is 2.47 times that of the first stage. This phenomenon may be attributed to the fact that at lower XG concentrations, the polymer plays an initial role in promoting nucleation. As the XG concentration further increases, the polymer chains begin to form a more complete network structure and more effectively adsorb Ca
2+, thereby facilitating the formation of additional CaCO
3. These CaCO
3 are then interconnected through the polymer network to form more stable bridging structures, resulting in a pronounced strength enhancement in the second growth stage [
47,
48].
On the other hand, E50 also increases with the increase of XG concentration, demonstrating that the addition of XG not only improves the UCS but also enhances the deformation resistance. As exhibited in Fig. 6(c), E50 increases with increasing UCS and a strong correlation is observed between the two parameters. The ratio of E50 to UCS is approximately 39.76, and the coefficient of determination (R2) is 0.959.
3.2 Slaking resistance
As shown in Fig. 5, under the action of UO, the cementation between sand particles is disturbed, and the particles gradually detach from the matrix. Notably, the detached particles are mostly dispersed individually, indicating that the detachment process mainly occurs on the surface of the sample rather than complete structural failure. After 10 min of UO, the majority of the sample retained structural integrity. This phenomenon confirms the cementation formed by CaCO3 provides a relatively high degree of stability and resistance to disturbance in water environment, further demonstrating the potential of microbially induced cementation in enhancing the slaking resistance of sand.
Figure 7 illustrates the time-dependent variation of SI at the U, M, and L sections of the specimens under different XG concentrations. The results indicate that the SI ranges between 1.0 and 3.0, showing an increasing trend with the increasing UO time. Notably, the most significant slaking occurs within the first 5 min, during which the SI increases by more than 70% of the total increment. After 5 min, the growth of SI slows down, and the disintegration process enters a relatively stable phase. This phenomenon is consistent with the Fig. 5 that the specimen largely retains its structural integrity after 10 min of UO, further confirming that the cementation formed by CaCO3 exhibits excellent structural stability.
At the same XG concentration, the
SI exhibits a gradually increasing trend from the bottom to the top of the specimen. This phenomenon can be attributed to the distribution of CaCO
3 under the two-phase grouting method: with the grouting of ES and CS from the bottom, CaCO
3 tends to precipitate in the lower part of the specimen [
49]. Consequently, the lower sections exhibit greater resistance to particle detachment under UO.
Figure 7 presents the variation of average
SI with XG concentration after 10 min of UO. As the XG concentration increases from 0 to 2 g/L, the average
SI decreases significantly from 2.588 to 1.323, demonstrating that the addition of XG improves the slaking resistance of biocemented sand in water environment. At the same time, this phenomenon indirectly reflects the strengthening effect of XG on inter-particle bonding, which is also one of the key factors contributing to the increase of UCS with increasing XG concentration. Furthermore, it is worth noting that XG can transforms into a colloidal gel that fills the pores between particles under saturated conditions [
50], which will create a barrier effect to reduce the water intrusion and further improves the slaking resistance of the biocemented sand.
3.3 CaCO3 content
The results of both the UCS tests and UO tests demonstrate that the addition of XG significantly enhances the mechanical properties and slaking resistance of the specimens. To further reveal the mechanism, quantitative analyses of CCC at different sections and under varying XG concentrations were conducted, the average CCC were also calculated, as shown in Fig. 8(a). It is seen that the CCC ranges from 1.36% to 2.32%, and increases from 1.477% to 2.179% as the XG concentration increases, demonstrating the nucleation-assist effect of XG on CaCO3 precipitation. Under the same XG concentration, CCC exhibits a decreasing trend along the grouting direction (from bottom to top), which explains the previously observed increase in the SI with specimen height.
The homogeneity of the specimen can be evaluated using the statistical measures of standard deviation (
S) and coefficient of variation (
CV), as defined in Eqs. (4) and (5) [
51]:
where N denotes the number of samples, xi denotes the CCC of the ith sample, and denotes the average CCC. Higher values of S and CV denote the lower homogeneity within the specimen.
The
S and
CV of
CCC under different XG concentrations is exhibited in Fig. 8(b). It is seen that when XG concentration is 0 g/L, the
S and
CV are 0.111 and 7.540%, respectively. With the addition of XG, the
S and
CV increase to ranges of 0.181–0.233 and 9.097%–12.103%, respectively, indicating a reduction of homogeneity of CaCO
3 distribution with the specimens under the action of XG. Furthermore, when the XG concentration exceeds 1 g/L, the
CCC in the M and U sections of the specimens decreases more significantly. This distribution gradient can be attributed to the high viscosity of XG increases the flow resistance of the ES, resulting in a decrease in the retention of ES along the grouting direction [
52], which accelerates the hydrolysis of urea at the bottom of the specimen during the grouting of the CS. As a result, the vertical gradient of
CCC distribution becomes more obvious with increasing XG concentration.
Figures 8(c) and 8(d) further illustrate the correlations between
CCC and both UCS and
SI. The results indicate that UCS increases exponentially with increasing
CCC, which is consistent with the findings reported by Sun et al. [
53]. Conversely,
SI exhibits an exponential decrease with increasing
CCC, indicating that higher
CCC significantly enhances the slaking resistance of the samples. The
CCC plays a critical role in determining the mechanical and durability properties of biocemented sand, as well as XG contributes to a notable improvement in CaCO
3 precipitation. Hence, although the heterogeneous distribution of
CCC induced by XG has begun to emerge, its negative impact on the mechanical and slaking resistance remains insignificant within the scope of this study. Considering the heterogeneous distribution of
CCC caused by XG carries a potential risk of evolving into structural defects. Therefore, future research should focus on optimizing the uniformity of CaCO
3 precipitation. Currently, various approaches have been proposed to improve the uniformity of EICP solidified soils during the grouting process, such as the low-pH method, low-temperature method, and the addition of inhibitors [
8]. The combined effects of these techniques with XG on the distribution of CaCO
3 deserve further investigation.
3.4 Microscopic analysis
3.4.1 Scanning electron microscopy with energy-dispersive spectroscopy
Figure 9 presents the microstructure of biocemented sand with different XG concentrations at magnifications of 100 ×, 400 ×, and 1000 ×, where the morphology and distribution of CaCO3 is observed. Due to the low low-energy at particle contact points and microscale surface indentations serve as preferential nucleation sites, CaCO3 adheres to particle surfaces to form coatings or accumulates at contact points to create bridging structures, the cementation between particles is enhanced accordingly. For the samples without XG (Fig. 9(c)), the CaCO3 precipitation is both insufficient in quantity and limited in crystal size. Consequently, few effective CaCO3 crystals are formed at particle contacts, and uncemented gaps still remain between particles. On the contrary, with the increase of XG concentration, the amount of CaCO3 crystals attached to particle surfaces increases accordingly, with larger crystal sizes observed (Figs. 9(f), 9(i), 9(l), and 9(o)). The precipitates gradually form larger aggregates at contact points, which almost fill the gap between particles.
This variation can be attributed to the physicochemical properties of XG itself. On the one hand, XG possesses high viscosity, enabling it to adsorb and accumulate in low-energy sites during the grouting, more ES is immobilized rather than be replaced by CS. On the other hand, XG adsorbs the Ca
2+ in the CS due to its negative charge [
54,
55], promoting CaCO
3 precipitation at the attachment sites of ES. As a result, the precipitation of effective CaCO
3 is promoted in the biocemented sand.
Moreover, fibrous structures formed by XG under dry conditions can be observed on particle surfaces and pores, as shown in Figs. 9(f) and 9(n). Under such condition, XG may enhance soil strength by establishing fibrous connections between particles. Whereas in saturated conditions, it swells into a hydrogel that fills the pores and prevent the water erosion. Considering the strong cementation effect of CaCO3 and the low concentration of XG, the strength enhancement due to fiber formation can be ignored. Therefore, the primary functions of XG are promoting the precipitation of CaCO3 through enzyme immobilization and filling pores under saturated conditions.
The elemental distribution at the particle interfaces of XG0, XG10, and XG20 is analyzed using EDS, the results are shown in Fig. 10. Based on the chemical compositions of sand and reactants, Ca is identified as a key indicator of CaCO3. Ca is distributed on the surfaces of sand particles and at particle contact points. In the sample without XG, the Ca content is measured at only 6.51% by EDS, and the spatial distribution of Ca appeared sparse due to the relatively low efficiency of CaCO3 precipitation. With the increase of XG concentration, EDS images show notably Ca accumulation on particle surfaces, especially at contact points between particles. Consequently, when the XG concentration rises to 2 g/L, the Ca content increases to 14.35% accordingly.
The EDS results indicate that with the assistance of XG, larger CaCO3 agglomerates and thicker CaCO3 coatings were formed, improving the bonding between particles significantly. The findings further explain the reason that the addition of XG enhances the mechanical strength and slaking resistance of the biocemented sand.
3.4.2 X-ray diffraction
Figure 11 presents the XRD patterns of biocemented sand with different XG concentrations. Due to the high sand content (exceeding 95%), obvious diffraction peaks of SiO
2 are observed in the pattern. In addition, the main crystalline forms of CaCO
3 generated by EICP are recognized as calcite and vaterite, with calcite showing stronger peak intensities than vaterite. Calcite is known for its more compact crystal structure, higher crystallinity, and superior bonding ability, thus contributing more effectively to cementation between particles [
36,
56].
With increasing of XG concentration, a noticeable enhancement in the vaterite peak intensity is observed. This phenomenon may be attributed to the influence of XG that inhibits the transformation of vaterite into calcite [
57,
58]. Despite minor variations in the crystalline composition, the CaCO
3 content increases obviously with higher XG concentrations, and the influence of crystal phase on biocemented sand still limited. Aas a result, the UCS and
SI still increase with XG concentration increased.
4 Discussion
4.1 Mechanism of xanthan gum-assisted CaCO3 nucleation
XG is a kind of extracellular polymeric substance produced from Xanthomonas campestris, its primary molecular structure is illustrated in Fig. 12 [
59]. It is seen that the is primarily composed of D-glucose, D-mannose, and D-glucuronic acid in an approximate molar ratio of 2:2:1. Its main chain is composed of β-D-glucose, while the side chains are composed of D-mannose and glucuronic acid. The molecule is a characteristic right-handed 5-fold helical secondary configuration. Owing to its unique molecular configuration, XG exhibits a range of exceptional properties, including high viscosity, excellent rheological behavior, superior freeze–thaw stability, and extremely low toxicity [
27].
The cementation mechanisms of sand under different reinforcement methods are illustrated in Fig. 13. SEM images confirm that in EICP-treated sand, CaCO3 exists with three morphological forms: interparticle bonding at contact points, surface coating on sand surfaces, and filling pores between particles. During the grouting of ES, the pores are first saturated by it. Due to the surface depressions, the low-energy sites are mainly at particle depressions and contact areas. Hence, although the ES within the pores is gradually displaced during the grouting of CS, several ES is still retained at the low-energy sites, and CaCO3 prefers to precipitate at these specific sites first. In terms of biocemented sand without XG, the ES exhibits low viscosity and weak adsorption, the reaction system lacks nucleation sites. Consequently, the efficiency of CaCO3 precipitation is reduced, the dispersed and ineffective free CaCO3 is more likely to form. This phenomenon corresponds with the sparse distribution of Ca observed in Fig. 10(b).
With the addition of XG, the viscosity of the ES increases significantly. Under the influence of matrix suction, more ES is retained at low-energy sites during grouting [
60], reducing the probability of being displaced by CS. Moreover, XG molecules contain terminal glucuronic acid and carboxylate groups, which guarantee a high degree of negative charge (Fig. 12), thereby enhancing their ability to adsorb Ca
2+ ions [
61]. Due to the additional nucleation sites provided by XG, more CaCO
3 prefers to precipitate and accumulate on particle surfaces and at contact points, improving effective cementation between particles. Hence, it can be considered that the addition of XG enhances the workability of biocemented sand by optimizing the distribution and deposition efficiency of CaCO
3.
4.2 Slaking behavior of biocemented sand under ultrasonic oscillation
Figure 14 illustrates the schematic of the slaking process of the biocemented sand under UO. The relative stability between sand particles is primarily provided by the presence of effective CaCO3. Under the disturbance of ultrasonic, the cementation between particles is destroyed. Since the surface sand particles are less constrained by CaCO3 compared to those inner the samples, the surface particles and the bonded CaCO3 detach first. Subsequently, as the outer layer detaches, the internal particles experience a reduced constraint, and the sample experiences a progressive slaking from the exterior to the interior. According to the relationship between CCC and the SI established in Fig. 8(d), specimens with higher CCC exhibit stronger cementation than those with lower CCC. Due to the generation of effective CaCO3 increases with higher XG concentrations, the samples with higher XG obtain lower SI under UO accordingly.
5 Conclusions
In this study, the sand was cemented using XG-immobilized enzyme to assist CaCO3 nucleation. The mechanical properties and slaking resistance of biocemented sand were evaluated, and microscopic analysis were further conducted to reveal the XG-assisted nucleation mechanism. This provides a foundation for improving the CaCO3 nucleation efficiency of biocementation technology in erosion control and hydrological engineering. The main conclusions are as follows.
1) XG exhibits a significant assisting effect on CaCO3 nucleation. As the XG concentration increased from 0 to 2 g/L, the UCS of the biocemented sand increased from 121.10 to 231.05 kPa after 4 cycles of grouting, exhibiting a strength increase of 90.8%. The E50 also increased correspondingly with XG content and showed a strong linear correlation with UCS
2) The SI of biocemented sand ranges from 1.0 to 3.0 and showed an increase along the grouting direction, which is attributed to the inhomogeneous distribution of CaCO3. As the XG concentration increased from 0 to 2 g/L, the average SI decreased from 2.588 to 1.323, showing an increasing slaking resistance with the addition of XG.
3) The UCS exhibits an exponential increase with the increase of CCC, whereas the SI decreases exponentially, confirming that CCC is the main parameter that controls the performance of biocemented sand. XG enhances the mechanical and slaking resistance properties of the biocemented sand by promoting the formation of effective CaCO3. However, the high viscosity of XG increases the inhomogeneous distribution of CaCO3, further optimization is needed to balance the cementation and homogeneity.
4) EDS results indicate that the Ca content rises from 6.51% to 14.35% as the XG concentration increases from 0 to 2 g/L. CaCO3 accumulated at particle contacts and surfaces, forming larger CaCO3 clusters between particle contact points, which are the microstructural basis for the improvement in strength and slaking resistance of biocemented sand caused by the addition of XG.
5) The mechanism of XG-assisted CaCO3 nucleation lies in two synergistic effects: first, the viscosity of ES increases with XG addition, enabling greater ES retention at low-energy sites during grouting; second, the negatively charged functional groups on XG significantly enhance Ca2+ adsorption, providing nucleation sites for the precipitation of CaCO3 at particle contact points, thereby improving the cementation efficiency of EICP.