Abstract
The carbonation behavior of seawater sea sand recycled aggregate concrete (SSRAC) was investigated in this study. Considering different added water, fine aggregates, and coarse aggregates, the specimens were divided into 12 groups for the accelerated carbonation test by 7 days, 14 days, and 28 days. Among them, river sand, sea sand, and mixed sand (the proportion of sea sand and shell sand was 4:1) were used as fine aggregates. The results show that the carbonation depths of concretes with different mixtures all increase over time. When the replacement ratio of recycled coarse aggregate (RCA) is not less than 50%, sea sand is the most suitable fine aggregate to acquire best carbonation resistance, while river sand is the worst. On the contrary, when the replacement ratio of RCA is not more than 30%, river sand is the most suitable fine aggregate, while sea sand is the worst. It can also be speculated that the most appropriate replacement ratio of RCA is 50% when sea sand is applied as fine aggregates in SSRAC. At the same time, 30% replacement ratio of RCA is appropriate when mixed sand is applied as fine aggregates in SSRAC.
Keywords
Introduction
With the rapid development of economic growth and urbanization, the cement industry in China developed fast in recent 30 years. In the year of 2017, Chinese cement production was 2.38 billion metric tons (Bildirici, 2019). Today, concrete is the most common construction material in the world due to its availability and easy preparation, which is composed of four basic ingredients: water, cement, coarse aggregates, and fine aggregates (Castillo et al., 2020). The tremendous consumption of natural resources like river sand, gravel, crushed stone, and fresh water in concrete industry has raised severe environmental concerns. Among the components of concrete, aggregates (coarse and fine) take up about 70–80% of concrete’s volume (Verian et al., 2018). The global demand for concrete aggregates was 45 billion metric tons in 2017, and this number will reach an estimated 66 billion metric tons by the end of 2025 (De Brito et al., 2019). It is believed that mining of sand and gravel is the most disastrous activity which can destroy natural environments and thus affect native wildlife (Padmalal and Maya, 2014). In particular, river sand has been exploited in a great deal by mainland China and other developing countries to meet the demand for a large number of concrete structures (Guo et al., 2020). River sand or gravel mining is perhaps the most detrimental factor leading to river degradation (Zhai et al., 2020). Meanwhile, as one of the most precious resources in earth, fresh water is in great short. A World Meteorological Organization (WMO) report (WMO, 1997) indicates that more than half of the world’s population will encounter water stress by 2025.
To address such problems above, the trend of utilizing recycled coarse aggregate (RCA) as a replacement for natural coarse aggregate (NCA), sea sand as a replacement for river sand, and seawater as a replacement for fresh water in concrete (i.e., seawater sea sand recycled aggregate concrete (SSRAC)) industry has been intensively investigated and prompted in recent years.
Seawater sea sand recycled aggregate concrete is a way to form a new kind of environmental construction material. Zhang et al. (2019) concluded that although RCA may decrease the long-term mechanical behavior of concrete, these aggregates could still be used with seawater and sea sand if proper measures were applied. Due to the chloride content in SSRAC, the use of glass-fiber reinforced plastic (GFRP) rather than normal steel is alternative in reinforced concrete to avoid corrosion (D’Antino and Pisani, 2019; Robert and Benmokrane, 2013; Zhou et al., 2018) However, GFRP bars are vulnerable in alkaline environments (Jia et al., 2020). Chen et al. (2006) found the exposure to alkaline environments reduced the tensile strength of the GFRP bar to its 50% approximately after a half year exposure in alkaline solutions with a pH value of about 13.6. At the same time, carbonation is a common phenomenon in concrete which leads to the reduction of alkalinity. According to the investigation by Kim et al. (2008), alkaline environmental condition had more influence on the degradation of GFRP rods than other environmental conditions. Since carbonation can reduce the content of free hydroxyl ions in concrete, it is feasible to use the carbonation process to delay the deterioration of GFRP bars in concrete environments and that is why it is meaningful to study carbonization of SSRAC.
Most existing investigations have been concerned with the carbonation of either recycled aggregate concrete (RAC) or seawater and sea sand concrete (SSC), while a few studies have examined the effect of using seawater, sea sand, and RCA at the same time on the carbonation behavior of SSRAC. It is generally accepted that the carbonation behavior of RAC made with recycled fine and/or coarse aggregates is slightly inferior to that of ordinary concrete with the same water-to-cement ratio due to the higher water absorption and air permeability (Otsuki et al., 2003; Silva et al., 2015). With the increasing replacement ratio of RCA and the same mix proportion to that of natural aggregate concrete (NAC), there is an increasing trend of the carbonation depth in RAC (Amorim et al., 2012; Sagoe-Crentsil et al., 2001). Silva et al. (2015) drew a conclusion that the carbonation depth of RAC with 100% replacement ratio of RCA was nearly 2.15 times greater than that of ordinary concrete. Zhang and Xiao (2018b) collected the existing test results of carbonation depth of RAC and reported that the carbonation coefficient of RAC follows a gamma distribution. The carbonation behavior of RAC was sensitive to the water-to-cement ratio and the replacement ratio of RCA. Zhang and Xiao (2018a) evaluated the existing prediction models of carbonation depth for RAC and proposed a reasonable model to assess the carbonation behavior of RAC.
As for concrete made with seawater and/or sea sand, Liu et al. (2016) reported that the carbonation of sea-sand concrete could be reduced 20–50% and claimed that chloride ions brought by sea sand could reduce the porosity and optimize the pore distribution of cement paste, indicating that the presence of chloride ions improved the carbonation resistance of concrete. However, studies by Cao et al. (2010) and Jiang et al. (2009) claimed that the carbonation depth development of sea-sand concrete is comparable to that of ordinary concrete. The carbonation depth is increasing as the carbonation time increases and the concrete grade decreases. Shen et al. (2019) explored the influence of carbonation on chloride binding. Ramezanianpour et al. (2014) investigated the combined effect of carbonation and chloride ion ingress on microscopic and mechanical properties of concrete. In addition, chloride diffusion is much faster than the speed of carbonation ingress (Wang et al., 2017). The content of shell sand is also a key difference between sea sand and river sand. Newman (1968) concluded that shell particles were strong and durable and had positive influence on the decrease of porosity. Existing study by Yang et al. (2010) showed that shell particles in fine aggregates improved the permeability resistance and had no apparent effect on carbonation behavior.
The purpose of this study is to investigate the carbonation behavior of SSRAC. Since the carbonation is likely to delay the deterioration of GFRP bars reinforced SSRAC, it is of much significance to learn the carbonation behavior of SSRAC. This research aims to explore the factors which can truly influence the carbonation behavior of SSRAC through the accelerated carbonation test.
Experimental program
Materials
Chemical composition of cementitious material (%).
Physical properties of sea sand and shell sand.

Particle size distribution of the fine aggregates.
Physical properties of coarse aggregates.
RCA: recycled coarse aggregate; NCA: natural coarse aggregate.
The mixtures were prepared with ordinary Portland cement 42.5 R of Chinese standard [37]. Besides, the superplasticizer was used in the mixtures. The seawater was prepared according to Chinese standard (JGJ 55-2011, 2011), the chemical composition given in the seawater preparation regulation provided by American Society for Testing and Materials (ASTM D1141-98, 2013), in which the content of chemical substance below 0.1 g/L could be neglected. The specific details of prepared seawater can be found in the study of Xiao et al. (2017).
Mix proportion and specimens
Concrete mixtures (kg/m3).
RCA: recycled coarse aggregate; NCA: natural coarse aggregate; SSRAC: seawater sea sand recycled aggregate concrete.
The water-to-cement ratio was fixed as 0.47 (corresponding to concrete C30), and the sand ratio was fixed as 0.43. According to shell particle content and the replacement ratio of RCA, the concrete mix proportion was divided into 12 groups, among which shell particle contents in fine aggregates and replacement ratios of RCA were divided into three and four grades, respectively. The shell particle contents of river sand, sea sand, and mixed sand (the ratio of sea sand to shell sand is 4:1) are 0, 1.66%, and 21.33%, respectively. Meanwhile, the replacement ratios of RCA included 0, 30%, 50%, and 100%. For RAC, since river sand was used as fine aggregates without shell particles, only the replacement ratio of RCA should be considered for them. For example, RAC-30 represents 30% replacement ratio of RCA adopted in RAC. Considering the other shell particle contents (1.66% and 21.33%), the first letter in the specimen’s name label including M and H stands for the medium and high shell particle content, respectively. For specimen M-SSRAC-30, M means sea sand with 1.66% shell particle content; 30 means 30% replacement ratio of RCA adopted in the mix proportion. The concrete mixtures for specimens are shown in Table 4. tIn this experiment, 6 identical specimens with the size of 100 mm × 100 mm × 300 mm were prepared for each mix proportion to acquire the mean value of carbonation depth.
The fabrication of concrete test specimens is as follows. First, add the fine aggregates, coarse aggregates, and cement to the concrete mixer and keep stirring until they were mixed evenly. The simulated seawater was prepared in advance by adding chemicals to fresh water. Then add the superplasticizer (3.19 kg/m3) to the simulated seawater and add them together to the mixer in the process of stirring. Pour the concrete slurry into the mold and compact it by a vibrating rod at the same time. After face processing to the concrete in the mold, the demolding and maintenance work was carried out. Finally, the specimens were exposed under outdoor conditions until the carbonation test.
Accelerated carbonation test
The carbonation test method in the standard GB/T 50082-2009 (2009) for testing long-term performance and durability of ordinary concrete was adopted in this research. The specimens were fully dried before the carbonation, and some adjustments were made according to actual conditions.
To investigate the carbonation behavior of SSRAC with a long period of curing, after the pouring of specimens, they were exposed to outdoor conditions for 90 days. The reason for longer age of curing is that the presence of salts such as NaCl and K2SO4 in seawater and sea sand can accelerate the hydration process of concrete leading to the rapid growth in the early strength (Xiao et al., 2018). At the same time, Cl− and SO42− ions diffusing in concrete can result in the formation of soft hydration products. The lower long-term strength compared to ordinary concrete was due to the leaching out of soft hydration products (Islam et al., 2012). Salt crystallization is also responsible for the lower long-term strength and development of internal cracking in concrete (Wegian, 2010). Therefore, considering the effects of hydration products and salt crystallization, 90-day curing is more suitable for SSRAC samples. Before the carbonation test, except the two opposite experimental surfaces for carbonation, the remaining four surfaces were sealed with paraffin under dry condition. Parallel lines at 10 mm intervals along the length of side were drawn by pencil to mark the predetermined carbonation depths. The test specimens were placed in the HTX-12W concrete carbonation test box, leaving a space of not less than 50 mm between the carbonized surfaces of each. Then seal the carbonation box tightly and turn on the power and carefully unscrew the carbon dioxide gas tank valve to inject carbon dioxide into the carbon box slowly. During this process, the carbon dioxide concentration was observed by the digital display, and the flow of carbon dioxide into the box was controlled by fine-tuning the carbon dioxide pressure reducer in order to keep the carbon dioxide concentration in the box within (20 ± 3)% finally. The relative humidity was set within the range of (70 ± 5)%, and the temperature was controlled to (20 ± 2)°C in the carbonation test box. Different carbonation periods including 7 days, 14 days, and 28 days were considered in this test. The whole process of carbonation was carried out in three stages: 0–7 days, 7–14 days, and 14–28 days. After 7-day carbonation, the destructive specimens were put into the carbonation box again after sealed by paraffin to continue carbonation for the results of 14-day carbonation. Similarly, after 14-day carbonation, the destructive specimens were put into the carbonation box after sealed by paraffin to continue carbonation for the results of 28-day carbonation.
Measurement of carbonation depth
After each stage of carbonation, the test specimens were taken out and cut with a concrete cutting machine. The thickness of each cut was about 50 mm. The carbonation depth was measured with phenolphthalein solution of 1% concentration sprayed on the cutting face as an indicator. After the measurement, the damaged paraffin covers were repaired, and the cutting face was sealed with paraffin as well. Then, the repaired test specimens were put into the carbonation box again to continue the next carbonation stage. Phenolphthalein solution was chosen as an indicator due to the pH range getting phenolphthalein solution red is about 8.2–10, so it would get red when applied to the non-carbonated zone of concrete. On the other hand, the phenolphthalein solution would still remain colorless when applied to the carbonated zone. Therefore, it is feasible to detect the complete carbonation zone in this way. For each specimen, multiple points were chosen to acquire a mean carbonation depth and measured by a stick with 1 mm precision after 30 s (GB/T 50082-2009, 2009), as shown in Figure 2. In all, six specimens were required for each mix proportion to acquire the mean carbonation depth. Measurement points of carbonation depth.
Test results
Carbonation depth
The mean values of carbonation depths by different carbonation periods are drawn in Figure 3. Carbonation depths of seawater sea sand recycled aggregate concrete.
As shown in Figure 3, the carbonation depths of concrete test specimens with different mixtures all increased over time. The average increase of 14-day carbonation depths was 145.0% compared with the 7-day carbonation depths. Meanwhile, the average increase of 28-day carbonation depths was 48.7% compared with the 14-day carbonation depths. For instance, the increases of carbonation depths of M-SSRAC-30 by 14-day and 28-day carbonation test compared with the previous stage were 144.7% and 37.7%, respectively. The increases of carbonation depths of M-SSRAC-100 by 14-day and 28-day carbonation test compared with the previous stage were 222.2% and 41.4%, respectively. It can be concluded that although the carbonation depths increased over time, carbonation mostly occurred in early age. The possible reason is that the reaction product between calcium hydroxide and carbonate, namely, calcium carbonate, plays a role in fulfilling the pores in concrete (Puatatsananon and Saouma, 2005) and in turn impedes the CO2 penetration.
Influence of replacement ratio of RCA
When the shell particle content in fine aggregates was fixed at 0, 1.66%, and 21.33%, respectively, the carbonation depth differed with the replacement ratio of RCA, as shown in Figure 4. Influence of the replacement ratio of recycled coarse aggregate on carbonation depth: (a) shell particle content of 0 in fine aggregates; (b) shell particle content of 1.66% in fine aggregates; and (c) shell particle content of 21.33% in fine aggregates.
When the fine aggregates used in concrete were river sand without any shell particles, as shown in Figure 4(a), RAC-100 with 100% replacement ratio of RCA had the highest carbonation depth in each carbonation stage. The 7-day carbonation depth of ordinary concrete RAC-0 was only 0.3 mm, while that of RAC-100 was 2.7 mm, which was 9 times greater than that of RAC-0. The 14-day carbonation depth of RAC-0 was 0.7 mm, while that of RAC-100 was 4.2 mm, which was 6 times of that of RAC-0. The 28-day carbonation depth of RAC-0 was 1.0 mm, while that of RAC-100 was 5.9 mm, which was about 6 times greater than that of RAC-0. The carbonation depth of RAC-50 which was with 50% replacement ratio of RCA was second-highest after RAC-100 in each carbonation stage. When the carbonation period was 7 days, the carbonation depths of RAC-100 and RAC-50 were 2.7 mm and 1.6 mm, indicating that the carbonation depth of RAC-100 was about 1.7 times greater than that of RAC-50. When the carbonation period was 14 days, the carbonation depths of RAC-100 and RAC-50 were 4.2 mm and 2.8 mm, indicating that the carbonation depth of RAC-100 was 1.5 times greater than that of RAC-50. When the carbonation period was 28 days, the carbonation depth of RAC-100 and RAC-50 was 5.9 mm and 5.4 mm, respectively, indicating that the carbonation depth of RAC-100 was about 1.1 times greater than that of RAC-50. The carbonation depth of RAC-30 had no obvious difference to that of RAC-0, which suggests that the replacement ratio of RCA not more than 30% has no apparent effect on the carbonation behavior of RAC. But the overall trend is that the carbonation depth of RAC increases with the increase in the replacement ratio of RCA, and the difference between the carbonation depth of RAC and that of ordinary concrete shows a tendency of gradually increasing over time. According to the investigation by Otsuki et al. (2003), the carbonation performance of RAC is influenced mainly by the presence of RCA and interface transition zone (ITZ). First, the porosity of RCA is greater than that of NCA, which increases the porosity of RAC compared with its NAC counterpart. Second, since ITZ is the weak zone of RAC, the initial location of crack tends to appear in ITZ which gives CO2 access of ingress. Therefore, the carbonation resistance gets worse with the increasing replacement ratio of RCA, consistent with the experimental phenomenon.
As shown in Figure 4(b), the carbonation depths of specimens with 1.66% shell particle content had no obvious trend with changes in the replacement ratio of RCA. The carbonation depths of M-SSRAC-0 and M-SSRAC-30 rather than M-SSRAC-100 were the highest. Similarly, Figure 4(c) shows the carbonation depths of specimens with 21.33% shell particle content and different replacement ratios of RCA. Although the carbonation depths of H-SSRAC-100 were highest, the carbonation depths of H-SSRAC-30 and H-SSRAC-50 were lower than H-SSRAC-0. Thus, it can be speculated that the presence of sea sand and mixed sand leads to the difference between the carbonation behavior of SSRAC and RAC. The carbonation depth of SSRAC does not increase with the increase in the replacement ratio of RCA any more. Compared to the single influence of the replacement ratio of RCA, the coupled influence of RCA and fine aggregates seems more important and complicated on the carbonation behavior of SSRAC.
Influence of shell particle content
When the replacement ratio of RCA was fixed at 0, 30%, 50%, and 100%, the carbonation depth varied with different shell particle contents, as shown in Figure 5. Influence of the shell particle content on the carbonation depth: (a) 0 replacement ratio of RCA; (b) 30% replacement ratio of RCA; (c) 50% replacement ratio of RCA; and (d) 100% replacement ratio of RCA. RCA: recycled coarse aggregate.
As shown in Figure 5(a) and (b), the replacement ratios of RCA were not more than 30%, and thus, the main component of coarse aggregates was NCA. It has been confirmed in section 3.2 that such small replacement ratio of RCA has no apparent effect on the porosity of RAC and the carbonation behavior is almost the same as ordinary concrete. The 28-day carbonation depths of RAC-0, M-SSRAC-0, and H-SSRAC-0 were 1.0 mm, 6.2 mm, and 3.0 mm, indicating that the 28-day carbonation depth of M-SSRAC-0 was about 6 times and 2 times greater than those of RAC-0 and H-SSRAC-0, respectively. The 28-day carbonation depths of RAC-30, M-SSRAC-30, and H-SSRAC-30 were 1.0 mm, 7.9 mm, and 1.5 mm, indicating that the 28-day carbonation depth of M-SSRAC-30 was about 8 times and 5 times greater than those of RAC-30 and H-SSRAC-30, respectively. When the replacement ratio of RCA was not more than 30%, the carbonation depth of concrete which used sea sand with 1.66% shell particle content was the maximum. Conversely, the carbonation depth of concrete which used river sand without any shell particle content was the minimum. When fine aggregates were mixed sand with 21.33% shell particle content, the carbonation depth was between the maximum and the minimum.
As shown in Figure 5(c) and (d), the replacement ratios of RCA were not less than 50%, and the results were totally different. The 28-day carbonation depths of RAC-50, M-SSRAC-50, and H-SSRAC-50 were 5.4 mm, 1.1 mm, and 1.4 mm, indicating that the 28-day carbonation depth of RAC-50 was about 5 times and 4 times greater than those of M-SSRAC-50 and H-SSRAC-50, respectively. The 28-day carbonation depths of RAC-100, M-SSRAC-100, and H-SSRAC-100 were 5.9 mm, 3.4 mm, and 5.4 mm, indicating that the 28-day carbonation depth of RAC-100 was about 1.7 times and 1.1 times greater than those of M-SSRAC-100 and H-SSRAC-100, respectively. It could be concluded that when the replacement ratio of RCA was not less than 50%, the carbonation depth of concrete which used river sand without shell particles was the maximum. Conversely, the carbonation depth of concrete which used sea sand with 1.66% shell particle content was the minimum. When fine aggregates were mixed sand with 21.33% shell particle content, the carbonation depth was between the maximum and the minimum.
No regularity can be derived from the angle of shell particle content to analyze the carbonation behavior of SSRAC. It should be mentioned that although the mixed sand selected in this experiment had a higher content of shell particles than sea sand, as shown in Table 2, the content of chloride ions was lower than that of sea sand. Chloride ions can react with the cement hydration product of tricalcium aluminate (3CaO·Al2O3, C3A) to generate refractory chlorine aluminate hydration. Friedel’s salt (FS, 3CaO·Al2O·CaCl2·10H2O) forms by the dissolution and precipitation reactions: C3A + 2CH + 2NaCl + 10H2O → FS + 2NaOH. Besides, chloride ions react with Ca(OH)2 produced by cement hydration to generate calcium chloride (CaCl2) with a low solubility on the surface of C-S-H, which reduces the pore size and hence the permeability (Kayyali and Haque, 1988). The presence of calcium chloride further accelerates tricalcium silicate (C3S) hydration to generate composite salt and increase the solid phase proportion in cement pastes (Shi et al., 2012). As a result, appropriate chloride content and RCA are beneficial for carbonation resistance. What’s more, the surface of RCA is usually attached with unhydrated cement, which can make it exhibit gel activity when encountering water. The reaction may happen on the surface of RCA, and the reaction products will fill the pores of RCA first rather than the cement matrix. However, excessive amounts of chloride relative to the amount of RCA will cause cracking and in turn accelerate the diffusion of CO2 (Qiao et al., 2018). The cracking can be attributed to the too much leaching out of hydration products and the crystallization pressure if the salt content is in excess. In a sense, there is a most suitable ratio of RCA and chloride content for best carbonation resistance. Compared to the shell particle content, the carbonation behavior is more affected by the high concentration of chloride ions.
Discussions
The process of carbonation in concrete can be divided into three steps: The diffusion of CO2 in concrete; the dissolution of CO2 in the pore solution; and the formation of calcium carbonate. In fact, the third step, namely, the reaction of Ca2+ and CO32− to generate calcium carbonate, is fairly quick. As a result, the most important factor controlling carbonation behavior is the diffusion rate of CO2, which is determined by pore size distribution and the porosity of concrete. Thus, pore size distribution and porosity are key factors which influence the carbonation rate. The computed tomography (CT) technique (NIKON XTH 320/225, Nikon Corporation, Tokyo, speed of 0.5 s/rotation, exposure of 300 kV and 250 mA, recon matrix of 2000 × 2000, and slice thickness of 1.0 mm) is used to analyze the porosity of concrete to understand its relation with carbonation resistance. The results are shown in Figure 6. Porosities tested by CT: (a) RAC specimen; (b) M-SSRAC specimen; (c) H-SSRAC specimen. CT: computed tomography; SSRAC: seawater sea sand recycled aggregate concrete.
For RAC, the porosity of RAC-100 was larger than that of RAC-0 which is in line with the conclusion drawn in section 3.2 that the carbonation depth of RAC increases with the increase in the replacement ratio of RCA. Combined with the experimental phenomenon shown in Figure 4(a), it can be deduced that when the replacement ratio of RCA is not less than 50%, the porosity and ITZ caused by RCA is apparent and notable.
For M-SSRAC, the porosity of M-SSRAC-0 was larger than that of M-SSRAC-100, indicating that chloride ions in sea sand were so excessive that the leaching out of hydration products and crystallization pressure resulted in large porosity. The presence of RCA in M-SSRAC-100 abated such adverse influence because the initial pores in RCA could admit a large number of crystals, reducing the possibility of cracks and pores in concrete. Combined with Figure 4(b), it can be speculated that 50% replacement ratio of RCA is most suitable for the chloride content in M-SSRAC. The pores brought by 100% replacement ratio of RCA itself are larger than the reduced pores filled by reaction products. As for M-SSRAC-0 and M-SSRAC-30, they lacked adequate RCA, so the chloride content was relatively excessive for them and hence, porosities caused by crystallization pressure were large.
For H-SSRAC, the porosity of H-SSRAC-0 was larger than that of H-SSRAC-100. From Figure 4(c), it seems that 30% replacement ratio of RCA was appropriate for the chloride content in H-SSRAC, consistent with the less chloride content compared with M-SSRAC. Consequently, 50% and 100% replacement ratio of RCA was relatively excessive and hence large porosities brought by RCA. For H-SSRAC-0, the coarse aggregates were all NCA, and the chloride in fine aggregates was detrimental to carbonation resistance.
For specimens with 0 replacement ratio of RCA, the porosities of RAC-0, M-SSRAC-0, and H-SSRAC-0 are consistent with the experimental phenomenon. As shown in Figure 5(a) and (b), in the case of 0 or 30% replacement ratio of RCA, not enough RCA could afford spare room on its surface to accommodate reaction products. Therefore, the more chloride, the more pores were caused by the leaching out of hydration products and crystallization pressure. The carbonation resistance of M-SSRAC was the worst due to its most chloride ions followed by H-SSRAC. However, for specimens with 100% replacement ratio of RCA, the porosity of RAC-100 is more than the others in accordance with its highest carbonation depth. The reason why the porosity of M-SSRAC-100 is more than H-SSRAC-100 is probably due to stochasticity in the CT test. As shown in Figure 5(c) and (d), in the case of 50% or 100% replacement ratio of RCA, the amount of RCA was so large that the porosity brought by it was considerable. Pores of RCA could be filled with the reaction products of chloride and unhydrated cement particles attached on the surface of RCA. Hence, the carbonation resistance of M-SSRAC was the best due to its most chloride ions followed by H-SSRAC. Summarily, when the replacement ratio of RCA is not more than 30%, the carbonation resistance is vulnerable due to the presence of chloride ions. On the other hand, when the replacement ratio of RCA is not less than 50%, the carbonation resistance improves instead under the influence of chloride ions.
In a word, for RAC, the replacement ratio of RCA which is not more than 30% has negligible impact on the carbonation behavior of RAC. Thereafter, the porosity increases with the increase in RCA and hence worse carbonation resistance. As for SSRAC, the most important influencing factor is not shell particle content but the ratio of RCA and chloride content. In this investigation, although sea sand and shell sand had different shell particle contents, no apparent effect for this reason could be observed, indicating that the content of shell particles had negligible influence on carbonation behavior of SSRAC. Conversely, due to the content of chloride ions in the sea sand and mixed sand was different, a regular phenomenon could be found. Considering the surface of RCA is usually attached with unhydrated cement, which react with chloride ions and form products filling the pores of RCA, moderate chloride ions can make up for the defect owing to the usage of RCA, beneficial for carbonation resistance. However, excessive chloride ions are negative in that the leaching out of hydration products and crystallization pressure tend to cause cracking in concrete.
Conclusions
In this investigation, 12 mix proportions were applied considering different shell particle contents and replacement ratios of RCA. The development trend of carbonation depth was experimentally studied, and the most influencing factors of carbonation behavior were deduced. Conclusions can be drawn, and recommendations on future researches are given based on the current state-of-the-art. The carbonation depths of specimens with different mix proportion all increased over time. The average increases of carbonation depths by 14 days and 28 days compared with 7 days and 14 days were 145% and 48.7%, respectively. It can be concluded that although the carbonation depth increases over time, carbonation mostly occurs in early age. For RAC, the replacement ratio of RCA which is not more than 30% has negligible impact on the porosity of RAC. The 28-day carbonation depth of concrete with 100% replacement ratio of RCA, RAC-100, was about six times greater than that of ordinary concrete RAC-0. The overall trend is that the carbonation depth of RAC increases with the increase in the replacement ratio of RCA, and the difference between the carbonation depth of RAC and that of ordinary concrete shows a trend of gradually increasing over time. As for SSRAC, due to the presence of sea sand and mixed sand, the carbonation depth of SSRAC does not increase with the increase in the replacement ratio of RCA any more. However, it is not because of the content of shell particles but the content of chloride ions in fine aggregates. Although three levels were set according to different shell particle contents, no clear relation can be concluded between carbonation resistance and shell particle content. Conversely, some regularities can be found from the viewpoints of chloride content. When the replacement ratio of RCA is not less than 50%, sea sand is the most suitable aggregate to acquire best carbonation resistance while river sand is the worst. On the contrary, when the replacement ratio of RCA is not more than 30%, river sand is the most suitable aggregate to acquire best carbonation resistance and sea sand is the worst. The leaching out of hydration products and crystallization pressure caused by chloride ions in sea sand or mixed sand can be a disadvantage to carbonation resistance. However, further investigations are need to clarify the effect of replacement ratio of RCA on the carbonation behavior of SSRAC. Due to the hydration process is responsible for the porosity and the pore size distribution in cement-based material, further research is needed to investigate the hydration process of SSRAC and the microstructures of hydration products. It should be mentioned that the conclusions above are obtained only by the analysis of the test results in this investigation.
Footnotes
Declaration of conflicting interests
The author(s) declared no potential conflicts of interest with respect to the research, authorship, and/or publication of this article.
Funding
The author(s) disclosed receipt of the following financial support for the research, authorship, and/or publication of this article: The authors wish to acknowledge the financial support by the National Natural Science Foundation of China (NSFC, No. 52008304, 52078358), the China Postdoctoral Science Foundation (2019M661620), the Science and Technology Innovation Research, and the Shanghai Jianfeng Yichang Engineering Technology Co., Ltd.
