Chloride Penetration into Concrete under the Coupling Effects of Internal and External Relative Humidity

Zhu, Fangzhi; Ma, Zhiming; Zhang, Mingmin

doi:https://doi.org/10.1155/2020/1468717

Advances in Civil Engineering

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Abstract Introduction Materials Experimental Results and Discussion Conclusions Data Availability Conflicts of Interest Acknowledgments References Copyright Related Articles

Research Article | Open Access

Volume 2020 | Article ID 1468717 | https://doi.org/10.1155/2020/1468717

Chloride Penetration into Concrete under the Coupling Effects of Internal and External Relative Humidity

Fangzhi Zhu,^1,2Zhiming Ma ,³and Mingmin Zhang²

Academic Editor: Claudio Mazzotti

Received01 Aug 2019

Revised18 Dec 2019

Accepted31 Dec 2019

Published11 Feb 2020

Abstract

Chloride penetration frequently happens in an unsaturated concrete; in this case, the chloride migration is under the coupling effects of internal moisture and external relative humidity (RH). Various chloride attack tests were designed in this paper to investigate the effects of internal moisture and external RH (50–100%) on the chloride penetration into an unsaturated concrete, and the chloride content was determined to quantify the chloride migration in concrete. The results highlighted that there was a good correlation between the chloride penetration into concrete and its internal RH. The chloride ion was difficult to penetrate into concrete when its internal RH was below 50%; however, the chloride penetration rate increased when the internal RH of concrete was above 75%, and the chloride migration increased with increasing RH and exposure duration. Water evaporation in concrete increased with decreasing external RH, and an obvious increase in the surface chloride content may be observed when external RH was 50%; however, when external RH was above 75%, the inner chloride content increased and surface chloride content decreased with increasing exposure duration. Simulating the chloride penetration under wet-dry cycling, the water migration resulted in an increase in the surface chloride content and a decrease in the inner chloride content, and the chloride crystal precipitated on the surface of concrete with a high w/c ratio.

1. Introduction

With rapid development of construction technology, concrete structure was inevitably exposed to various harsh environments, mainly including chloride attack, freezing-thawing, and carbonation environments [1–3]. In particular, chloride penetration frequently resulted in the steel corrosion of reinforced concrete and reduced its service life, which was a key indicator for concrete durability [4, 5]. Worldwide scholars have conducted a mass of studies to investigate the chloride penetration into concrete, and they found that the chloride penetration was different when concrete subjected to various exposure environments; moreover, the capillary absorption, concentration gradient, and convection provided the main driving force for chloride penetration into concrete [6–8]. In any case, the chloride migration was controlled by the internal moisture content of concrete and the external RH of the exposure environment.

For concrete subjected to underwater, the chloride penetration into saturated concrete has been systematically investigated by scholars around the world, and some valuable conclusions have been obtained [9, 10]. For simulating the chloride migration in an unsaturated concrete when exposed to marine tidal zone and spray zone, the chloride penetration was frequently determined by capillary absorption test and wet-dry cycling test, and the previous study reported that the chloride penetration was close to the wet-dry cycles, ion concentration and exposure duration [11–13]. However, a quantitative test to evaluate the chloride migration in such unsaturated concrete was lacking, and the influence mechanism of water convection on the chloride migration was not clear yet.

In practice, the concrete with various moisture content was frequently subjected to the condition with various RH values, and the previous investigations found that the internal moisture content and external RH have an obvious impact on the properties of concrete. For the mechanical properties, Barluenga et al. [14] and Han et al. [15] investigated the impact of applied curing RH on the mechanical properties of concrete, and the results reported that increasing curing RH was helpful to the strength of concrete. For the early age and long-time deformation of concrete, Yalçınkaya and Yazıcı [16] and Frech-Baronet et al. [17] studied the effect of RH on the shrinkage and creep of concrete, and the results reported that the shrinkage value decreased with increasing RH, whereas the increasing RH led to a decrease in the indentation modulus and long-term creep rate was increased. For the durability of concrete, the previous investigations found that the carbonation rate of concrete exposed to 40–70% RH was higher than that exposed to other RH [18–20]. Some scholars further investigated the influence of RH and moisture content on the chloride penetration into concrete; for example, Homan et al. [21] reported that the increasing internal moisture content aggravated the chloride penetration, and the water convection had a significant impact on chloride migration in concrete [22]. Bastidas-Arteaga et al. [23] and Samson et al. [24] proposed a comprehensive probabilistic model to predict the chloride migration in an unsaturated concrete, and the influence factors of moisture content and RH were considered in this model. However, a quantitative test for determining the influence of internal moisture and external RH on the chloride penetration was lacking, which was helpful to better understand the chloride migration in an unsaturated concrete.

Based on the introduction above, this paper was developed to investigate the effects of internal moisture content and external RH on chloride penetration into concrete. The concrete specimen with various sizes was first prepared, and then various chloride attack tests were designed and applied on the specimen with various internal moisture content and external RH values (50–100%). The chloride content was determined to quantify the chloride distribution in concrete under the coupling effect of internal and external RH; moreover, the chloride penetration with coupling effects of water convection was also determined in this paper, which was helpful to achieve a better understanding on the chloride penetration into concrete under wet-dry cycling. We hope the findings in this paper were helpful to the further investigation of chloride penetration into unsaturated concrete.

2. Materials and Experimental Details

2.1. Mixture Proportions and Concrete Specimens

Table 1 shows the mix proportion of concrete. The grade of Portland cement was PO 42.5. The size of the natural coarse aggregate was 5–25 mm, and the fineness module of sand was 2.9. The water-to-cement ratio (w/c) of concrete in this paper was 0.4, 0.5, and 0.6. To reduce the effect of mixture flowability on the properties of hardened concrete, the slump of all the concrete mixtures with various w/c ratios was controlled around 90 mm by adjusting the content of water reducing agent in such mixture. The cube specimen with the size of 100 mm was first prepared according to the mix proportion in Table 1, and the specimens after hardening were placed in a standard curing room for 28 d (T = 20 ± 2°C, RH ≥ 95%).

2.2. Experiment for Chloride Penetration into Concrete with Various Internal Moisture Content

Attributed to that the chloride migration was difficult to happen in concrete when its internal RH was below 50%, the targeted RH in this paper was 50–100%. One was expected that the RH around 80% may have an obvious impact on the chloride migration in concrete; thus, two similar RH values (75% RH and 80% RH) were presented, and they were also helpful to the testing accuracy in this paper. Figure 1 shows the experimental flow for chloride penetration into concrete with various internal RH values and the concrete w/c used in this section was 0.5. Referring to the related references and standard [25, 26], 5% NaCl solution was used in the chloride penetration test. Observing from Figure 1(a) when the internal RH of concrete was 50–80%, the cube specimen was first placed into a small specimen with the size of 100 mm × 100 mm × 25 mm, to rapidly reach the targeted internal RH in concrete; and then the specimens were, respectively, placed in a vacuum saturation meter which contained 5% NaCl solution and water, and the duration of vacuum filling water was 24 h; in this case, some specimens titled A were saturated with 5% NaCl solution, and the other specimens titled B were saturated with water. After that, the specimens were placed in a room with constant temperature and RH for 2 months, and the targeted internal RH in the specimen reached 50%, 75%, and 80%, respectively. Finally, A specimen and B specimen with the same internal RH were connected with an ultrathin filter paper for 1, 6, and 12 months, and in this case, the chloride ion in A specimen could migrate from A specimen to B specimen under the driving force of concentration gradient.

(a)

(b)

Figure 1(b) shows the experimental flow for chloride penetration into concrete with an internal RH of 100%, and the specimen size in this test was 100 mm × 100 mm × 50 mm. The specimens were first saturated with 5% NaCl solution and water, and in this case, the internal RH was 100%. Subsequently, the A specimen saturated with 5% NaCl solution and B specimen saturated with water were immediately connected through an ultrathin filter paper, and the connecting duration (chloride penetration time) was 1, 6, and 12 months. After the chloride penetration test, the chloride content in concrete was determined, and the chloride migration under the application of various internal RH values could be quantified.

2.3. Experiment for Chloride Penetration into Concrete Exposed to Various External RH Values

In this section, the chloride penetration into concrete was studied when subjected to the external environment with various RH values. Figure 2 shows the detailed experiment flow. The w/c of concrete used in this section was 0.5, and the specimen size was 100 mm × 100 mm × 100 mm. The specimen after curing was first placed in an air-drying oven until a constant weight was reached. After that, except for the two opposite sides, four sides of the specimen were sealed with wax and aluminum tape. The remaining one side was connected with 5% NaCl solution, and the opposite side was exposed to air; in this case, enough chloride penetrated into concrete by capillary absorption, and the whole duration of chloride attack was 1 week. Finally, the specimen after chloride attack was placed in a condition with constant temperature and humidity (T = 20°C; RH = 50%, 75%, 80%, and 100%), and the chloride penetration into concrete was with the coupling effect of external RH. After 1, 6, and 12 months, the chloride content in such specimen was determined to quantify the chloride distribution in concrete when subjected to various external RH values.

2.4. Test for Chloride Migration with the Coupling of Water Convection

Although numerous studies on the chloride penetration under wet-dry cycling have been conducted, the investigation on the quantitative influence of water convection on the chloride migration in unsaturated concrete was lacking. Simulating the chloride migration under wet-dry cycling, this section investigated the chloride penetration into concrete with the coupling effect of water convection, and meanwhile, the experiment of chloride migration by concentration gradient was further compared. In addition, this test further investigated the effect of chloride attack duration and water convection duration on the chloride distribution in concrete. Figure 3 shows the specific experiment flow. The w/c of concrete used in this section was 0.4 and 0.6, and the specimen size was 100 mm × 50 mm × 20 mm. The chloride penetration test was first conducted, and the chloride attack duration was 2 and 16 weeks. After an initial chloride attack test, all the surfaces of the part of the speciments were sealed and placed for various durations; in this case, the internal moisture content was 100%, and the chloride migration from a high concentration to a low concentration by the driving force of concentration gradient. The other part of the specimens, after an initial chloride attack test, were subjected to the application of water convection; in the test of chloride-water convection, the chloride attack surface was exposed to the air, and its opposite surface was contacted with water, and the contacting time was 2, 4, 8, and 16 weeks. Finally, the chloride content in concrete was determined, which could well quantify the effects of the concentration gradient and convection on chloride migration in concrete.

2.5. Chloride Content Determination

Referring to the related references and Chinese standard Technical specification for test of chloride ion content in concrete (JGJ/T322-2013), the free chloride content was determined by the method of chemical titration [27–29]. Specimens after chloride attack test were dried completely in an air-drying oven until reaching a constant weight (50°C, approximately 7 d). Subsequently, one layer of the specimen with a thickness of about 1 mm was milled starting from the chloride attack surface, and the concrete powder derived from various layers was obtained in this way. Finally, the obtained powder was dissolved in water for 24 h; in this case, the free chloride ion contained in powder could be dissolved in water, and finally the chloride content was determined. Equation (1) shows the specific formula used in determining free chloride ion by the method of chemical titration, where presents the content of free chloride ion, in %; is the concentration of solution, in mol/l; presents the weight of concrete powder, in ; stands for the volume of water, in ml; is the volume of filter liquor, in ml; and is the consumed volume of solution, in ml:

3. Experimental Results and Discussion

3.1. Chloride Penetration into Concrete with Various Internal Moisture Content

Figure 4 shows the chloride content curves of concrete with various internal RH values, and the surface and maximum chloride content was used to quantify the chloride penetration rate [30, 31]. When the internal RH was 50% and up to 6 months, there was no obvious decrease in the chloride content in the A specimen that was saturated with NaCl solution, and there was a slight increase in the chloride content in the B specimen that was saturated with water. When the exposure duration was 12 months, some chloride ions migrated from the inner layer to the surface of the A specimen, and meanwhile, there was a slight increase in the surface chloride content of the B specimen; this may be due to that the low internal RH hampered the chloride migrating from A specimen to B specimen, and a long time exposure was needed to achieve the chloride migration in concrete. When the internal RH was 75% and 80%, as shown in Figures 4(b) and 4(c), the chloride content in the A specimen generally decreased and the chloride content in the B specimen increased with increasing exposure duration; moreover, an obvious increase in the surface chloride content in the B specimen was observed when the exposure duration was 12 months; for example, the surface chloride content of the B specimen was, respectively, 0.027%, 0.035%, and 0.035% when the internal RH was 50%, 75%, and 80% after 1-month exposure and the results were 0.053%, 0.115%, and 0.124% after 12-month exposure.

(a)

(b)

(c)

(d)

Observing from Figure 4(d), when the internal RH was 100%, there was an obvious decrease in the chloride content of the A specimen with increasing exposure duration; moreover, the chloride content at various depths trended to be balanced, and this may be because the chloride rapidly migrated from high concentration to low concentration by concentration gradient when internal RH was 100%, and finally a similar chloride content in various depths was reached. Some chloride ions migrated from the surface layer to the inner layer of the A specimen, and the other chloride ions migrated from A specimen to B specimen, which resulted in an obvious increase in the surface content of B specimen. In addition, the surface and inner chloride content in the B specimen with 100% RH was both higher than that with the other internal RH, which was attributed to that the increasing internal RH promoted the chloride migration from the A specimen to B specimen. When the exposure duration was the same, it was noticed that the difference value between the surface chloride content in A and B specimens decreased with increasing RH, and the surface chloride content in A and B specimens was almost the same when the internal RH was 100%.

Figure 5 shows the chloride content curves of concrete after various exposure durations. When the exposure duration was 1 month, the surface chloride content in the B specimen with 50% RH, 75% RH, and 80% RH was almost zero, whereas the surface chloride content with 100% RH reached 0.1%. When the exposure duration was 6 months, the surface chloride content in B specimen with 50% RH and 75% RH was still lower than that with 80% RH and 100% RH. When the exposure duration was 12 months, the surface and inner chloride content with 50% was much lower than that with 75% RH, 80% RH, and 100% RH. For concrete with internal RH of above 75%, the results above highlighted that the increasing internal RH was helpful to the chloride migration in concrete, and relatively low RH required more time to migrate enough chloride ion. Analyzing the reason was that the chloride penetration was mainly by the medium of water, the chloride penetration into concrete was mainly by massive water-saturated passageways [32–34]. The decreasing RH resulted in a decrease in the number of water-saturated passageways in concrete and thus the chloride migration was decreased. However, for the concrete with 50% RH, the prolonged exposure duration did not significantly increase the chloride penetration into the B specimen. This was because the capillary absorption force caused by unsaturated capillary pores, as well as the ion adsorption force between the C-S-H and chloride ion, further hindered the chloride migration in unsaturated concrete, and thus the chloride migration from the A specimen to B specimen with 50% RH was quite slow.

(a)

(b)

(c)

Figure 6 further shows a relationship between the relative maximum chloride content and internal RH of concrete (B specimen), and a binomial relation could be observed. The increase in the maximum chloride content was slight when the internal RH ranged 50–75%, and the increase was obvious when the internal RH was above 75%. The specific equation was also described in this figure, where C_Rmax was the relative value of the maximum chloride concrete in %; RH was the internal relative humidity, in %.

3.2. Chloride Penetration into Concrete when Subjected to Various External RH Values

Figure 7(a) shows the chloride content curves of concrete subjected to the condition with 50% RH. When the exposure duration was 1 month, the surface and maximum chloride content after 1 month was higher than the control group without exposure; this was because the water evaporation resulted in the chloride migration from inner to surface layer. However, when the exposure duration was 12 months, the surface and maximum chloride content after 12 months was lower than the control group; this was due to that the water convection was decreased with increasing exposure duration and chloride ion migration from the high concentration to the low concentration by concentration gradient, which resulted in a decrease in the surface chloride content and an increase in the inner layer of concrete, such as the maximum chloride content after 6 and 12 months was 5.3% and 26.4% lower than that after 1 month.

(a)

(b)

(c)

(d)

Figures 7(b)–7(d) show the chloride content curves of concrete exposed to the environment with 75–100% RH. It was noticed that the maximum chloride content decreased with increasing exposure duration; for example, the maximum chloride content of concrete subjected to 75–100% RH was 17.6–20.5% lower than the control group when the exposure duration was 1 month, and the results were 42.0–54.5% when the exposure duration was 12 months. Furthermore, the chloride content in inner layer decreased with increasing exposure duration; for example, the balanced chloride content of concrete subjected to 75–100% RH was 31.2–40.6% higher than of the control group when the exposure duration was 1 month, and the results were 122.5–134.4% when the exposure duration was 12 months.

The results above highlighted that external RH had an obvious impact on the chloride penetration into concrete. When the external RH was 50%, the water evaporation at the early exposure played a dominant role in the chloride migration, and the water evaporation decreased with increasing exposure duration, and the chloride migration by concentration gradient began to play a key role in the chloride penetration at the latter period of air exposure. However, when the external RH was above 75%, the chloride migration by concentration gradient played a dominant role in chloride migration at the early and latter stages of air exposure and the chloride ion migrated from high concentration to low concentration, which resulted in a decrease in the surface content and an increase in the chloride content in the inner layer of concrete. Especially for concrete subjected to 75–100% RH, the chloride content on the surface layer and in the inner layer was almost the same after 12-month exposures, and this phenomenon was not observed for concrete subjected to 50% RH. Figure 8 shows the balanced chloride content in the inner layer of concrete when subjected to various external RH values. The balanced chloride content increased obviously at the first exposure duration, and then the increase became slow with the further increase of exposure duration. In addition, the difference value between the balanced chloride content with 50% RH and that with 75–100% RH was significant with increasing exposure duration.

Figure 9 shows the chloride content curves of concrete after various exposure durations. At the early period of air exposure (1 month), the water evaporation resulted in the chloride migration from the inner layer to the surface layer in concrete, and in this case, the maximum chloride content in concrete subjected to 50–80% RH was higher than that subjected to 100% RH, and even the maximum chloride content in concrete with 50% RH was higher than the control group without exposing to external environment. At the latter period of air exposure (12 months), the internal RH in concrete tends to be close to the external RH (50%), and there was no obvious difference on the chloride distribution in concrete after environment exposure and the control group, which further proved that the chloride migration was difficult to happen in concrete with low RH. However, when the external RH was 75–100%, the chloride content in the surface and inner layer was tended to be the same, and in this case, the concentration gradient provided the driving force for chloride migration from high concentration to low concentration. It was noticed that the difference value on the surface and inner chloride content was decreased with increasing external RH, which indicated that the high external RH promoted the chloride migration by a concentration gradient. Figure 9(d) shows a relationship between the balanced chloride content in inner layer and the exposed external RH after various exposure durations, and a linear relationship could be observed between them; moreover, the specific equation was also described in this figure, where C_SA was the chloride content at stability area of concrete, in %; RH was the external RH, in %.

(a)

(b)

(c)

(d)

3.3. Chloride Migration in Concrete with the Coupling of Water Convection

Simulating the chloride migration under wet-dry cycling, the chloride content in concrete was determined after various durations of water convection. Observing from Figures 10(a) and 10(c), when the chloride attack duration was 2 weeks, in this case, there was no enough chloride ion present in concrete. The surface chloride content increased with increasing duration of water convection up to 8 months; this was because the water convection resulted in the chloride migration from the inner to surface layer. When the duration of water convection was 16 months, the surface chloride content in concrete with 0.4 w/c was high than that after 0–8 months; this may be due to that the concrete with low w/c had high density and the water convection was steady with water evaporation, and thus the chloride continued steadily migrating from the inner to the surface layer in concrete. However for concrete with 0.6 w/c, the surface chloride content in concrete after 16 months was lower than that after 0–8 months; this was because the concrete with high w/c had high porosity, and the rapid water evaporation resulted in the separation of NaCl crystal on the surface; thus, the surface chloride content was decreased.

(a)

(b)

(c)

(d)

Figure 10

Chloride content curves of concrete after chloride attack and water convection time. (a) After 2-week chloride attack (w/c = 0.4), (b) after 16-week chloride attack (w/c = 0.4), (c) after 2-week chloride attack (w/c = 0.6), and (d) after 16-week chloride attack (w/c = 0.6). “2 w Cl⁻” represents that chloride content was immediately determined after 2-week chloride attack (control group); “2 w Cl⁻ + 16 w H₂O” presents that the concrete was first subjected to the chloride attack for 2 weeks and then the opposite surface connected with water for 16 weeks.

Observing from Figures 10(b) and 10(d), there was enough chloride ion contained in concrete when the chloride attack duration was 16 weeks. When the duration of water convection was 2 weeks, the surface chloride content in concrete with 0.4 and 0.6 w/c was both higher than that of the control group, which was attributed to that the water convection promoted the chloride migration from the inner to surface layer. However, when the duration of water convection was above 8 weeks, the surface chloride content in concrete with 0.4 and 0.6 w/c was both lower than that of the control group, and a contrary phenomenon was observed for the inner chloride content.

On the one side, when the concrete contained enough chloride ion, the separation of NaCl crystal could be observed on the surface of concrete with continuous water evaporation, which decreased the surface chloride content; moreover, the decrease in the surface chloride content of concrete with 0.6 w/c was more obvious than that with 0.4 w/c. On the other side, the chloride migration was easy to happen when enough chloride was contained in concrete, which resulted in the chloride migration from the surface layer (high concentration) to the inner layer (low concentration). In particular, the surface and inner chloride content in concrete with 0.6 w/c was close when the water convection duration was 16 weeks, and the inner chloride content in such concrete was much higher than the control group. The results above showed that the water convection played a key role in the chloride migration in concrete, and the change was more obvious for the chloride content in the surface layer; however, with the further increase of water convection duration, the chloride migration by concentration gradient resulted in an increase in the inner chloride content of concrete. Compared with the results in Figures 10(b) and 10(d), the effect of water convection and concentration gradient on chloride migration in concrete with high w/c was much higher than that with low w/c. The results above highlighted that the concrete properties (w/c), chloride attack duration, and water convection duration all had an obvious impact on the chloride distribution in concrete, which should be seriously considered in the test of wet-dry cycle.

Figures 11(a) and 11(b) show a comparison between the chloride penetration by convection and concentration gradient when the concrete w/c was 0.4. The surface chloride content by convection was higher than that by concentration gradient after the same duration; moreover, the difference on the surface chloride content by convection and concentration gradient after 2 weeks was more obvious than that after 16 weeks. However, there was no obvious difference on the inner chloride content by convection and concentration gradient. This was because that the effect of water convection on the chloride distribution was obvious when the chloride penetration depths were below 6 mm, whereas the effect of chloride migration by the concentration gradient on chloride distribution was significant in the inner concrete. The intensity by convection was higher than that by a concentration gradient, and the continuous convection resulted in the chloride gathering around the surface layer with water evaporation, which led to the chloride content by convection was higher than that by concentration gradient [35]. However, the water convection was feeble in the inner layer of concrete, and thus there was no obvious difference on the inner chloride content in various concrete after the same duration.

(a)

(b)

(c)

(d)

Figure 11

Curves of chloride content by convection and concentration gradient. (a) After 2-week chloride attack (w/c = 0.4), (b) after 16-week chloride attack (w/c = 0.4), (c) after 2-week chloride attack (w/c = 0.6), and (d) after 16-week chloride attack (w/c = 0.6). “2 w Cl⁻” represents that chloride content was immediately determined after 2-week chloride attack (control group); “2 w Cl⁻ + 8 w CM” presents that the concrete was first subjected to the chloride attack for 2 weeks, and then all the surfaces were sealed and standing for 8 weeks, and in this case, chloride migration (CM) was by the concentration gradient.

Observing from Figures 11(a)–11(d), when the chloride attack duration was 2 weeks and there was no enough chloride ion in concrete, the surface chloride content by convection was higher than that by a concentration gradient. However, when the chloride attack duration was 16 weeks and there was enough chloride ion in concrete, the surface chloride content by convection was lower than that by concentration gradient, and this was because of the separation of NaCl crystal on the surface layer with continuous water evaporation. In addition, the separation of NaCl crystal was prone to happen in concrete with high w/c than that with low w/c; moreover, the initial chloride content in concrete with high w/c was higher than that with low w/c, which further aggravated the chloride precipitation on surface and meanwhile migration to the inner layer. Therefore, the surface chloride content by convection was higher than that by a concentration gradient in concrete with 0.4 w/c, whereas an opposite result was obtained for concrete with 0.6 w/c. The results above highlighted that the concrete properties (w/c), chloride attack duration, and water convection duration were the main reason that resulted in an obvious difference on the chloride penetration by convection and concentration gradient.

This paper provided an insight into the impact of internal and external RH on the chloride penetration into concrete. It was noted that the results and discussion were based on the macroscopic experimental results in this paper. The macroproperties was closely related to the microproperties of cementitious materials [36–38], and thus further microscopic test and analysis should be conducted to achieve a better understanding on the chloride migration mechanism in unsaturated concrete. In addition, considering the wide use of recycled concrete in construction engineering [39–41], the chloride penetration into recycled concrete under the coupling effects of internal moisture content and external RH should be investigated in further.

4. Conclusions

Concrete was inevitably subjected to various environments, and this paper was developed to quantify the effects of internal moisture content and external RH on the chloride migration in an unsaturated concrete. Based on the results and discussion above, following conclusions were obtained:(1)Chloride migration was difficult to happen in concrete with internal RH below 50%. However, the chloride ion rapidly migrated in concrete when its internal RH was above 75%, and chloride penetration rate increased with increasing internal RH. In particular, a good relationship was observed between the maximum chloride content and internal moisture content of concrete.(2)When concrete suffered chloride attack and then exposed to the environment with RH below 50%, the chloride migration from the inner to the surface layer was more obvious than that from the surface layer to the inner layer, and an obvious increase in the surface chloride content could be observed in concrete at the early period of exposure. However for the concrete subjected to the external RH above 75%, the chloride migration by concentration difference played a key role in the chloride distribution in concrete, and the surface chloride content decreased and the inner chloride content increased with increasing exposure duration; finally, the chloride content in surface layer and inner layer was tended to be the same.(3)For chloride migration under the coupling effect of water convection, the chloride migration was significantly impact by the water convection when the chloride penetration depth was below 6 mm, whereas the chloride migration by concentration difference played a leading role in the chloride distribution in the inner layer of concrete (above 6 mm). The concrete properties (w/c), chloride attack duration, and water convection duration all had an obvious impact on the chloride distribution in concrete, and there was an obvious difference on the chloride distribution by water convection and concentration gradient.

Data Availability

We confirm the data are available in this manuscript. The data in this manuscript were obtained through a series of tests. The related data used to support the findings of this study are available from the corresponding author upon request.

Conflicts of Interest

We confirm that there are no any conflicts of interest in this paper.

Acknowledgments

The authors gratefully acknowledge the substantial support of ongoing projects titled “Project 333” of Jiangsu Province (BRA2017273) and China Postdoctoral Science Foundation (2019M651579).

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Copyright © 2020 Fangzhi Zhu et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

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