OJCE  Vol.7 No.3 , September 2017
Non-Destructive Imaging of Water Permeation through Cementitious Materials Using MRI
ABSTRACT
In this study, water permeation through cementitious materials was observed using magnetic resonance imaging (MRI). The influence of cement type on the magnetic resonance signal was studied subsequent to determining the parameters required for imaging. Consequently, adequate imaging of water permeating through hardened cement paste (HCP) made with white Portland cement was achieved, while water permeation through ordinary Portland cement-based HCP yielded poor signal. HCPs maintained at various levels of relative humidity (RH) were observed, and the signal was detected only from those maintained at an RH of higher than 85%. The water permeation depths in HCP were observed by using MRI, and the measured depths were compared to those measured via a spraying water detector on the split surface of the specimens. As a result, good agreement was confirmed between the two methods. Additionally, MRI was applied to concrete specimens; although it was found that water was not detected when a lightweight aggregate was used, water permeation through concrete with limestone aggregate was detectable via MRI. MRI will help in understanding how water permeation causes and accelerates concrete deteriorations such as rebar corrosion and freezing and thawing.

1. Introduction

Water is known to yield deleterious effects on concrete structures. To observe the depth of water permeation through concrete, the concrete specimen can be split to measure the depth of the surface colour changes [1] [2] . However, the determination of water permeation depth in concrete is difficult because 70% to 80% of the split surface area is aggregate, and the colour change due to permeated water is generally only visible in the cement paste. Some researchers have cut concrete specimens and dried them to evaluate mass changes due to water transfer, and to determine the moisture distribution [3] . Alternatively, humidity sensors can be used to measure the moisture distribution [4] or water penetration depth in concrete [5] . Justnes et al. [6] and Pleinert et al. [7] applied neutron radiography to observe water in cementitious materials; however, it was found that the sample thickness had to be limited to a few centimetres to allow the neutron ray to completely pass through the sample. The above methods only yield one- to two-dimensional information.

In this paper, magnetic resonance imaging (MRI) was used to observe water permeation through concrete. MRI can acquire three-dimensional information because it receives radio-frequency signals from any position in the sample at which hydrogen atoms are present. Moreover, it is non-destructive and enables the observation of water movement in real time. However, a disadvantage of this method is that, as strong magnets are implemented, MRI cannot be applied to reinforced concrete because of the strong attraction of steel; additionally, magnetic materials such as steel bars cause distortion of the obtained images. In their study using MRI to observe concrete structures, Marfisi et al. [8] reported that magnetic components in ordinary Portland cement (OPC) affect the captured images. In addition, Marfisi et al. [9] employed MRI to evaluate fractures in concrete. They reported that limestone and quartz aggregates are preferred to observe concrete via MRI and that granite is not suitable. Kaufmann et al. [10] implemented MRI to observe water permeation through concrete specimens, but as they used OPC, the obtained images were not clear. It was found that deuterated water can yield marginal improvements in the image, but it is expensive. Additionally, Kaufmann et al. did not explicitly confirm whether the penetration depth captured via MRI was correct, as they merely calculated the depth via determination of mass increase due to immersion, which was accomplished by comparing the dry and saturated masses.

The objective of this paper is to study the applicability of MRI to the observation of water permeation through concrete. To begin, the necessary parameters for MRI were determined by evaluating the hardened cement paste (HCP) made with white Portland cement (WPC). WPC was used because magnetic components in OPC affected the captured image, as will be discussed in a later section. Then, HCPs made with WPC and maintained at various levels of relative humidity (RH) were observed via MRI to determine the threshold of water detection. Next, HPCs dried at various temperatures were soaked in water; the permeation depth was subsequently imaged via MRI, and the observed depth was compared to the depth as measured on the splitting surface. Lastly, concrete specimens with lightweight aggregate (LWA) and limestone aggregate (LSA) were prepared and observed via MRI to determine the effects of aggregates on the obtained images. Concrete with the commonly used granite aggregate was not studied because Marfisi et al. [8] has already reported that the obtained MRI image of concrete containing granite was distorted.

2. MRI Background Information (Hashemi et al. [11] )

The general principle of MRI is that it constructs images from the signal emitted from the hydrogen nuclei in the object under observation. To image, a strong magnetic field is first applied to the object. When an object containing hydrogen atoms enters the external magnetic field, the spin of the nuclei is oriented to the direction of the magnetic field; this direction is generally assumed as the Z axis. When a radio-frequency pulse with the same frequency as the proton spin is applied to the object, the axis of the spin inclines towards the X-Y plane, which is orthogonal to the Z axis. This inclination angle is called the flip angle. The inclined spin is recovered towards the Z axis after the radio-frequency pulse has ceased. Thus, MRI constructs images according to the signal that is emitted from the hydrogen nuclei as the spin recovers from the X-Y plane to the Z axis. The parameters describing the recovery of the Z-axis component (Mz) and decay of the X-Y-plane component (MXY) are T1 and T2, respectively. T1 and T2 show the relaxation curves expressed by Equation (1) and Equation (2), respectively.

(1)

(2)

T1 and T2 vary according to the mobility of hydrogen nuclei. The parameters for MRI observation must be optimized to obtain a clear image. The echo time (TE: time interval between radio-frequency pulse and signal acquisition) and repetition time (TR: time interval of radio-frequency pulse) are the most important parameters.

Marfisi et al. [8] used TE = 3.5 ms and TR = 100 ms to obtain MRI images of water in concrete. However, these TE and TR values cannot be used because these parameters vary according to the magnetic density. Marfisi et al. employed MRI with a magnetic density of 2 T, while the MRI used in this study applies 3 T. T2 is obtained only when a perfectly uniform external magnetic field is applied; however, as real external magnetic fields are always non-uniform, the actual acquired signal is denoted as, in distinction from T2.

3. Experimental Methods

3.1. Specimens

The material properties are shown in Table 1. HPCs of φ 50 × 100 mm and water-to-cement ratio (W/C) of 0.4 were respectively prepared using OPC and WPC. The specimens used to study the effects of RH via imaging were seal- cured up to 28 days following casting, and then maintained at a temperature of 20˚C under 60% RH for 1 month. These specimens were cut into 2-cm-thick slices via a water-cooling cutter and dried under conditions of 20˚C and 60% RH

Table 1. Material specifications.

for 2 weeks. Then, these cut samples were stored in desiccators at 76%, 85%, 98% or 100% RH for 1 month and subsequently imaged via MRI. After MRI, the samples were oven-dried at 105˚C for three days, and mass decrease of the sample due to drying was divided by the mass of the sample after it was oven-dried to evaluate moisture content. In a similar manner, HPCs used to evaluate the effects of cement type were seal-cured for 28 days subsequent to casting. These specimens were dried under conditions of 20˚C and 60% RH for 1 month, 40˚C and 10% RH for 2 weeks or 105˚C for 3 d. After drying, they were each soaked in 1-cm-deep water for 3 d in a covered container prior to imaging as shown in Figure 1. Then, the specimens were split and a water leakage testing agent, MORAYMILLE (TASETO, Kanagawa, Japan), was applied to measure the water permeation depth.

The material properties and mix design of the concrete specimens are provided in Table 1 and Table 2, respectively. WCP was used to prepare concrete specimens of φ 100 × 200 mm. Concrete specimens with LWA were demoulded 24 h after casting and dried at 105˚C for 6 d. The specimens were then soaked in 1-cm-deep water for 3 d and imaged via MRI. Three concrete specimens with LSA were cast; of these, two of them were demoulded 24 h after casting and dried at 105˚C or 20˚C (60% RH) until MRI imaging was performed at an age of 48 h. The remaining specimen was demoulded immediately prior to MRI imaging following 48 h aging. After imaging, the specimens maintained at 105˚C were once again stored at 105˚C, while the remaining specimens were stored in a 20˚C chamber under 60% RH. Once aged for 18 d, they were each soaked in 1-cm-deep water in an open-air container for 2 d prior to secondary imaging.

3.2. Pore Structure Analysis

The pore structure of the HCPs dried under conditions of 40˚C and 10% RH for 2 weeks was analysed via mercury intrusion porosimetry (MIP). The samples for MIP were collected from the HCP at depths greater than 2 cm from the surface. The collected samples were subsequently immersed in acetone for 24 h and dried for 24 h via the D-Dry method, in which the sample is equilibrated with ice at −79˚C, prior to performing MIP.

Figure 1. Schematic of water absorption (in covered container).

Table 2. Mix design.

3.3. Determination of T1 and

The MAGNETOM Prisma MRI (SIEMENS, Munich, Germany), equipped with a magnetic flux density of 3 T, was used for MRI imaging. To determine the optimum parameters for imaging the prepared samples, the relaxation times of T1 and were studied. T1 was calculated via the following equation.

(3)

In this study, the flip angles α1 = 11˚ and α2 = 56˚ were used to acquire the signals S1 and S2, respectively.

was determined by applying two different values of TE and subsequently solving the following equation to fit the signals obtained in the resulting image.

(4)

In this study, TE values of 0.87 and 1.2 ms were used, and the obtained MXYs were substituted into Equation (4) to determine. The resulting relaxation curves for T1 and are illustrated in Section 4.1 for TE and TR set to 1.19 and 8.4 ms, respectively. Although the resolution of constructed images can be improved by repeating acquired signals, a resolution (the size of an imaging voxel) of 1 × 1 × 1 mm was used in this study without repetition because this resolution is sufficient to measure the depth of water permeation through cementitious material. The required time to acquire a single image was approximately 2 min.

4. Results and Discussion

4.1. Determining Imaging Parameters

T1 and were studied to determine the optimum parameters for imaging. The signal intensity obtained with α1 = 11˚ and α2 = 56˚ were 181 and 697, respectively. Substituting these values into Equation (3) yields T1 = 6.88 ms. The signal intensity acquired by implementing TE = 0.87 and 1.2 ms were 2207 and 623, respectively. Subsequently, the value of obtained by substituting the above values into Equation (4) and performing fitting was 0.26 ms. These T1 and values are very short as compared to those of bulk water, which are each approximately 2500 ms [11] . Dissolved ions in water and small pores are known to decrease T1 and [8] [12] . Figure 2 shows the calculated relaxation curves for MZ and MXY assuming M0 = 1. MXY can be observed to decay faster than MZ; MXY decreased to one-thousandth of M0 at 1.8 ms; this indicates that TE and TR should be set small to acquire a strong signal. Thus, in this study, TE and TR were set to 1.19 ms and 8.4 ms, respectively.

4.2. Effects of Relative Humidity

Acquired images of specimens stored at various levels of RH are shown in Figure 3. Images of the specimens maintained at higher levels of RH are visibly clearer, as indicated by the contrast, while the specimens maintained at 76% and 85% RH do not yield a strong contrast. The masses of specimens maintained at 98% and 100% RH exhibited continuing increase at the time of MRI imaging. This result indicates that the specimens maintained at RHs of lower than 85% did not emit a sufficiently strong signal, and that stronger signals will be acquired from specimens maintained at 98% and 100% RH at constant mass.

Figure 2. Relaxation curves: MZ and MXY.

Figure 3. Images of cement pastes under various levels of RH.

The moisture contents of the samples stored at levels of 76%, 85%, 98% and 100% RH are shown in Figure 4. These results indicate that the volume having a moisture content of more than 0.19 was detected under the conditions in this study. However, it should be noted that the moisture-level threshold for detection obtained in this study may vary according to the MRI device and imaging parameters.

4.3. Comparison of Permeation Depth Observation Methods

In Figure 5, the images of HCP made with WPC acquired via MRI, and those of the split surfaces obtained via water leakage detection are shown. In the split surface images, the dark-coloured areas indicate positions of water detection by the water leakage testing agent. Comparison of the results of both methods reveals a good agreement on water permeation depth that is independent of the method of drying. Note that the colours in the captured images differ because the measured positions of the samples differed, which thus yielded a difference in acquired signal strength; the colour difference is not an indication of a difference in water content. Therefore, these results indicate that, although MRI can provide a non-destructive measure of water permeation depth, the distribution of water content may be difficult to acquire because, as shown in Figure 5, the signal strength varies according to position.

4.4. Effects of Cement Type on MRI Signal

No signal was acquired from the HCP made with OPC while water was observed on its split surface (Figure 6). Moreover, the permeation depth of HCP made with OPC was lesser than that of HCP made with WPC. This is likely due to the magnetic components in OPC inhibiting the signal such that no water was detected using the measurement conditions in this study [8] . Figure 7 illustrates the pore structures of HCP specimens comprising WPC and OPC that were dried under conditions of 40˚C and 10% RH for 2 weeks. HCP made with OPC exhibited a denser pore structure as compared to HPC made with WPC; this difference in porosity is suggested to be the cause of differing permeation depths.

Figure 4. Water content in cement paste as a function of RH.

(a) (b)

Figure 5. Comparison of MRI images of HCP made with WPC and splitting surface as obtained via a water detector. (a) Dried at 20˚C for 1 month; (b) Dried at 20˚C for 2 weeks.

Figure 6. Split surface of HCP made with OPC.

Figure 7. Pore size distribution in HCP.

4.5. Effects of Aggregate Type

We have not provided the captured image of concrete with LWA because no signal was acquired. The acquired images of concrete with LSA at age 48 h are shown in Figure 8. The seal-cured specimen exhibits a stronger signal than that cured under conditions of 20˚C and 60% RH. As these two specimens were identically positioned, the difference in signal intensity is directly proportional to the difference in water content; this can be confirmed by observing Figure 8(c), which shows that water was not detected in the sample dried at 105˚C.

Figure 9 shows the images of the concrete samples with LSA after having been soaked in water. It can be seen that water permeates deeper within the specimen cured at 20˚C in 60% RH than in the seal-cured specimen, while the specimen dried at 105˚C was found to have the greatest depth of water permeation. The water permeation profile was observed to be convex, deeper at the centre and shallower along the sides. This convex-shaped water front is presumed to be attributed to the drying of the side of the specimens, because, as shown in Figure 10, the specimens were soaked in water in a room maintained at a temperature of 20˚C and 40% RH. This result indicates that, in water permeation or water absorption test, the sides of the sample must be covered to prevent evaporation of the permeated water through the sides of the sample, thereby affecting the water permeation behaviour and causing it to differ from that observed in an actual concrete member.

(a) (b) (c)

Figure 8. Images of HC with LSA; age: 48 h. (a) Seal-cured; (b) 20˚C 60% RH; (c) 105˚C.

(a) (b) (c)

Figure 9. Images of HC with LSA after being soaked in water. (a) Seal-cured; (b) 20˚C 60% RH; (c) 105˚C.

Figure 10. Schematic of water permeation and evaporation in an open-air container.

5. Conclusions

Non-destructive imaging of water in cementitious material was performed by implementing MRI; the following results were obtained according to the conditions and parameters used in this study.

- T1 and, which yielded the relaxation curves for the signal acquired from HCP with WPC, were determined as 6.88 and 0.26 ms, respectively.

- The water permeation through HCP comprising WPC was detected via MRI. The resulting permeation depths as measured via MRI and a water leakage testing agent showing surface splitting demonstrated good agreement.

- In this study, HCP, which has a moisture content of more than 0.19, was detected via MRI.

- MRI was able to image the moisture loss and water permeation through concrete with LSA, but not in concrete with LWA.

The water permeation depth in concrete with LSA was detected via MRI. The permeation depth increased as the concrete dried, yielding a convex-shaped water front, which is indicative of evaporation of permeated water through the sides of the specimen.

Acknowledgements

The authors would like to thank Dr. Hironori Nakatani at the Center for Evolutionary Cognitive Sciences at the University of Tokyo and Mr. Katsutoshi Murata at Siemens Healthineers Japan for setting the protocol for MRI. The lime stone aggregate was provided by Sumitomo Osaka Cement. This study was supported by a research grant from the Japan Concrete Institute.

Cite this paper
Sakai, Y. , Yokoyama, Y. and Kishi, T. (2017) Non-Destructive Imaging of Water Permeation through Cementitious Materials Using MRI. Open Journal of Civil Engineering, 7, 378-388. doi: 10.4236/ojce.2017.73026.
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