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Schematic freeze – thaw cycle 

Schematic freeze – thaw cycle 

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This article outlines the combined effects of saltwater and water flow on deterioration of concrete under freezing and thawing cycles. In order to simulate the real freezing situation that concrete usually undergoes, four sets of experimental exposure conditions were designed. These exposure conditions include plain flowing water, flowing saltwater...

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... the pore is connected to the surface through pores in which the pore solution freezes at a higher temperature than the actual one. The salt concentration may be increased locally owing to segregation of salt ions. The next step in the formation of ice is redistribution of pore solution when the temperature ranges between À 5°C and minimum temperature of the frost cycle (Kaufmann 2004). Local supercooling occurs if large pores or whole pore regions are connected to the ice front through smaller “ neck ” pores only. Especially, highly porous border zones around aggregates and porous non-frost-resistant aggregates might be separated from the ice front through smaller cement matrix pores leading to high hydrostatic pressure (Fagerlund 1997) when reached by the ice front. The thermodynamic equilibrium in the pore solution is disturbed by the ice formation (Scherer 1999). Because of the lower chemical potential, unfrozen pore solution, mostly in smaller pores or locally supercooled pore regions, flows toward the existing ice in the larger pores and freezes there. Liquid transport is also induced by a higher salt concentration ahead of the ice front (osmosis). This redistribution may induce internal shrinkage and additional hydrostatic pressures (Kaufmann 1999). Empty pore space, resulting from the bigger thermal contraction of ice than of the matrix, is refilled. At heating, the ice will expand more than the surrounding matrix, which induces additional tension. The lower the minimal temperature of the frost cycle, the stronger the tension. Additional tension also depends on the efficiency of the redistribution of the liquid (Kaufmann 2004). Water flow exists in the vicinity of many concrete structures during winter. When the temperature reaches 0°C, water flow does not allow the ice to form on the surface of concrete. According to the ice-formation procedure, freezing is mostly initiated from preexisting ice. As a result, it seems that water flow can slow down the formation of ice in concrete pores during the freezing cycle. This research aims to simulate the real freeze thaw exposure conditions that concrete usually undergoes. The effects of water flow on durability of concrete under freeze – thaw cycles, especially the combined effects of water flow and saltwater, are going to be examined. Usually, water flow exists in the vicinity of many concrete structures. In addition, deicing salt is commonly used for melting the frost and snow in cold regions. To simulate the water flow and the presence of saltwater, four sets of freezing and thawing exposure conditions were designed. These conditions include still plain water, flowing plain water, still saltwater, and flowing saltwater. Therefore, the damaging effects of water flow and saltwater, especially their combined effects, were examined. Two types of concrete with different water – cement ratio were prepared and submerged in each freeze – thaw condition. Weight change and compressive strength change of each sample were measured during the cycles. The concrete samples were prepared according to ACI 211.3R [American Concrete Institute (ACI) 2002]. Coarse aggregates were crushed stones (diameter ranging from 5 mm to 20 mm), and fine aggregates were natural river sand (fineness modulus of 2.6). Two types of concrete were prepared with water – cement ratios of 0.4 and 0.45 and a fine aggregate percentage of 0.45. Table 1 shows the major parameters of the mixtures. These ingredients were mixed for approximately 1 min and then water was added. Finally, the ingredients were mixed for approximately 2 – 3 min. Beams were cast in three approximately equal layers. Each layer was vibrated by using a vibrating table. The vibration was carried out until the bubbles stopped coming to the top. Lower water – cement ratio concrete samples were vibrated longer. For each concrete type, three beams with the dimensions of 70 × 10 × 10 cm were cast. All concrete samples were submerged in water and cured for 28 days. Because of the space limitations, 35 cores were drilled out of each concrete specimen with a diameter of 5 cm. Finally, 96 cylindrical samples with the dimensions of 5 × 10 cm were placed in four different freeze – thaw exposure conditions. In each exposure condition, 24 samples were submerged. After each seven cycles, weight changes in all the samples were measured. In addition, for measuring the compressive strength loss, three samples of each concrete type were tested after each seven cycles. To simulate the real freeze thaw conditions that occur in cold regions, four sets of experiments were designed. These include flowing plain water, still plain water, flowing saltwater, and still saltwater. Water flow was produced by an electromotor with a propeller. The motor rotated 2.4 times per second, providing slow water flow (0 : 2 m = s) to simulate the effects of flowing water in freezing – thawing cycles. Fig. 1 shows the set of the electromotor with the propeller, and Fig. 2 shows a schematic freeze – thaw cycle. In this research, 3% sodium chloride solution was used and samples were submerged in the solution during the freeze – thaw cycles. Because of the wide use of deicing salt for melting the snow or as a major component of seawater, salt is mostly available in freezing and thawing cycles. The samples were put in the freeze – thaw chamber that was planned to provide varying temperature ranging from þ 4 : 4°C to À 17 : 8°C. Both the freezing and thawing of the samples were conducted in water. The length of the cycles was considered as 24 h because the presence of deicing salt and water flow slows down the ice formation. This cycle length limited the practical number of freeze – thaw cycles, and 28 cycles were completed. Weight and compressive strength of the samples were measured before, during, and after the tests. Visual observation of the freezing condition and concrete deterioration was per- formed for each cycle. The comparison of the still plain water and flowing plain water showed that the most common deterioration in plain water was cracking, but the depth and number of concrete cracks in flowing plain water were significantly more than still plain water. In still plain water, the water surface freezes when the temperature reaches 0°C, and gradually, the depth of ice increases, but in flowing plain water, the water flow does not allow ice formation when the temperature reaches 0°C. In this situation, small ice particles form at the places in which the water flow is at the lowest level. Gradually, the ice formation continues forward to the highest water flow area. Finally, the ice stops the electromotor and a thin layer of ice forms on the surface. As the freezing cycles continue, the depth of this layer increases. The use of 3% sodium chloride in still saltwater showed that the deterio- rating effects of saltwater are more aggressive than water flow. In addition to cracking, samples underwent surface scaling, crumbling, and erosion. Freezing and thawing in flowing saltwater showed that the combined effects of saltwater and water flow are significantly more than other freeze – thaw conditions. Early deterioration of concrete occurred because of severe cracking and scaling. After four freeze – thaw cycles, many of the samples underwent great deterioration, and after seven cycles, complete deterioration of some of the samples happened. Furthermore, great chemical reaction occurred between concrete materials and saltwater. After four cycles, a white deposit of calcium carbonate sediment appeared because of rapid chemical reactions. The presence of water flow increases the rate and speed of chemical reactions. As a result, the rate of deterioration is more severe and faster under freezing and thawing cycles in the flowing saltwater exposure condition. Fig. 3 illustrates the formation of ice in flowing plain water, and Fig. 4 shows a white deposit because of chemical reactions between concrete materials and saltwater. Fig. 5 shows schematic types of samples ’ deterioration and their relative severity in different freezing conditions. Saturated surface dry (SSD) weight loss of concrete samples was measured as an important factor. After every seven cycles, samples were taken out of the container for weight measurement. At first, the samples were placed in a tub of tap water, and loose particles on the samples were removed gently by hand. Then, the samples were laid on a paper towel to dry, and if the sample was not too friable, it was blotted with paper towels. Samples were rotated periodically to facilitate drying of all faces. After 15 – 20 min, samples were weighed precisely. Figs. 6 and 7 illus- trate the weight change in types A and B concrete under different freeze – thaw conditions. As shown in Fig. 6, type A concrete with a water – cement ratio of 0.4 remained intact under freeze – thaw cycles in still plain water, flowing plain water, and still saltwater, but underwent 10% weight loss after 14 cycles in flowing saltwater and 100% weight loss after 28 cycles because of severe cracking and scaling. According to Fig. 7, Type B concrete with a water – cement ratio of 0.45 remained intact in still plain water, whereas it underwent a 24.37% weight loss because of severe cracking and scaling in flowing plain water. In addition, it lost 4.03% of its weight after seven cycles in still saltwater, 38.21% after 14 cycles, and 51.59% after 21 cycles. whereas it lost 78.37% of its weight just after seven cycles in flowing saltwater and 100% after 14 cycles. The comparison of Type A and B concrete samples shows that the lowering of the water – cement ratio has great influences on durability of concrete under freeze – thaw cycles. Results indicated that the presence of water flow or saltwater increases the deterioration of concrete, but the deteriorative effects of saltwater are considerably more than water flow on deterioration of concrete. The combined effects of ...

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... To evaluate the state of concrete structures and determine their carrying capacities, it is possible to make use of several of the structures' mechanical and physical attributes. The researcher carried out a static truckload test on a recently built bridge to determine how the bridge reacted when a truck drove over it [1][2][3][4]. The weight and compressive strength of the samples were evaluated both before and after the freeze-thaw cycles, and the findings were analyzed. ...
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An engineering assessment was performed on concrete cubes casted from M25 concrete for checking the efficiency of non-destructive testing methods namely Schmidt’s rebound hammer test and Ultra Sonic Pulse Velocity test. The study was aimed at checking the viability of these above named non-destructive tests. Firstly, in the case of undamaged concrete structures and later on in the case of concrete structures damaged by fire, and then to compare the results to find out the efficiency of non-destructive testing methods. It is assumed that in the case of an undamaged structure the concrete is a homogenous mixture with equal strength at all depths. Hence, the non-destructive tests even if they are able to measure the surface strength like in case of the rebound hammer test may give a pretty accurate value when compared to the compressive tests performed in the laboratory. In the case of a structure, which has been damaged by fire, the concrete may no longer be homogenous at all depths and there might be considerable changes in its internal structure. Hence, this study is an attempt to carry out non-destructive tests on such concrete samples, which have been damaged by fire and then find out the viability and accuracy of the results when compared to the compressive tests performed in the laboratory.