1. Introduction
In ordinary concrete, which is a composite due to its structure, there are two basic phases, i.e., cement matrix and aggregate grains, which are included in the structure of the paste [
1,
2]. The matrix in a concrete composite, which is a continuous phase, is susceptible to moisture, temperature, and corrosion. However, rigid grains of aggregate, as fillers in the concrete composite structure, are characterized by their resistance to environmental influences and the independence of their properties from working time [
3,
4,
5].
In concrete, the volume of aggregate is on average 60% to 80% [
6,
7,
8,
9,
10,
11]. This means that both concrete type and grain size are two of the basic factors that have a significant impact on concrete features as follows [
12,
13,
14,
15,
16,
17]:
Moreover, aggregates are relatively cheap compared to other components of concrete. This means that, whenever possible, they are also used to reduce the total cost of the construction materials [
18,
19]. All the above factors mean that the characteristics of aggregates are necessary for the design and prediction of important features of cement concretes [
20,
21,
22].
In Poland, as well as in most European Union countries and the USA, for the production of concrete, usually mineral aggregates are used as coarse aggregates [
7,
23]. These are fillers obtained from rock massifs, as opposed to artificial aggregates, mainly derived from industrial waste such as gravelite, shale, aluminoporite, ashburst, foamed slag, etc. [
24,
25]. There are two basic groups of mineral aggregates [
26,
27,
28,
29]:
Natural aggregates;
Crushed aggregates.
A natural aggregate is created from the crumbling of rocks caused by the forces of nature, mainly rock erosion. A group of these aggregates includes, among others, sands, sand–gravel mixes, and gravels [
30,
31,
32]. In turn, a crushed stone aggregate is created from the fragmentation of rocks as a result of intentional human activity. Aggregates belonging to this group are mainly granites, limestones, and dolomites. The remaining crushed stone aggregates come from rocks: sandstones, diorites, basalts, and gabbro [
33,
34,
35,
36,
37].
Among mineral aggregates, gravels constitute the largest share in the production of concrete, which is understandable due to their price and availability [
38,
39,
40,
41,
42]. The remaining part consists of crushed stone aggregates. It is estimated that in the USA mineral aggregates used for concrete account for more than 90% of all types of aggregates used (approximately 50% are gravels and the rest are crushed stone aggregates, of which 66% are crushed aggregates from carbonate rocks). However, in Poland and the European Union, 97% of mineral aggregates are used for concrete, including 65% from gravel and 35% from crushed aggregates, from which 20% are derived from carbonate rocks [
6,
7,
23]. Aggregates obtained from carbonate rocks are usually limestones or dolomites [
43,
44,
45].
Because in modern concrete technology, aggregates belonging to both groups discussed above, i.e., both natural and crushed aggregates, are used to a large extent, this article presents in-depth research results on the important material characteristics of concrete composites made using various types of mineral aggregates. The article focuses on the assessment of the fracture toughness of concretes made of aggregates from various types of rocks [
46,
47,
48]. In addition, in this study, analysis has been performed on the zones of the composites where damages occurred and on how the process of intra-material cracks propagated in the concrete structure [
49,
50,
51,
52,
53].
It should be noted that such research is important both from a scientific and engineering point of view. This is due to the fact that possible changes in both the basic strength characteristics of concrete composites and their other specific parameters and properties, e.g., brittleness, tendency to develop structural damage, or fracture toughness, are strictly dependent on the characteristics of coarse aggregate grains as follows [
52,
53,
54,
55,
56]:
2. Properties of Mineral Aggregates in Terms of Susceptibility of Concrete to Brittle Fracture
The quality of aggregates is determined by the conditions of their formation, as well as the geological characteristics and mineral composition of the rocks from which they are obtained [
4,
57,
58,
59]. A detailed breakdown of mineral aggregates depending on their genetic and petrographic origin is presented, e.g., in [
6]. In addition to the petrographic characteristics, their external features such as the size, shape, and texture of the grain surface are also important [
6,
60,
61]. These properties determine their adhesion, and thus the structure of the ITZ between the coarse aggregate and the paste [
62,
63,
64].
The shape of the grains of natural aggregates is usually spherical, oval, very rounded, rounded, or irregular, while the shape of crushed stone aggregates is elongated, thickset, flat, or angular [
6]. The share of flat and elongated grains in the crumbs pile negatively affects the workability of the concrete mix, which reduces the tightness, frost resistance, and strength of the concrete. In addition, such grains have a larger surface area in relation to the volume, which has a negative impact as it causes the unnecessary increase in the amount of cement in concrete [
65,
66,
67]. Based on [
6,
68,
69], it was found that the most beneficial effect is achieved when the shape of the aggregate grains is similar to a sphere or cube. This reduces the friction between the paste and the aggregate, which results in better workability of the concrete mix and an increase in the tightness and strength of the composite. According to [
6], the void content of the aggregate decreases from about 40.5% in the absence of rounded grains in the crumb pile to 34% with the content consisting of 100% spherical grains. The resulting reduction in intergranular voids also affects the apparent density of concrete, which consequently improves its mechanical and strength parameters, and reduces its susceptibility to possible damage [
47,
70,
71,
72].
The second important parameter that describes the structure of aggregates is their texture. It determines the adhesion of grains to the cement paste and influences the water demand for the concrete mixture. Texture also has an impact on the strength of concrete, mainly bending strength [
6,
22,
73,
74]. Grains of natural aggregates usually have a smooth texture, while crushed aggregate grains have a rough or crystalline texture. A rougher texture results in greater adhesion forces between the aggregate grains and the cement paste. The above conclusion therefore proves that crushed aggregates have a higher adhesion than natural aggregates [
75,
76]. This is determined by the rougher surface of these fillers. It enables the mechanical bonding of the inclusions in question at the contact surfaces with the cement matrix [
6,
10,
77,
78].
Another factor that has a significant impact on the increase or decrease in aggregate adhesion is the share of mineral dusts with a diameter below 0.063 mm in the cement paste. Such dusts, in most cases, adversely affect the properties of the concrete mix and concrete, as they increase water demand and surround the aggregate grains, hindering the direct access of the cement paste. The exceptions here are fillers obtained from carbonate rocks. Limestone or dolomite powders increase the tightness and strength of the concrete [
6,
79]. It has also been observed that in the case of carbonate aggregates their favorable chemical and physical composition causes the formation of chemical bonds on their surfaces, which positively affects adhesion [
6,
80,
81]. In addition, the use of granite powder as a partial substitute for fine aggregates also has a beneficial effect on improving the strength properties of concrete [
82,
83].
In previous studies on the influence of the type of coarse aggregate on the strength and mechanical parameters of concrete and its fracture toughness, it was found that the dominant role here is played by the features of the aggregate discussed above, and the adhesion between the aggregate and the paste [
84]. The above factors also affect the structure of the ITZ between the coarse aggregate and the paste. On the other hand, this zone in concrete has a decisive influence on the fracture behavior of the construction material.
Thus, recapitulating the above considerations, it should be stated that the adhesion of hardened cement paste to the coarse aggregate and, consequently, the fracture toughness of concrete is influenced by such features of aggregates as: mechanical bonding of the paste to the aggregate surface, the formation of chemical reaction products between these materials, and capillary adhesion between the aggregate and the paste. The fourth factor that can determine the formation of strong ITZs in the structure of concrete is the so-called epitaxy phenomenon, which is a chemical process that causes the construction and growth of new crystal networks on the surface of aggregate grains. This phenomenon is usually observed in chemically reactive aggregates and can intensify the strengthening of the ITZ zone in concretes with fillers of this type [
28]. Considering the above,
Figure 1 shows schematically all the factors determining the ITZ in cement concretes, which have a direct and indirect effect on the susceptibility of concrete to cracking.
With regards to testing the strength parameters of concrete, for example, it was observed that crushed granite and crushed basalt performed best at compression than those made with natural gravels of similar grading [
85,
86]. Moreover, the highest compressive strength was achieved from concrete containing crushed quartzite, followed by concrete containing river gravel [
86]. Similarly, the study presented in [
87,
88] for different grades of concrete revealed that the highest compressive strength was achieved by all grades of concrete containing 12 mm quartzite, followed by concrete containing granite and river gravel. However, according to [
89,
90], the type of coarse aggregate used has a great influence on the strength and elasticity modulus of ordinary and high-performance concrete.
The results of the first studies analyzing the impact of the type of aggregates used on the parameters of concrete fracture mechanics using the first model of cracking [
91,
92] showed that the values of the fracture energy (
GIc) and the critical stress intensity factor (
KIc) are higher in the case of concretes made of high-strength aggregates, e.g., crushed stone aggregates, obtained from igneous or carbonate rocks, than weaker ones, e.g., gravels or gravelites [
91,
92]. A beneficial effect on the values of fracture mechanics parameters when using aggregates from igneous rocks is demonstrated in [
33,
34,
93,
94,
95]. On the other hand, the high fracture toughness of concretes made of limestone aggregates in comparison to gravel concretes was confirmed, e.g., in the tests described in [
34]. The favorable fracture toughness results obtained for concrete with limestone aggregate resulted from the physical and chemical reactions occurring in the ITZ area between the coarse aggregates and the paste [
80]. These reactions improved bond strength between paste and limestone aggregates [
96].
The influence of the type of aggregate used on the parameters of the concrete fracture mechanics, using the first model of cracking, was also discussed in the works [
97,
98,
99,
100,
101,
102]. In these studies, composites with dolomite and gravel fillers were analyzed. Additionally, the addition of silica fume (SF) was used to strengthen the structure of the composites. The results of the conducted research showed that the highest
KIc and critical crack tip opening displacement (
CTODc) values appeared for dolomite concretes containing 10% SF, while the lowest values were in the case of gravel concretes without the addition of active SF [
97,
98].
In turn, in work [
99], the influence of six different types of coarse aggregate on the fracture energy values of ordinary concretes was studied. The following types of aggregates were taken into account: dolerite, dolomitic limestone, granite, limestone, quartzite, and river grave. The obtained results of the experiments showed that the highest fracture toughness was in the case of concretes made with a granite and limestone aggregate, while the lowest fracture toughness was for concrete with gravel aggregate, and puzzlingly, dolomite aggregate. The relatively low fracture toughness of concrete with dolomite aggregates was due to the smooth grain surface of this aggregate. This, in turn, resulted in a weakening of the ITZ between the aggregate and the paste and, consequently, lower fracture toughness values for this material [
100].
At this point, it should also be noted that research has also been carried out so far on the influence of the type of coarse aggregates on the fracture toughness of cementitious concretes using the second model of cracking [
93,
101,
102,
103], and the assessment of the destruction surface of concretes made of various aggregates using the fractal technique [
104,
105] and digital image correlation technique [
106,
107]. Moreover, the influence of the type of coarse aggregate in the context of improving the fracture toughness of concretes intended for road construction was also assessed [
78,
108,
109,
110].
Analyzing the previous publications in this field, it should be stated that the results of tests on fracture toughness of concretes made using various types of aggregates presented in the literature are ambiguous. In addition, they do not contain the full range of data on the scope of fracture toughness of such materials. There is also a lack of detailed information about the processes of initiation and propagation of cracks depending on the type of aggregate used.
In addition, the results to date on the fracture toughness of concretes with different aggregates mostly refer to the analysis of only one selected fracture mechanics parameter, usually in terms of linear fracture mechanics. To date, the most commonly analyzed parameter has been the critical stress intensity factor or fracture energy. However, the literature lacks research results that comprehensively analyze the effect of the type of coarse aggregate on the parameters of both linear and nonlinear fracture mechanics of concretes. In addition, there is no clear indication in the literature as to which of the factors, listed in
Figure 1, significantly affect the fracture toughness of concretes made using different types of coarse aggregates.
Therefore, it was proposed to undertake experimental research in this area. The aim was to accurately assess the impact of the type of mineral aggregate on the values of the basic parameters of the fracture mechanics of ordinary concretes, in both linear and non-linear terms. In order to obtain the most reliable comparison of the obtained test results, mineral aggregates, both natural and crushed, from the same geographic area were used in the experiments [
111].
5. Discussion of the Obtained Research Results
The type of coarse aggregate used, in addition to factors such as the aggregate’s grain size and its volumetric content, have a decisive impact on the fracture toughness of concrete and the characteristics of its fracture process. Therefore, this article attempts to determine the impact of four different types of coarse mineral aggregates as follows:
Values of the basic parameters of fracture mechanics in linear and non-linear terms, i.e., and CTODc;
Places of the first microcracks occurring in each material;
The course of the development process of structural microcracks that determined the destruction of the concrete composite.
In addition, the impact of coarse aggregates used on the basic concrete strength parameters, i.e., fcm and fctm, was also examined, and the brittleness index was calculated for each material, i.e., BI. In order to characterize the impact of selected types of coarse aggregate on the analyzed processes in the most holistic approach, fillers significantly different from each other were used to make the concretes. Differences between the individual aggregates occurred in relation to the way in which they were formed, the rock massifs from which they were obtained, and the important feature from the point of view of fractures development in the concrete, i.e., the characteristics of the surface of their grains. What is important, all aggregates used had very close grain size distributions.
Aggregates with the following important features were used to make the concretes (
Table 2):
Natural gravel aggregate with a low strength of 34 MPa, and smooth and rounded grains;
Crushed, chemically reactive limestone aggregate with a quite high strength of 100.2 MPa, and a rough grain surface;
Crushed, not chemically reactive granite aggregate with a high strength of 115.8 MPa, and a rough grain surface;
Crushed, not chemically reactive basalt aggregate with a very high strength of 142.5 MPa, and a rough grain surface.
Analyzing the obtained test results for mechanical parameters, one can see a clear improvement in all concretes made of crushed stone aggregates. In the case of all series of concretes, made both on limestone aggregate obtained from carbonate rocks and aggregates obtained from igneous rocks, i.e., granites and basalt, both the fracture mechanics parameters, and CTODc, as well as the strength parameters, fcm and fctm, were clearly higher than the values obtained for concrete with a gravel aggregate.
Moreover, based on the analysis of the relationships presented in
Figure 9, a clear correlation of changes in the obtained results between the strength parameters and the fracture mechanics parameters can be seen. However, it is worth noting that the impact of the applied change in the structure of the material, consisting of the replacement of the gravel aggregate with crushed stone aggregates, was more clearly visible in the case of changes in the values of fracture mechanics parameters (
Figure 6 and
Figure 9).
The obtained results on mechanical parameters were rather expected, because as shown in previous works, both the shape of crushed stone aggregate grains, their texture, and the properties of the rocks from which they are obtained have a decidedly positive effect on improving the parameters of concretes [
4,
5,
55,
56,
66,
130,
131]. However, the level of the beneficial effect resulting from the replacement of pebble aggregate with crushed stone aggregates varied depending on its type.
Based on the results shown in the graphs of relative changes in the analyzed parameters, it can be seen that the strength indexes have improved in the range from several percent for concrete with limestone aggregate to over 40% for concrete with basalt aggregate (
Figure 5). However, in the case of fracture mechanics parameters, the benefits from the change in the type of coarse aggregate ranged from 20% for C–LM series concrete to over 70% for C–BA series concrete (
Figure 9).
Such results confirm the theses and conclusions resulting from other previous studies. They showed that the applied material modification of concrete, and in particular the change in its basic component, i.e., the type of coarse aggregate, has a much more significant impact on the parameters of the fracture mechanics of the concrete. However, changes in the values of strength parameters as a result of such activities are noticeable to a lesser extent [
34,
81].
Differences in percentage changes between the strength parameters and the fracture mechanics parameters result from the fact that the change in the coarse aggregate used has a stronger impact on the process of damage and destruction of the concrete, and consequently, on the parameters describing this phenomenon.
Therefore, in order to correlate the values of fracture mechanics parameters with the process of development of fractures in the structure of materials, their brittleness has been assessed. Also, an inspection of the cross sections’ destruction of the concrete samples after the fracture toughness test has been performed. The analysis of the research material showed a strict dependence of the concrete brittleness index and the nature of the beam fracture on the type of coarse aggregate used to prepare the samples (
Figure 10).
However, on the basis of macroscopic examination of the sample fractures, it was found that in the process of their destruction, three phenomena occurred as follows:
The phenomenon of decohesion in the ITZ area is dominated by the forces of cohesion between the aggregate and the paste. These forces are most often the result of the mechanical interlocking of paste particles with the rough surface of the aggregates. In addition, in the case of chemically reactive aggregates they can be strengthened with chemical reaction products, causing the formation of additional bonds in the ITZ rea (
Figure 1).
In the cross-sections of concrete samples, the largest signs of decohesion were observed in C–GL series concrete. The contact areas of smooth gravel grains were clearly exposed, with clear damage in the ITZ areas. In addition, in the concrete of this series, damages in the cement matrix were also visible (
Figure 10a).
Concrete of the C–LM series had much better cohesion at the boundary of paste and coarse aggregate. Damages in the ITZ area of this material were visible to a lesser extent than in the case of gravel concrete. In the structure of this material, through-fractures across the grains appeared in a small number (
Figure 10b). The compactness of the material in the ITZ area of these concretes was the result of both the rough surface of the limestone aggregates and the presence of chemical reaction products of the aggregate with the paste, as well as the presence of epitaxial crystals on the grain surface of these fillers.
However, in the case of both series of concretes made of aggregates derived from igneous rocks characterized by high strength parameters, i.e., C–GT and C–BA, the process of samples destruction was mainly the result of damage occurring through the grains of the coarse aggregate. This way of destruction proves the high brittleness of both concretes (
Figure 6) and the high level of cohesion in the ITZ area of these materials. However, the cohesion between the grains of granite and basalt aggregates with the paste was mainly the result of the favorable properties of these aggregates, and their rough texture. The rough lamellar surface of basalt and granite aggregates clearly improved the properties of the ITZ area and increased the fracture toughness of concretes with these aggregates. It should be noted that due to the very beneficial properties of aggregates derived from igneous rocks, they are often used as a filler in high-performance and ultra-high-performance concretes [
79,
122], and road concretes [
100,
101,
102,
103,
132].
In order to determine the exact reasons for the fracture toughness results obtained, an additional in-depth structural evaluation of all concretes was carried out after the experiments. Based on the comprehensive analyses of the failure surfaces of each of the analyzed materials (
Figure 10) in conjunction with their fracture mechanics parameters (
Figure 8), an attempt was made to determine which characteristic features of each aggregate had a decisive influence on the obtained test results.
On this basis, it was found that the high values of both
and
CTODc were determined in the case of basalt concretes by the strength of the aggregate itself and the “lamellar” shape of the basalt grains, which behaved like wedges in the process of material failure (
Figure 10d). These aggregates worked similarly to dowels in concrete structures in the process of force transmission in the concrete structure. Therefore, they could further reduce the spreading forces present in the material structure. This is evidenced by the observation of basalt grains very well bonded to the structure of the cement matrix (
Figure 10d). Thanks to these characteristics, basalt aggregates clearly delayed the fracture processes of C–BA series concrete, resulting in its best fracture toughness (
Figure 8).
The characteristics of the granite aggregates, such as their high strength and varied surface, had a similar effect on the fairly high fracture toughness of the C–GT series concrete. This implied the formation of compact interfaces in the ITZ area between granite grains and the paste, as observed in
Figure 10c. Consequently, this resulted in a clear improvement in the fracture toughness of this concrete (
Figure 8).
On the other hand, decidedly different characteristics of the aggregates determined the fracture toughness of the C–LM series concrete. In addition to the well-developed and varied grain surface of these aggregates (
Figure 10b), the chemical reactivity of the limestones and their unique and specific epitaxial features (
Figure 8) influenced the rather high values of the fracture mechanics parameters of this material.
In contrast, the low fracture toughness of the C–GL series of concrete was the result of the poorly developed and unshaped surface of the spherical gravel grains. Aggregates of this type, additionally characterized by low mechanic parameters (
Table 3), were not able to form sufficiently strong interfaces in the ITZ area between gravel grains and the paste. This resulted in the formation of decohesion cracks in this area of the concrete, as shown in
Figure 10a. The consequence was a marked decrease in the fracture toughness of this material in both linear and non-linear terms (
Figure 8).
A summary of the data including the results of the tests of fracture mechanics parameters and the assessment of fracture processes of concretes made of aggregates from various types of rocks is presented in
Table 7.