Gradation-Based Framework for Asphalt Mixtures Licentiate Thesis Bernardita Lira Miranda KTH, Royal Institute of Technology School of Architecture and Built Environment Department of Transport Science Division of Highway and Railway Engineering SE-100 44 Stockholm April 2012 TRITA-TSC-LIC 12-001 ISBN 978-91-85539-81-9 ©Bernardita Lira 2012 Abstract Asphalt mixture microstructure is formed by aggregates, bitumen binder and air voids. Aggregates make for up to 90% of the mixtures volume and the structure formed by them will depend mostly on their size distribution and shape. The study presented in this thesis has as main objective to develop a framework that allows the characterization of asphalt mixtures based on the aggregates gradation and its impact on pavement performance. Moreover, the study aims to identify the range of aggregate sizes which form the load carrying structure, called Primary Structure, and determine its quality. The method has been developed as a numerical procedure based on packing theory of spheres. Parameters like porosity, coordination number and disruption factor of the Primary Structure; and a binder distribution parameter for the different sub-structures have been used to evaluate the quality of the load carrying structure and predict the impact on several failure modes. The distribution of bitumen binder has been derived from a geometrical model which relates porosity of the mixture with film thickness of particles considering the overlapping reduction as the film grows. The model obtained is a closer approximation to a physical characteristic of the compacted mixture separated according to different elements of the structure. The framework has been evaluated on several field and laboratory mixtures and predictions have been made about their rutting performance and moisture resistance. The calculated parameters have compared favourably with the performances reported from the field and laboratory testing. The developed gradation analysis framework has proven to be a tool to identify those mixtures with a poor rutting performance based on the gradation of the aggregates. The Gradation - Based Framework has satisfactory distinguished between good and bad performance of asphalt mixtures when related to permanent deformation and moisture damage. The calculated parameters have allowed identifying and understanding the main mechanisms and variables involved in permanent deformation and moisture damage of asphalt mixtures. The developed model can be used as a tool to determine the optimal gradation to assure good performance for hot mix asphalt pavements. Keywords: Asphalt, aggregate gradation, packing theory, asphalt microstructure, porosity, film thickness, rutting, moisture damage. i Acknowledgment The work presented in this licentiate thesis has been carried out between June 2009 and February 2012 at the division of Highway and Railway Engineering, School of Architecture and the Built Environment at the Royal Institute of Technology, KTH. I would like to express my gratitude to Trafikverket for the financial support to the project. I would also like to thank my supervisors Professor Björn Birgisson and Dr. Denis Jelagin for their guidance during this process. I am very grateful to Mr Måns Collin and Dr. Per Redelius for all the great discussion that helped us understand and develop the final model. I would like to thank my colleagues at the department which were always there to put a smile in the difficult times. Also, nothing would have been possible without the invaluable help of Mrs Agneta Arnius in all the administrative matters. Finally, I would like to thank my husband Kristian for his support and patience and my family in Chile that always believed in me. Bernardita Lira Stockholm, February 2012 iii List of enclosed papers I. Lira, B., D. Jelagin, B. Birgisson, Gradation Based Framework for Asphalt Mixtures Submitted to Journal of Materials and Structures, October 2011 II. Lira, B., D. Jelagin, B. Birgisson, Binder Distribution Model for Asphalt Mixtures Based on Packing of the Primary Structure To be submitted to International Journal of Pavement Engineering v TABLE OF CONTENTS Abstract Keywords Acknowledgements List of enclosed papers 1. Introduction 2. Theoretical Model 3. Results 4. Discussion and Conclusions 5. Bibliography Paper I. Gradation-Based Framework for Asphalt Mixtures. Lira, B., D. Jelagin, B. Birgisson Paper II. Binder Distribution Model for Asphalt Mixtures Based on Packing of the Primary Structure. Lira, B., D. Jelagin, B. Birgisson vii 1. Introduction The impact of aggregate gradation on the performance of asphalt mixtures has been extensively studied through the years. Several studies, e.g. (Kandhal, et al., 1998), (Nukunya, et al., 2001), (Birgisson, et al., 2004) have shown that there is a relationship between aggregate particles size distribution and the resistance to cracking, rutting, ageing and moisture damage. Furthermore, the way that aggregate particles, bitumen binder and air voids interact with each other will determine how a mixture will respond to different loading conditions ( (Campen, et al., 1959), (Kumar & Goetz, 1977)). Through studying and understanding these interactions future design can be optimized by combining the available materials in the best possible way. The objective of the present project is to develop a framework to characterize asphalt mixtures based on their microstructure. Asphalt mixture microstructure is formed mostly by aggregate particles and the structure that will be formed depends mainly on their size distribution, shape and concentration. Bitumen binder will then flow around the particles forming a film around them and binding all the components together. The framework aims to describe different types of mixtures depending on how the aggregates group, how the bitumen is distributed among them and the resulting size and location of the air voids. This configuration will finally determine the type of response that an asphalt mixture will have during loading. Experimental studies on granular material (e.g. Cundall, et al. 1982) have shown the existence of stress-transmitting paths enclosing virtually stress free regions (Jaeger and Nagel 1992). In particulate materials then, the load is transferred through chains of particles and other smaller particles play the secondary role of preventing the main chain from buckling (e. g. Santamarina 2001). Based on the observations mentioned above two substructures within the aggregate particles have been defined: the Primary Structure, range of sizes which due to their concentration provide the load bearing capacity of the mixture, and the Secondary Structure, material smaller than the first one which provides stability to the structure (Lira, et al., 2011). Packing theory for spherical particles has been used to identify each sub-structure. Results from field and laboratory mixtures have been used to validate the relationship between the Primary Structure content and rutting performance. The model also proposes a distribution system of the bitumen binder around the Primary and Secondary Structure. It is shown that the thickness of the film around both structures has a great influence on not only permanent deformation but also on the resistance for moisture damage on asphalt mixtures (Lira, et al., 2012). 1 2. Theoretical Model Mineral aggregates used for pavement construction are largely obtained from local suppliers. A consequence of this is that certain regions will have better quality materials than others. It is for this reason that is of key importance to understand the way aggregate particles interact, and in that way give a tool to engineer mixtures to obtain the best performance possible according to the available materials. Aggregate´s physical characteristics, such as resistance to abrasion and strength, are determined primarily by its mineral composition. However, the production process can significantly improve the quality of the aggregate by elimination of weaker rock layers and by the effect of crushing on the particle shape and gradation of the aggregate. Aggregate gradation is the distribution of particle sizes expressed as a per cent of the total weight. Gradation is determined by sieve analysis and is normally expressed as total per cent passing various sieve sizes. Aggregate gradation is certainly one of the most important properties of an HMA (hot mix asphalt) design. It affects almost all the important properties of an asphalt mixture, including stiffness, stability, durability, permeability, workability, fatigue resistance, friction, and resistance to moisture damage (Brown, et al., 2009). Early studies have proposed that the best gradation for HMA is the one that gives the densest packing, increasing stability through increased interparticle contact (Fuller & Thompson, 1907) (Goode & Lufsey, 1962). However, there must be sufficient air void space to allow enough bitumen binder to be incorporated to ensure durability and workability, while still leaving some air voids in the mixture to avoid bleeding or rutting. In 2006 a conceptual and theoretical approach to evaluate coarse aggregate structure based on gradation was developed by (Roque, et al. 2006). The method identifies the load carrying size range (DASR) in the mixtures and relates the quality of this structure to the asphalt mixture performance. However, the DASR identification procedure is valid strictly for gradations composed of discrete particle size with a size ratio 2:1. Packing theory is a tool that allows the analysis of aggregate gradations based on the geometrically systematic arrangement of uniform spheres. The term packing is applied to any manner of arrangement of solid units in which each constituent unit is supported and held in place in the earth´s gravitational field by tangent contact with its neighbour (Graton & Fraser, 1935). From a two-dimensional geometric view there are two different types of layers, a square and a rhombic layer, as shown in Figure 1. When combining those two different layers in a three-dimensional space, six different arrangements are obtained. It can be observed in Table 1 that only four are presented as some of the square arrangements are repeated by the rhombic ones. By observing the values of porosities it can be determined that the simple cubic packing is the loosest state and the rhombohedral packing is the densest one. 2 Table 1. Properties of various packing arrangements Tangent neighbours Volume of the unit cell Volume of unit void Porosity Simple Cubic 6 8,00 R3 3,81 R3 47,67% Orthorhombic 8 6,93 R3 2,74 R3 39,54% Tetragonal – sphenoidal 10 6,00 R3 1,81 R3 30,19% Rhombohedral 12 5,66 R3 1,47 R3 25,95% Figure 1. Types of layer. A) Square layer; B) rhombic layer (Graton & Fraser, 1935) For an assemblage of equal-sized particles to be in contact with each other then they must have porosity not higher than the loosest state given by packing theory. In order to transfer load, stones need to form a continuous network, which means, the concentration of the load carrying range has to be minimum around 45%. Concentration can be defined as follows: Wretn Wtot [1] where Wretn represents the weight of aggregate retained at sieve n and Wtot is the total weight of aggregates. Based on standard practice is acceptable to assume that such a concentration is not achieved by only one size material in a gradation. Packing theory can be used to define the range of material where stone-to-stone contact is assured and a concentration higher than 45% can be achieved. This analysis is done by checking the interaction between consecutive sieve sizes and determining if their individual concentrations are enough to assure contact between particles of both sizes. For this analysis four initial assumptions are taken: All particles are considered spherical. The aggregate particles are uniformly distributed within the total volume. 3 The material retained at a certain sieve size presents a continuous size distribution characterized by the parameter B. This means that the mean diameter ( Dn ) at a sieve size can be described as presented in[2], where Dmin is the opening of the sieve and Dmax is the opening of the previous sieve. Dn B Dmin Dmax [2] The maximum concentration of spheres of two different sizes is equivalent to a rhombohedral packing type ( Dmax&D 0, 74 ). n n1 The following model identifies three different groups within the mineral aggregates: the Primary Structure, the Secondary Structure and the oversized material as shown in Figure 2. The Primary Structure (PS) is a range of sizes in the gradation that due to its concentration provides the load bearing capacity for the mix. The PS acts as a central core where all the particles are connected with each other, and the more connections there are the stronger the core is. The Secondary Structure (SS) is formed by the particles with a smaller size than the PS. The SS fills in the voids between the PS particles and provides stability to the PS. Finally, there are oversized particles which size is bigger than the PS and which do not contribute to any load carrying. To determine the PS range the analysis must consider the tightest and loosest case in which two consecutive sizes can have stone-to-stone contact, which are represented in Figure 3. 100 90 80 60 50 40 30 20 Sieve size 0.45 [mm] Figure 2. Gradation Analysis Framework 4 19. 0 12. 5 9.5 4.7 5 2.3 6 1.1 8 0 0.6 0 10 0.0 75 0.1 5 0.3 0 % Passing 70 Figure 3. Tightest (a.) and loosest (b.) configurations of the Primary Structure For two consecutive sieve sizes with diameter Dn and Dn1 and concentrations n and n1 respectively, the average particle diameter ( Davg ) can be calculated as: Davg Dn n Dn 1 n 1 n n 1 [3] The tightest case is built upon the addition of smaller spheres to one-sized un-compacted bigger spheres. The bigger spheres will present a simple cubic configuration as shown on Figure 3 previous the addition of smaller spheres. When these are added the porosity decreases until a minimum representing a rhombohedral packing, assuring the contact between the smaller spheres and the surrounding bigger ones. Numerically this can be expressed as: Davg Dn 0,52 Dn1 0, 22 0, 703 Dn 0, 297 Dn 1 0, 74 [4] In the loosest case the bigger spheres have no contact with each other, allowing the smaller spheres to be positioned in between them. To assure contact between both sized spheres then the distance between the bigger spheres must not be bigger than the diameter of the smaller spheres. This can be calculated by using the separation distance between the surfaces of two neighbouring elements (Coussot, 2005) as described in[5]. 1 3 max h 2r 1 5 [5] The solution for two contiguous sieve sizes can be calculated considering h Dn1 , r Dn / 2 , max 0,74 and φ as the volume fraction of the spheres belonging to the sieve size “n”. This will give the following relation[6]: 1 Dn 0, 74 3 Dn 1 2 1 2 [6] 1 3 Dn 1 0, 74 1 Dn Taking into consideration different sieve systems it is possible to notice that the relationship Dn1 / Dn moves between γmax=0,77 and γmin=0,47 giving φ=0,13 and φ=0,23 respectively. Contact between particles will then be assured for a minimum concentration of the biggest sphere of 0,23. This can be expressed as: Davg Dn 0, 23 Dn 1 0,51 0,311 Dn 0, 689 Dn 1 0, 74 [7] Finally, interaction between two contiguous sieve sizes will occur if the average diameter for the particles is within the following limits, as given by equation[8]. A summary of the process to determine the Primary Structure is given in Figure 4. 0,311 Dn 0,689 Dn1 Davg 0,703 Dn 0, 297 Dn1 6 [8] From Gradation: - sieve sizes D1 and D2 - per cent retained at each sieve φ1 and φ2 Calculation of the Average Particle Size 𝐷1 𝜑1 + 𝐷2 𝜑2 𝐷𝑎𝑣𝑔 = 𝜑1 + 𝜑2 Calculation of the Interaction Range Limits 𝑚𝑖𝑛 = 0,311 ∗ 𝐷1 + 0,689 ∗ 𝐷2 𝑚𝑎𝑥 = 0,703 ∗ 𝐷1 + 0,297 ∗ 𝐷2 Check Interaction 𝑚𝑖𝑛 ≤ 𝐷𝑎𝑣𝑔 ≤ 𝑚𝑎𝑥 YES NO D1 and D2 have not enough interaction to belong to the Primary Structure D1 and D2 do interact and the might belong to the Primary Structure Continue the analysis with the next sieve sizes until Dlast Figure 4. Primary Structure Identification Porosity of the Primary Structure The relation between performance of asphalt mixtures and gradation characteristics is influenced by several aggregate properties, e.g. stone texture, shape and stiffness. In the following framework only the influence of the whole structure formed by the stones is considered, which is characterized by porosity of the assemblage and contact points due to their contribution to shear resistance. The calculation of the Primary Structure Porosity is based on the general definition of porosity as a measure of the void spaces in a material, given as a fraction of the volume of voids over the total volume (VT). The volume of voids for the Primary Structure is everything in the mixture that is not considered to be part of the PS, and the total volume of the mixture is all except the volume of particles bigger than the Primary Structure. In[9] VaSS is the volume of aggregate belonging to the Secondary 7 Structure, Vaoversized is the volume of aggregate bigger than the Primary Structure, Vbtot is the total volume of bitumen binder, VbabsPS is the volume of bitumen binder absorbed by the Primary Structure, and Vv is the total volume of voids. PS VV VaSS Vbtot Vv VbabsPS VT VT Vaoversized [9] Coordination number (m) is the average of contact points per particle and can be calculated using the relationship in[10], where η is the porosity, based on packing theory: m 2,827 1,069 [10] Disruption Factor The Disruption Factor (DF) is a parameter developed to evaluate the potential of the Secondary Structure to disrupt the Primary Structure (Guarin 2009; Guarin, et al. 2011 under revision). The DF is calculated as following: DF Vdp Volume of potentially disruptive particles Vdp PS Volume of PS voids Vv Wdp [11] Gsb The weight of potentially disruptive particles considers the material belonging to the SS bigger than the average void size of the PS, which depends on the packing arrangement (porosity) of the PS particles. Rutting performance is related to the mixtures capacity to resist shear. An adequate amount of Secondary Structure, specially the potentially disruptive particles, will benefit the mixture in the load carrying capacity. Bitumen Distribution Parameter (t) The developed framework proposes a solution to calculate the coating thickness of aggregates in a hierarchical order according to particle size and the packing configuration of the Primary Structure. In the following model particles with size below the last sieve size (fines) and the bitumen binder are considered to form a composite material called mastic. This mastic is distributed around the Secondary Structure with a certain thickness (tSS). If this film is too thin then the particles of the Secondary Structure will act as a granular material instead of a composite 8 one, leading to a brittle response under loading. The mixture of mastic and Secondary Structure will then flow around the Primary Structure, coating it with a certain thickness (tPS). The thickness of this second coating will depend on the packing configuration of the Primary Structure and the per cent of air voids in the mixture, as the coat will represent the distance between the air void and the aggregate-binder interface. The relationship between film thickness and porosity developed by (Cooke & Rowe, 1999) has been used to determine tSS and tPS. This relationship considers the different packing arrangements that a set of spherical particles can present, and the change in porosity when varying the film thickness taking into consideration the overlapping of the film as it grows. The particles belonging to the Secondary Structure are always considered to be packed in the densest possible way (φ=0,74), as their porosities are very low as calculated according to[12]. However, the porosities of the Primary Structure will vary from the tightest case to very loose; giving a dependency of the film thickness on the packing arrangement. SS Vv V f V tot V eff SS a f b tot v eff VT Va Va Vb Vv [12] Once calculated SS and (the porosity used to determine the PS coating thickness is the one of the whole mixture and not PS ), the graph presented in Figure 5 is used to estimate a dimensionless parameter 2 Lt / d p which represents the thickness of the film ( Lt ) related to the particles diameter ( d p ). The diameter of the particle will be the weighted average size of the sub-structure used. 0.5 Simple Cubic Orthorhombic Tetragonal Rhombohedral Porosity, 0.4 0.3 0.2 0.1 0 0 0.1 0.2 0.3 0.4 0.5 Dimensionless parameter, 2Lt/dp 0.6 0.7 Figure 5. Relation between porosity and film thickness as developed by (Cooke & Rowe, 1999) 9 In Figure 5 only the theoretical packing arrangements are defined, but as the coordination number for different mixtures is the average of contact points per volume, then interpolation has to be done between the theoretical curves. In the case of having a mixture with a coordination number less than 6 (simple cubic), then the distance between coated particles must be taken into account for the final coating thickness. For cases with m<6 the coating thickness (t) is calculated as following: tm6 tm 6 1 dp 0,4764 3 tm 6 1 2 1 PS [13] In [13] tm=6 is the film thickness calculated assuming a simple cubic packing and dp is the particles diameter. 3. Results To validate the framework several field mixtures with known rutting performance have been analysed, these mixtures are: WesTrack road test facility [35, 36, 37, 38, 39, 54, 55, 56] in Nevada (USA) placed and tested by the Federal Highway Administration (FHWA, 1998); NCAT’s test track [E2, E3, E4, E8, E9, N5, N6, N7, and N8] in Alabama (USA) placed and tested at National Centre for Asphalt Technology (Powell, 2001). Also, laboratory mixtures tested for rutting and moisture damage have been analysed. These mixtures are: Limestone [FL] and granite [GA] mixtures [ICf, ICgood, ICc, IC-48], specially designed to analyse the effect of material smaller than the load bearing range size on rutting performance. This mixtures were tested with the asphalt pavement analyser (APA) (Guarin, et al., 2011); Laboratory based oolitic limestone mixtures [C3, C4/F3, C5, F2, F4, F5, F6] of varying gradations design for studying shear instability for different compactive methods with APA (Birgisson, et al., 2004); Limestone and granite mixtures [C1, C2, C3, F1, F2, F3/C4], designed to study the relationship between moisture damage, air void distribution and material surface properties (Birgisson, et al., 2005). Performance of an asphalt mix can be evaluated by checking individual failure modes. Two of the most common failure cases are rutting and moisture damage. When the thickness of the mastic surrounding the Secondary Structure is too low, then the particles are not bonded 10 Rut Depth[mm] per million ESALs 20 WesTrack NCAT E NCAT N 15 10 5 0 40 50 60 70 % of PS over the total mix volume Rut Depth[mm] per million ESALs Rut Depth[mm] per million ESALs Rut Depth[mm] per million ESALs to each other producing a brittle response to loading. This reduces significantly the capacity of a mixture to resist permanent deformation. In the case of the Primary Structure, low coating thickness affects the durability of the mixture by increasing the possibility of rutting due to densification from the traffic. However, low thickness around the PS means interconnected air voids which help the drainage of moisture trapped in the mix. In the opposite case, when the coating thickness around the PS is too thick there is a risk of losing the contact points between the PS particles, affecting the general load bearing capacity of the mixture. 20 WesTrack NCAT E NCAT N 15 10 5 0 0 0.2 0.4 tSS [mm] 0.6 0.8 20 WesTrack NCAT E NCAT N 15 10 5 0 0 1 2 3 Disruption Factor 4 5 20 WesTrack NCAT E NCAT N 15 10 5 0 0.5 1 1.5 2 tPS [mm] Figure 6. Results for Field Mixtures Figure 6 presents the results for WesTrack and NCAT mixtures. It is possible to observe how the framework is capable to identify those mixtures with rutting problems isolating them to the extremes. High content of material acting as the load bearer structure produces mixtures that suffer high permanent deformation. This is due to lack of supporting material providing stability under loading. The Disruption Factor shows this effect as mixtures with poor rutting performance have a higher potential to have their PS disrupted. Furthermore, these “bad” mixtures also present low film thickness around both structures. Low thickness 11 around the SS shows a lack of bond between the supporting material, and low thickness around the PS shows lack of supporting material in general. 10 8 8 6 4 Granite (G) Limestone (G) Limestone (B) 2 0 20 APA Rut [mm] APA Rut [mm] 10 6 4 0 30 40 50 60 % of PS over the total mix volume 10 10 8 8 6 4 Granite (G) Limestone (G) Limestone (B) 2 0 0.08 0.1 0.12 Granite (G) Limestone (G) Limestone (B) 2 APA Rut [mm] APA Rut [mm] Figure 7 shows the results for laboratory mixtures tested with the Asphalt Pavement Analyser (APA). As it can be observed in the left upper plot there is no clear tendency for the material from (Guarin, et al., 2011), however the limestone mixtures from (Birgisson, et al., 2004) show that there is a minimum rutting depth for mixtures with a PS content around 45 – 50% and it increases towards the extremes. Once again, it can be observed in the Disruption Factor results that the rutting depth increases for DF>1. 0 0.5 1 Disruption Factor 6 4 Granite (G) Limestone (G) Limestone (B) 2 0 0.5 0.14 tSS [mm] 1.5 1 1.5 2 tPS [mm] Figure 7. Results for Laboratory mixtures with APA test In (Birgisson, et al., 2005) two groups of aggregates were used: oolitic limestone that in the past has not shown significant stripping potential and crushed Georgia granite that has shown potential to stripping. All mixtures were made up of four components: coarse aggregate, fine aggregate, screenings and mineral filler. They were blended together in different proportions providing six HMA mixtures for each mineral aggregate type which were volumetrically equivalent to each other. The mixtures were designed according to the SuperPave volumetric mix design method and all specimens were compacted on the IPC Servopac SuperPave gyratoric compactor to 7-8% air voids. 12 Average Void Diameter [mm] Average Void Diameter [mm] Using digital images from X-ray Computed Tomographic imaging the air void size distribution and number of air voids was determined for each specimen. In Figure 8 the relation between air void size and thickness of film around the Primary and Secondary Structures is presented. It can be observed that the higher tSS then the particles are better “glued” together making the air voids bigger but fewer. The opposite trend is observed with tPS as the space in between the particles will clearly decrease with thicker film around them. Limestone Granite 1.6 1.4 1.2 1 0.8 0.09 0.1 0.11 0.12 0.13 0.14 0.15 Limestone Granite 1.6 1.4 1.2 1 0.8 0.4 0.6 tSS [mm] 0.8 1 1.2 tPS [mm] Figure 8. Correlation between air void size and binder distribution The granite mixtures were tested with the Hamburg Wheel Tracking Device to determine their natural resistance too moisture damage. The test specifications determine that the test is continued until either rut of 12,5 mm depth is measured or the number of loading cycles reaches 20000. The number of cycles to strip, Ns, is defined as the loading cycle where the rate of permanent displacement measured during the test markedly increases. 2.2 x 10 4 2.2 4 2 N of cycles to strip N of cycles to strip 2 x 10 1.8 1.6 1.4 1.2 1 1.8 1.6 1.4 1.2 1 0.8 0.08 0.1 0.12 tSS [mm] 0.14 0.16 0.8 0.4 0.6 0.8 1 tPS [mm] Figure 9. Hamburg wheel Device test results for granite mixtures 13 1.2 1.4 The results given in Figure 9 show the number of cycles to strip related to the thickness around Primary and Secondary Structure. It can be observed that for a low value of tSS mixtures strip very fast as the stones have no protection against moisture, and for a ticker coating around the SS the air pockets are smaller but more numerous. In this case the thickness of the PS is also high and the more air voids there are the bigger the surface are exposed to water. It is possible to observe that there is an optimum tSS for which the resistance to stripping is highest. At this level the stones in the SS are protected against moisture and at the same time they leave enough open channels for the water to drain as tPS is low. 1.2 1.2 Limestone Granite 0.8 1 ERc/ERu ERc/ERu 1 0.6 0.4 0.2 0.08 Limestone Granite 0.8 0.6 0.4 0.1 0.12 tSS [mm] 0.14 0.2 0.4 0.16 0.6 0.8 1 tPS [mm] 1.2 1.4 Figure 10. Moisture analysis for limestone and granite mixtures Figure 10 presents the energy ratio results of limestone and granite mixtures. Energy ratio is a parameter that measures the fracture resistance of mixtures based on the dissipated creep strain energy, forming a basis for a performance-based fracture criterion for flexible pavements (Birgisson, et al., 2005). Since it is known that the fracture resistance of a mixture is strongly affected by moisture damage, by evaluating the energy ratio of the conditioned and the unconditioned samples a measure of the moisture damage is given. According to the given definition, moisture damage decreases with higher ERc/ERu. The influence of the film thickness around the PS is very well captured by the limestones, as lower films means bigger air voids providing a proper drainage for the water trapped in the structure as well as there is less mixtures exposed to the moisture. It can be noticed in this type of testing that granite mixtures do not present such a clear response as in the Hamburg Wheel Tracking Device. This is due to the conditioning of the samples, as for energy ratio testing the samples are forced into saturation creating conditions which are unreal to certain types of minerals, like granites, provoking a general failure of the samples. 14 4. Discussion and Conclusions The following thesis presents a framework developed to characterize asphalt mixtures based on the aggregates gradation and the structure formed by them. The framework identifies the range of material which forms the Primary Structure and is the main load bearing assembly. The amount of material belonging to the Primary Structure may influence the load response of a mixture and can be characterized by its porosity and coordination number according to packing theory of spheres. Particles that are smaller than the Primary Structure are called the Secondary Structure and they provide stability to the main network by keeping it in place, while particles that are bigger than the Primary Structure are just considered to be floating in the mixture as their concentration is not enough to influence the load carrying ability of the mixture. A complete characterization of asphalt’s microstructure is achieved by determining the way that the bitumen binder is distributed and how this affects the size and distribution of the air voids. For this purpose a hierarchical distribution system has been developed which assumes the following sequence: bitumen binder and fines creates mastic which covers the particles of the Secondary Structure; this composite is then the material that coats the Primary Structure. Both thicknesses have been calculated using a previous relationship based on packing of the particles and the overlapping of the film as it grows. This method has given a geometrical solution to binder distribution for each sub-structure, which increases the understanding of asphalt mixture microstructure. The framework has been validated by taking mixtures with known field rutting performance and laboratory mixtures that have been tested for both rutting and moisture damage. The range for Primary and Secondary Structure as well as porosity of the Primary Structure, coordination number and the binder distribution parameter for each structure have been calculated for each one of the mixtures. Results obtained show a favourable relation between the per cent of material that the Primary Structure represents of the whole mixture and the resistance to rutting, suggesting that there might be an optimum of material that would give a minimum permanent deformation. Film thickness of the Primary Structure has shown to be a key parameter to prevent moisture damage, as it is directly related to the size of the air voids and the protection of the aggregate/mastic interface. The developed framework is a tool to engineer mixtures and optimize the use of available materials. The advantages of the model is its flexibility for any type of sieve system used and its ability to include different size distribution within a sieve size, reducing the limitations from previously developed models. The assumption of having aggregates as spherical particles has shown, even though a very rough approximation, to give a good corelation to performance on asphalt mixtures. It is still desirable to include the influence of aggregates shape and texture, and the differences on mixture response depending on the mineral composition of the aggregates. Packing theory has proven that independent of the 15 shape of the particles the concept of contact points and porosity can be used to describe the structure formed by the aggregates. The biggest potential of the developed framework can be seen from the simulation side, as it works as a tool to reduce the number of variables in asphalt microstructure. The Gradation - Based Framework has satisfactory distinguished between good and bad performance of asphalt mixtures when related to permanent deformation and moisture damage. Further work is needed to calibrate the model based on x-ray tomography or similar tools, to determine the range of validity of the formulations and to identify the critical ranges for Primary Structure content and coating thickness for optimal performance and more durable asphalt pavements. The developed model can be used as a tool to determine the optimal gradation to assure good performance for hot mix asphalt pavements. 16 5. 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