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Engineering Reactive Clay Systems by Ground Rubber Replacement and Polyacrylamide Treatment

This study investigates the combined performance of ground rubber (GR), the additive, and polyacrylamide (PAM), the binder, as a sustainable solution towards ameliorating the inferior geotechnical attributes of an expansive clay. The first phase of the experimental program examined the effects of PAM concentration on the soil’s mechanical properties—consistency, sediment volume attributes, compactability, unconfined compressive strength (UCS), reactivity and microstructure features. The second phase investigated the effects of GR content, with and without the optimum PAM concentration. An increase in PAM beyond 0.2 g/L, the identified optimum concentration, caused the excess PAM to act as a lubricant rather than a flocculant. This feature facilitated reduced overall resistance to sliding of soil particles relative to each other, thereby adversely influencing the improvement in stress–strain–strength response achieved for ≤0.2 g/L PAM. This transitional mechanism was further verified by the consistency limits and sediment volume properties, both of which exhibited only minor variations beyond 0.2 g/L PAM. The greater the GR content, the higher the mobilized UCS up to 10% GR, beyond which the dominant GR-to-GR interaction (i.e., rubber-clustering) adversely influenced the stress–strain–strength response. Reduction in the soil’s swell–shrink capacity, however, was consistently in favor of higher GR contents. Addition of PAM to the GR-blended samples amended the soil aggregate–GR connection interface, thereby achieving further improvements in the soil’s UCS and volume change behaviors. A maximum GR content of 20%, paired with 0.2 g/L PAM, managed to satisfy a major decrease in the swell–shrink capacity while improving the strength-related features, and thus was deemed as the optimum choice.


Introduction
Clay soils are often characterized as problematic construction materials, as their intrinsic mechanical attributes present significant challenges for geotechnical engineering systems. Meanwhile, shortage of land for development, as well as increasing costs associated with construction and raw materials, necessitate maximum utilization of locally-available materials, one being problematic clay soils. In this context, expansive clays are consistently viewed among the most significant, widespread, costly and least publicized geological hazards, and thus demand further attention [1]. A notable fraction of expansive clays consists of active smectite minerals, which exhibit significant swell-shrink volume changes, as well as desiccation-induced cracking, upon the addition or removal of moisture [2,3]. These  1 I F = ∆w/∆log 10 δ (where w = moisture content, and δ = cone penetration depth); and 2 Ratio of equilibrium sediment volume of 10 g oven-dried soil, passing 425 µm sieve, in distilled water to that of kerosene.
The conventional grain-size analysis indicated a clay fraction (< 2 µm) of 44%, along with 36% silt (2-75 µm) and 20% sand (0.075-4.75 mm). The liquid limit (as determined for 20-mm cone penetration depth using the 80 g-30 • fall-cone device) and standard thread-rolling plastic limit were measured as w L = 78.04% and w P = 22.41%, respectively; giving a plasticity index of I P = 55.6%, such that the soil was classified as clay with high plasticity (CH) in accordance with the Unified Soil Classification System (USCS). The free swell ratio (FSR)-a quantitative measure of clay mineralogy and hence the soil's expansive potential [50]-was obtained as FSR = 2.27, thereby indicating that the soil's clay fraction was mainly dominated by active smectite minerals, such as montmorillonite. In terms of expansivity, the FSR corresponded to an undesirable, high expansive potential (see Table A1 of the Appendix A Polymers 2019, 11, 1675 4 of 23 section for relevant classification criteria). The standard Proctor compaction test resulted in a relatively high optimum moisture content of w opt = 20.24%, along with a maximum dry density of ρ dmax = 1.62 Mg/m 3 ; the latter produces a minimum void ratio of e min = 0.702.

Ground Rubber
Commercially-available tire-derived ground rubber (GR) was used as the additive to partially replace the low-grade host soil. The physical properties and chemical composition of GR, as supplied by the manufacturer or independently measured as per relevant ASTM standards, are summarized in Table 2. In terms of gradation, the rubber particles were found to be similar in size to fine-medium sand (0.075-2 mm). The GR particle diameters corresponding to 10%, 30% and 60% finer-d 10 , d 30 and d 60 -were obtained as 0.182 mm, 0.334 mm and 0.513 mm, respectively. The coefficients of uniformity and curvature were hence calculated as C u = d 60 /d 10 = 2.81 and C c = d 30 2 /d 60 d 10 = 1.20, from which the gradation of the GR material can be classified as equivalent to poorly-graded sand (SP) according to the USCS criterion. Other physical properties included a specific surface area of SSA = 0.05 m 2 /g and a specific gravity of G s GR = 1.09; the latter is approximately 2.5-fold lower than that of the clay soil (G s S = 2.76). The chemical composition of GR was mainly dominated by styrene-butadiene copolymer and carbon black, with mass fractions of 55% and 25-35%, respectively. Optical and scanning electron microscopy (SEM) techniques were employed to observe the morphological features of the GR particles, and the results are illustrated in Figure 1. The GR particles were found to be non-spherical and highly-irregular in shape (see Figure 1b); their surfaces encompassed a series of peaks and troughs of varying heights, depths and spacing, as well as occasional cavities and micro-cracks, thus signifying a dominant rough surface texture (see Figure 1c). Such morphological features may potentially promote adhesion and/or generate frictional resistance at the soil aggregate-GR interface, and thus alter the soil fabric into a unitary mass of enhanced shear resistance [4,26,27].

Polyacrylamide
A commercially-available polymer agent, chemically referred to as polyacrylamide (PAM), was used as the binder. It was supplied in granular form and was diluted with water for application (see Figure A1 of the Appendix A section). PAMs are a group of hydrophilic, miscible synthetic polymers formed by the polymerization of acrylamide (AMD) and related monomers (CH2=CHC(O)NH2); they can be synthesized in non-ionic, cationic or anionic forms [51]. The anionic variant, as used in the present study, can be developed through two common pathways: (i) hydrolysis of non-ionic PAM with a strong base such as sodium hydroxide (NaOH), as demonstrated in Figure 2a; and (ii) copolymerization of AMD and acrylic acid or a salt of acrylic acid (e.g., sodium acrylate), as illustrated in Figure 2b [52]. Anionic PAMs are mainly employed to encourage flocculation of aqueous suspensions [51,53,54]. Other common applications, as reported in the literature, include their widespread use in the mining industry for thickening and dewatering of concentrates and tailings, as well as their successful adoption in routine construction practices, such as soil compaction, and for erosion control [52,55,56]. The physical and chemical properties of the used PAM, as supplied by the manufacturer, included a pH of 6.9 (at 25 °C), a moderate density charge of approximately 18%, and a relatively high molecular weight of 12-15 Mg/mol (equivalent to approximately 150,000 monomer units per molecule).

Polyacrylamide
A commercially-available polymer agent, chemically referred to as polyacrylamide (PAM), was used as the binder. It was supplied in granular form and was diluted with water for application (see Figure A1 of the Appendix A section). PAMs are a group of hydrophilic, miscible synthetic polymers formed by the polymerization of acrylamide (AMD) and related monomers (CH 2 =CHC(O)NH 2 ); they can be synthesized in non-ionic, cationic or anionic forms [51]. The anionic variant, as used in the present study, can be developed through two common pathways: (i) hydrolysis of non-ionic PAM with a strong base such as sodium hydroxide (NaOH), as demonstrated in Figure 2a; and (ii) copolymerization of AMD and acrylic acid or a salt of acrylic acid (e.g., sodium acrylate), as illustrated in Figure 2b [52].

Polyacrylamide
A commercially-available polymer agent, chemically referred to as polyacrylamide (PAM), was used as the binder. It was supplied in granular form and was diluted with water for application (see Figure A1 of the Appendix A section). PAMs are a group of hydrophilic, miscible synthetic polymers formed by the polymerization of acrylamide (AMD) and related monomers (CH2=CHC(O)NH2); they can be synthesized in non-ionic, cationic or anionic forms [51]. The anionic variant, as used in the present study, can be developed through two common pathways: (i) hydrolysis of non-ionic PAM with a strong base such as sodium hydroxide (NaOH), as demonstrated in Figure 2a; and (ii) copolymerization of AMD and acrylic acid or a salt of acrylic acid (e.g., sodium acrylate), as illustrated in Figure 2b [52]. Anionic PAMs are mainly employed to encourage flocculation of aqueous suspensions [51,53,54]. Other common applications, as reported in the literature, include their widespread use in the mining industry for thickening and dewatering of concentrates and tailings, as well as their successful adoption in routine construction practices, such as soil compaction, and for erosion control [52,55,56]. The physical and chemical properties of the used PAM, as supplied by the manufacturer, included a pH of 6.9 (at 25 °C), a moderate density charge of approximately 18%, and a relatively high molecular weight of 12-15 Mg/mol (equivalent to approximately 150,000 monomer units per molecule). Anionic PAMs are mainly employed to encourage flocculation of aqueous suspensions [51,53,54]. Other common applications, as reported in the literature, include their widespread use in the mining industry for thickening and dewatering of concentrates and tailings, as well as their successful adoption in routine construction practices, such as soil compaction, and for erosion control [52,55,56]. The physical and chemical properties of the used PAM, as supplied by the manufacturer, included a pH of 6.9 (at 25 • C), a moderate density charge of approximately 18%, and a relatively high molecular weight of 12-15 Mg/mol (equivalent to approximately 150,000 monomer units per molecule).

Mix Designs and Sample Preparations
In this study, a total of thirteen mix designs, consisting of one control (hereafter the natural soil), four PAM-treated, four GR-blended and four PAM + GR cases, were examined (see Table 3). For ease of presentation, the following coding system was adopted to designate the various mix designs: where S = the natural soil; P x = x g/L PAM; and R y = y% GR. As outlined in Table 3, the experimental program was carried out in two phases. The first phase, the results of which are presented in Section 4.1, examined the effects of PAM-treatment, at varying PAM concentrations, on the soil's mechanical properties, namely consistency, sediment volume attributes, compactability, UCS and microstructure features; the results of this section were analyzed to identify the optimum PAM concentration. The second phase, the results of which are presented in Section 4.2, investigated the effects of GR inclusion, with and without the optimum PAM concentration (later to be found as P c = 0.2 g/L), through a series of standard Proctor compaction, UCS and soil reactivity tests. The PAM, GR and moisture contents with respect to the various mix designs were, respectively, defined as: Furthermore, the specific gravity of solids for those mix designs containing GR-SP x R y where x = {0, 0.2}, and y = {5, 10, 20, 30}-was calculated by the following theoretical relationship [34,57]: where G s M = specific gravity of GR-blended mixtures (either with or without PAM); G s S = specific gravity of soil solids (= 2.76); and G s GR = specific gravity of GR particles (= 1.09).
The natural soil and GR were blended in dry form, as per the selected mix designs outlined in Table 3. The required volume of moisture, either water or PAM solution, corresponding to the mixtures' standard Proctor optimum moisture content (values presented in Table 6 and Figure 6), was added to each blend and thoroughly mixed using a hand trowel. For those mix designs containing PAM, great care was taken to pulverize any clumped particles, thus targeting homogeneity of the mixtures. A special stainless-steel split mold, as previously described by the authors, was used for sample preparations by means of the static compaction technique [4,38]. The mold consisted of three segments-the top collar, the middle section, and the bottom collar. The middle section, measuring 50 mm in diameter and 100 mm in height, accommodates the samples prepared for the UCS tests (see Section 3.2), as well as the core shrinkage tests (a component of the soil reactivity test, as outlined in Section 3.3). The samples were formed by static compaction in the mold in five equal-height layers, each layer having achieved its respective standard Proctor maximum dry density (values presented in Table 6 and Figure 6). Samples for the oedometer swell tests, a second component of the soil reactivity test (see Section 3.3), were prepared in a similar fashion; in this case, however, a different mold with a middle section measuring 50 mm in diameter and 20 mm in height, along with three compaction layers, were adopted. The samples with PAM as the sole stabilizing agent were enclosed in multiple layers of cling wrap and maintained at ambient laboratory temperature conditions for T c = 1, 4, 7 and 14 d to examine the effect of curing duration on the UCS. For those mix designs containing the optimum PAM and GR, the same curing procedure was carried out for only 7 d (later to be found as the optimum curing period). The methodologies associated with the UCS, soil reactivity and SEM tests are presented in the following sections. Table 3. Soil-PAM-GR mix designs and their properties.

Group
Sample

UCS Test
UCS tests were carried out in accordance with ASTM D2166-16 (American Society for Testing and Materials, PA, USA). The prepared samples were axially compressed at a constant displacement rate of 1 mm/min, as commonly adopted in the literature [26,37,38]. The axial strains and corresponding axial stresses were recorded at predefined time intervals to a point at which the maximum axial stress required for sample failure, the UCS, was achieved. On account of the curing periods adopted for the samples containing PAM, a total of 25 UCS tests-one for control (natural soil), sixteen for PAM-treated, four for GR-blended and four for PAM + GR blends-were carried out to address the thirteen mix designs outlined in Table 3.

Soil Reactivity Test
Soil reactivity tests were carried out in accordance with AS 1289.7.1.1-03 (Standards Australia, NSW, Australia). The test incorporates results obtained from the core shrinkage and the oedometer swell tests, performed on two companion samples, into a unique parameter referred to as the shrink-swell index: where I ss = shrink-swell index (%pF −1 ); [pF] = 1 + log[kPa]; ε sh = shrinkage potential (%); ε sw = swelling potential (%); ∆ψ = range of total suction change (pF); ψ sh = total suction upon completion of the core shrinkage test (pF); and ψ sw = total suction upon completion of the oedometer swell test (pF). The methodologies associated with the two test components-the core shrinkage and the oedometer swell tests-are presented in the following.

•
Core shrinkage test: The prepared 50-mm diameter by 100-mm long samples were allowed to desiccate at ambient laboratory temperature conditions. For each sample, the incurred axial shrinkage strain was regularly monitored (by a dial displacement transducer) to a point at which shrinkage ceased. The desiccated samples were then oven-dried at 105 • C for 24 hr. Final height measurements were taken by a Vernier caliper, from which the ultimate shrinkage strain, denoted as ε sh and referred to as the shrinkage potential, was determined.

•
Oedometer swell test: The prepared 50-mm diameter by 20-mm high samples were inundated with water and allowed to swell in a conventional oedometer setup under a nominal vertical stress of 25 kPa. For each sample, the incurred axial swelling strain was monitored during predefined time intervals to a point at which the ultimate swelling strain, denoted as ε sw and referred to as the swelling potential, was achieved.
The shrink-swell index represents percentage axial strain, either shrinkage or swelling, per change in unit suction of the soil, and thus can be employed to estimate free ground surface movements under field conditions [58]. Other applications, as commonly adopted in Australian geotechnical practice, include its use for site classification, as well as its importance to perceive and hence specify the soil degree of expansivity. Classification procedures for expansive soils based on the shrink-swell index, as proposed by Seddon [59], are summarized in Table A2 of the Appendix A section. The denominator in Equation (6), ∆ψ = ψ sh − ψ sw , represents the range of total suction change with respect to the sample's volume increase from air-dry to near saturation conditions; it is commonly taken as ∆ψ = 1.8 pF, suggested based on collective experience of the Australian AS 2870 code committee [58]. Although this standard value is widely accepted for natural fine-grained soils, the same may not necessarily hold true for stabilized expansive soils. As such, to examine the validity of the 1.8 pF value for the stabilized expansive soil under investigation in the present study, independent suction measurements were taken upon completion of the core shrinkage and oedometer swell tests by means of the WP4C (METER Group, WA, USA) dew point potentiometer apparatus device [60]. As such, two sets of I ss values were measured for each sample: (i) conventional shrink-swell index I ssc , obtained by ∆ψ = 1.8 pF; and (ii) modified shrink-swell index I ssm , obtained by actual ∆ψ measurements. In this regard, as outlined in Table 3, a total of eight mix designs-one for control (natural soil or SP 0 R 0 ), one for PAM-treated (SP 0.2 R 0 ), four for GR-blended (SP 0 R y where y = {5, 10, 20, 30}) and four for PAM + GR blends (SP 0.2 R y where y = {5, 10, 20, 30})-were examined.

SEM Analysis
The SEM technique was used to observe the evolution of soil fabric in response to PAM-treatment; relevant microstructure analyses were carried out using an SEM characterization scheme developed by Soltani et al. [4]. The Philips XL20 (Amsterdam, The Netherlands) scanning electron microscope was used for SEM imaging; apparatus specifications included a resolution of 4 µm, along with a maximum magnification ratio of 50,000×. In this regard, typical mix designs consisting of SP 0 R 0 (natural soil) and SP 0.2 R 0 were examined. The desired samples, prepared as per Section 3.1, were first air-dried for approximately 14 d. The desiccated samples were then carefully fractured into cubic-shaped pieces, approximately 1 cm 3 in volume, and were further scanned at various magnification ratios ranging from 250× to 20,000×.

Effect of PAM on Soil Consistency
Typical flow curves for the natural soil (SP 0 R 0 ) and the sample treated with 0.6 g/L PAM (SP 0.6 R 0 ) are provided in Figure 3. As a result of PAM-treatment, the flow curve exhibited a notable, counterclockwise rotation, thereby leading to a major increase in values of both the flow index I F = ∆w/∆log 10 δ (where w = moisture content, and δ = cone penetration depth) and the liquid limit w L . Table 4 presents the complete results of the consistency limits tests for the natural soil and various 6}. The greater the PAM concentration, the higher the consistency limits up to P c = 0.2 g/L, beyond which the effect of PAM-treatment was found to be marginal. The rate of increase in the liquid limit, however, was more pronounced compared with that of the plastic limit w P and the plasticity index I P . The natural soil resulted in w L = 78.04% (I P = 55.63%), while the samples treated with P c = 0.1 g/L, 0.2 g/L, 0.4 g/L and 0.6 g/L produced higher values of w L = 82.82%, 87.61%, 87.22% and 85.80% (I P = 59.09%, 62.76%, 61.36% and 60.93%), respectively. Consequently, PAM-treatment did not alter the soil's USCS classification, as the original CH "clay with high plasticity" category remained unchanged for all treated blends.   The consistency limits, the liquid limit and flow index in particular, can be employed to infer the development of soil fabric [40,61]. An increase in the liquid limit, as is the case with PAM-treated blends (see Table 4), implies that an edge-to-face flocculated fabric dominates the matrix [62]. Compared to a face-to-face dispersed fabric, a flocculated fabric offers higher cone penetration/shear resistance, which in turn promotes higher liquid limits-that is, the standard 20-mm cone penetration depth is achieved for higher moisture contents.  Table 5. The greater the PAM concentration, the lower the equilibrium sediment volume (and hence the lower the FSR) up to P c = 0.2 g/L, beyond which the rate of decrease was marginal. The soil-water suspension (SP 0 R 0 ) had an equilibrium sediment volume of V D = 34.0 cm 3 (FSR = 2.27), whereas the soil-PAM suspensions with P c = 0.1 g/L, 0.2 g/L, 0.4 g/L and 0.6 g/L produced lower values of V P = 28.5 cm 3 , 25.0 cm 3 , 24.5 cm 3 and 23.0 cm 3 (FSR = 1.90, 1.67, 1.63 and 1.53), respectively. As outlined in Table A1, the FSR can be used to perceive the soil degree of expansivity [50]. The natural soil (SP 0 R 0 ) manifested an undesirable, high degree of expansivity, while the four PAM-treated cases all exhibited an improved, moderate expansive potential.
Much like the consistency limits (see Section 4.1.1), the FSR serves as an indicator of fabric evolution in response to pore-fluid variations, or in this case PAM-treatment [4,40]. A decrease in the FSR for the PAM-treated blends (see Table 5) signifies an increased tendency for particle flocculation, which in turn justifies the observed reduction in the equilibrium sediment volume [40]. In this regard, the maximum tendency for particle flocculation seems to be achieved at P c = 0.2 g/L, as greater PAM concentrations did not promote notable further reductions in V P and hence the FSR. These trends are also in agreement with those observed for the liquid limit and the flow index, both of which exhibited only minor variations beyond 0.2 g/L PAM.

Effect of PAM on Soil Compactability
Typical standard Proctor compaction curves, along with representative saturation lines (based on measured G s S = 2.76), for the natural soil (SP 0 R 0 ) and the sample treated with 0.6 g/L PAM (SP 0.6 R 0 ) are provided in Figure 4. As a result of PAM-treatment, the compaction locus underwent a considerable upward translation in the ρ d :w space (where ρ d = dry density, and w = moisture content), thereby signifying a notable increase in the maximum dry density ρ dmax (follow the "Compaction Path" in Figure 4). However, the variation in corresponding optimum moisture content w opt values were found to be marginal. Table 6   Much like the consistency limits (see Section 4.1.1), the FSR serves as an indicator of fabric evolution in response to pore-fluid variations, or in this case PAM-treatment [4,40]. A decrease in the FSR for the PAM-treated blends (see Table 5) signifies an increased tendency for particle flocculation, which in turn justifies the observed reduction in the equilibrium sediment volume [40]. In this regard, the maximum tendency for particle flocculation seems to be achieved at Pc = 0.2 g/l, as greater PAM concentrations did not promote notable further reductions in VP and hence the FSR. These trends are also in agreement with those observed for the liquid limit and the flow index, both of which exhibited only minor variations beyond 0.2 g/l PAM.

Effect of PAM on Soil Compactability
Typical standard Proctor compaction curves, along with representative saturation lines (based on measured Gs S = 2.76), for the natural soil (SP0R0) and the sample treated with 0.6 g/l PAM (SP0.6R0) are provided in Figure 4. As a result of PAM-treatment, the compaction locus underwent a considerable upward translation in the ρd:w space (where ρd = dry density, and w = moisture content), thereby signifying a notable increase in the maximum dry density ρdmax (follow the "Compaction Path" in Figure 4). However, the variation in corresponding optimum moisture content wopt values were found to be marginal. Table 6    Moisture content, w (%)   The increase in maximum dry density with increasing PAM concentration can be attributed to the higher viscosity of PAM solutions compared with that of water. That is, the increase in pore-fluid viscosity for the PAM-treated blends induces contact lubrication in the soil matrix; during compaction, this feature facilitates the movement and sliding of soil particles with much less effort/friction, thereby giving rise to higher maximum dry densities [44,48,61] Figure 5a. The constitutive response for the natural soil sample (SP 0 R 0 ) demonstrated a rise-fall behavior with a visually-detectable peak point. As a result of increasing PAM concentration, the stress-strain trace progressively transitioned towards a more ductile behavior. In terms of UCS, the greater the PAM concentration, the higher the mobilized UCS up to P c = 0.2 g/L, beyond which PAM-treatment was found to adversely influence strength development (follow the "Strength Path" in Figure 5a). At T c = 1 d, the natural soil produced a UCS of q u = 72.28 kPa, while the addition of 0.1 g/L and 0.2 g/L PAM, at T c = 1 d, led to mobilized higher values of 96.87 kPa and 128.43 kPa-equivalent to improvements of η = 34% and 78%-respectively. For the same curing period, the higher PAM concentrations of 0.4 g/L and 0.6 g/L resulted in q u = 83.18 kPa and 54.14 kPa, respectively; the former, SP 0.4 R 0 , holding a 15% advantage over the natural soil, whereas the latter, SP 0.6 R 0 , exhibits a significant 25% reduction with respect to the natural soil.  The increase in maximum dry density with increasing PAM concentration can be attributed to the higher viscosity of PAM solutions compared with that of water. That is, the increase in pore-fluid viscosity for the PAM-treated blends induces contact lubrication in the soil matrix; during compaction, this feature facilitates the movement and sliding of soil particles with much less effort/friction, thereby giving rise to higher maximum dry densities [44,48,61] Figure 5a. The constitutive response for the natural soil sample (SP0R0) demonstrated a rise-fall behavior with a visually-detectable peak point. As a result of increasing PAM concentration, the stress-strain trace progressively transitioned towards a more ductile behavior. In terms of UCS, the greater the PAM concentration, the higher the mobilized UCS up to Pc = 0.2 g/l, beyond which PAM-treatment was found to adversely influence strength development (follow the "Strength Path" in Figure 5a). At Tc = 1 d, the natural soil produced a UCS of qu = 72.28 kPa, while the addition of 0.1 g/l and 0.2 g/l PAM, at Tc = 1 d, led to mobilized higher values of 96.87 kPa and 128.43 kPa-equivalent to improvements of η = 34% and 78%respectively. For the same curing period, the higher PAM concentrations of 0.4 g/l and 0.6 g/l resulted in qu = 83.18 kPa and 54.14 kPa, respectively; the former, SP0.4R0, holding a 15% advantage over the natural soil, whereas the latter, SP0.6R0, exhibits a significant 25% reduction with respect to the natural soil.   Stress-strain curves for the natural soil (SP 0 R 0 ) and various samples treated with 0.2 g/L PAM (SP 0.2 R 0 ) cured for T c = 1, 4, 7 and 14 d are provided in Figure 5b. For any given PAM concentration, an increase in curing period was found to produce a major increase in the UCS up to T c = 7 d, beyond which the effect of curing was found to be marginal (follow the "Strength Path" in Figure 5b), with the axial strain at failure (failure mode) remaining remarkably unchanged. As a typical case, the sample SP 0.2 R 0 resulted in q u = 128.43 kPa, 141.23 kPa, 164.47 kPa and 168.34 kPa-equivalent to improvements of η = 78%, 95%, 128% and 133% with respect to the natural soil (SP 0 R 0 )-at T c = 1, 4, 7 and 14 d, respectively.
The complete results of the UCS tests, along with other stress-strain features, namely the deformability index I D , the elastic stiffness modulus E 50 , the peak strain energy E U and the resilient modulus E R , are summarized in Table 7. At any given curing time, the deformability index-a measure of the sample's ductility, as defined in the footer of Table 7 [63]-exhibited a monotonically-increasing trend with respect to PAM concentration, meaning that the greater the PAM concentration, the more ductile the sample's response to unconfined compression. By definition, I D has a value of unity for the natural soil (SP 0 R 0 ). As typical cases, the samples SP 0.1 R 0 , SP 0.2 R 0 , SP 0.4 R 0 and SP 0.6 R 0 cured for T c = 1 d resulted in I D = 1.10, 1.19, 1.62 and 1.90, respectively. For any given PAM concentration, the effect of curing period was found to be marginal; for instance, the sample SP 0.2 R 0 resulted in I D = 1.19, 1.24, 1.19 and 1.16 at T c = 1, 4, 7 and 14 d, respectively. The elastic stiffness modulus, peak strain energy and resilient modulus, as defined in the footer of Table 7 [64][65][66], all demonstrated a trend similar to that observed for the UCS. As such, at any given curing period, the greater the PAM concentration, the higher the E 50 , E U and E R values up to P c = 0.2 g/L, beyond which PAM-treatment adversely influenced the sample's stiffness, toughness and resilience. In terms of stiffness, for instance, the natural soil resulted in E 50 = 1.97 MPa, while the addition of 0.1 g/L, 0.   1 Percent change in the UCS (or q u ); 2 Axial strain at failure; 3 I D = ε u S /ε u N where ε u S = axial strain at failure for the stabilized sample, and ε u N = axial strain at failure for the natural soil [63]; 4 E 50 = secant modulus at 50% of the UCS (or q u ) [66]; 5 E U = area under the stress-strain curve up to the failure point [65]; and 6 Computed from E R (psi) = 124 × q u (psi) + 9980, as suggested by Thompson [64].

Effect of PAM + GR on Soil Compactability
Standard Proctor compaction curves, along with corresponding zero-air void (ZAV) saturation lines, for the natural soil and various GR-blended samples untreated-SP 0 R y where y = {0, 5, 10, 20, 30}-and treated with 0.2 g/L PAM-SP 0.2 R y where y = {0, 5, 10, 20, 30}-are provided in Figure 6a,b, respectively. As a result of GR inclusion, the compaction locus underwent a linear downward-leftward translation over the ρ d :w space, thus indicating a notable decrease in both the maximum dry density and the optimum moisture content associated with increasing GR content (follow the "Compaction Path" in Figure 6). The greater the GR content, the lower the compaction characteristics, with PAM-treated cases holding a slight advantage over their untreated counterparts. The natural soil (SP 0 R 0 ) and the untreated GR-blended samples with R c = 5%, 10%, 20% and 30% produced ρ dmax = 1.62 Mg/m 3  Standard Proctor compaction curves, along with corresponding zero-air void (ZAV) saturation lines, for the natural soil and various GR-blended samples untreated-SP0Ry where y = {0, 5, 10, 20, 30}-and treated with 0.2 g/l PAM-SP0.2Ry where y = {0, 5, 10, 20, 30}-are provided in Figures 6a  and 6b, respectively. As a result of GR inclusion, the compaction locus underwent a linear downward-leftward translation over the ρd:w space, thus indicating a notable decrease in both the maximum dry density and the optimum moisture content associated with increasing GR content (follow the "Compaction Path" in Figure 6). The greater the GR content, the lower the compaction characteristics, with PAM-treated cases holding a slight advantage over their untreated counterparts. The natural soil (SP0R0) and the untreated GR-blended samples with Rc = 5%, 10%, 20% and 30% produced ρdmax = 1.62 Mg/m 3   Reduction in the compaction characteristics, particularly the maximum dry density, advocates the use of GR as a sustainable, lightweight fill alternative to traditional quarried materials, such as sands and aggregates. The GR material's lower specific gravity of 1.09 and hydrophobic character (< 4% water adsorption) compared with that of the soil grains, and active clay minerals in particular, corroborate the observed reduction in the compaction characteristics [36,37,57]. Moreover, the compacted GR particles, though rather resilient, may gradually recover their initial shape due to the elastic rebound, thereby reducing the efficiency of compactive effort and hence leading to lower maximum dry densities [26,57].

Effect of PAM + GR on UCS
Stress-strain curves for the natural soil and various GR-blended samples untreated-SP0Ry where y = {0, 5, 10, 20, 30}-and treated with 0.2 g/l PAM at Tc = 7 d-SP0.2Ry where y = {0, 5, 10, 20, 30}-are provided in Figures 7a and 7b, respectively. As a result of increasing GR content, the constitutive response progressively transitioned towards a strain-hardening character; the greater the GR content, the more pronounced the strain-hardening effect and hence the more ductile the failures (see Figure 7a). For any given GR content, the addition of PAM further enhanced the strainhardening failure mode, while simultaneously enhancing the sample's UCS and stiffness (see Figure   1 Dry density, ρ  Reduction in the compaction characteristics, particularly the maximum dry density, advocates the use of GR as a sustainable, lightweight fill alternative to traditional quarried materials, such as sands and aggregates. The GR material's lower specific gravity of 1.09 and hydrophobic character (<4% water adsorption) compared with that of the soil grains, and active clay minerals in particular, corroborate the observed reduction in the compaction characteristics [36,37,57]. Moreover, the compacted GR particles, though rather resilient, may gradually recover their initial shape due to the elastic rebound, thereby reducing the efficiency of compactive effort and hence leading to lower maximum dry densities [26,57].

Effect of PAM + GR on UCS
Stress-strain curves for the natural soil and various GR-blended samples untreated-SP 0 R y where y = {0, 5, 10, 20, 30}-and treated with 0.2 g/L PAM at T c = 7 d-SP 0.2 R y where y = {0, 5, 10, 20, 30}-are provided in Figure 7a,b, respectively. As a result of increasing GR content, the constitutive response progressively transitioned towards a strain-hardening character; the greater the GR content, the more pronounced the strain-hardening effect and hence the more ductile the failures (see Figure 7a). For any given GR content, the addition of PAM further enhanced the strain-hardening failure mode, while simultaneously enhancing the sample's UCS and stiffness (see Figure 7b). In terms of UCS, the greater the GR content, the higher the UCS up to R c = 10%, beyond which GR inclusion was found to adversely influence strength development (follow the "Strength Path" in Figure 7a). When treated with PAM, the UCS exhibited the same rise-fall behavior with GR content; however, all treated cases outperformed their untreated counterparts (follow the "Strength Path" in Figure 7b). The natural soil (SP 0 R 0 ) resulted in q u = 72.28 kPa, while the addition of 5% and 10% GR produced higher values of 91.21 kPa and 98.61 kPa-equivalent to improvements of η = 26% and 36%-respectively.
The higher GR contents of 20% and 30% resulted in lower values of q u = 62.28 kPa and 46.61 kPa, respectively; equating to major reductions of 14% and 36% with respect to the natural soil. As a result of PAM-treatment, the aforementioned values increased to 164.47 kPa, 208.94 kPa, 211.09 kPa, 106.18 kPa and 65.15 kPa, respectively. The latter, SP 0.2 R 30 , corresponds to a notable 10% UCS reduction with respect to the natural soil, while the former cases, i.e., SP 0.2 R 0 , SP 0.2 R 5 , SP 0.2 R 10 and SP 0.2 R 30 , signify major improvements of 128%, 189%, 192% and 47%, respectively. 7b). In terms of UCS, the greater the GR content, the higher the UCS up to Rc = 10%, beyond which GR inclusion was found to adversely influence strength development (follow the "Strength Path" in Figure 7a). When treated with PAM, the UCS exhibited the same rise-fall behavior with GR content; however, all treated cases outperformed their untreated counterparts (follow the "Strength Path" in Figure 7b). The natural soil (SP0R0) resulted in qu = 72.28 kPa, while the addition of 5% and 10% GR produced higher values of 91.21 kPa and 98.61 kPa-equivalent to improvements of η = 26% and 36%-respectively. The higher GR contents of 20% and 30% resulted in lower values of qu = 62.28 kPa and 46.61 kPa, respectively; equating to major reductions of 14% and 36% with respect to the natural soil. As a result of PAM-treatment, the aforementioned values increased to 164.47 kPa, 208.94 kPa, 211.09 kPa, 106.18 kPa and 65.15 kPa, respectively. The latter, SP0.2R30, corresponds to a notable 10% UCS reduction with respect to the natural soil, while the former cases, i.e., SP0.2R0, SP0.2R5, SP0.2R10 and SP0.2R30, signify major improvements of 128%, 189%, 192% and 47%, respectively. Other stress-strain features-the deformability index ID, the elastic stiffness modulus E50, the peak strain energy (or toughness) EU and the resilient modulus ER-are summarized in Table 8. The greater the GR content, the higher the deformability index and the lower the E50 value, with PAMtreated cases generally promoting higher values compared with similar untreated cases. Moreover, the peak strain energy and the resilient modulus both demonstrated trends similar to that observed for the UCS. The greater the GR content, the higher the EU and ER values up to Rc = 10%, beyond which GR inclusion adversely influenced the sample's toughness and resilience. Moreover, the samples treated with PAM consistently outperformed their untreated counterparts by exhibiting higher EU and ER values. In terms of stiffness, for instance, the samples SP0R0, SP0R5, SP0R10, SP0R20 and SP0R30 resulted in E50 = 1.   Other stress-strain features-the deformability index I D , the elastic stiffness modulus E 50 , the peak strain energy (or toughness) E U and the resilient modulus E R -are summarized in Table 8. The greater the GR content, the higher the deformability index and the lower the E 50 value, with PAM-treated cases generally promoting higher values compared with similar untreated cases. Moreover, the peak strain energy and the resilient modulus both demonstrated trends similar to that observed for the UCS. The greater the GR content, the higher the E U and E R values up to R c = 10%, beyond which GR inclusion adversely influenced the sample's toughness and resilience. Moreover, the samples treated with PAM consistently outperformed their untreated counterparts by exhibiting higher E U and E R values. In terms of stiffness, for instance, the samples SP 0 R 0 , SP 0 R 5 , SP 0 R 10 , SP 0 R 20 and SP 0 R 30 resulted in E 50 = 1.   1 Percent change in the UCS (or q u ); 2 Axial strain at failure; 3 I D = ε u S /ε u N where ε u S = axial strain at failure for the stabilized sample, and ε u N = axial strain at failure for the natural soil [63]; 4 E 50 = secant modulus at 50% of the UCS (or q u ) [66]; 5 E U = area under the stress-strain curve up to the failure point [65]; and 6 Computed from E R (psi) = 124 × q u (psi) + 9980, as suggested by Thompson [64]. Figure 8 illustrates the variations of shrinkage and swelling potentials, ε sh and ε sw , against GR content for the natural soil and various GR-blended samples, untreated and treated with 0.2 g/L PAM-SP x R y where x = {0, 0.2}, and y = {0, 5, 10, 20, 30}. The greater the GR content, the lower the shrinkage and swelling potentials, following a monotonically-decreasing trend, with PAM-treated cases achieving a notable advantage over their untreated counterparts (compare the trendlines "SP 0 R y " and "SP 0.2 R y " in Figure 8). In terms of swelling, for instance, the natural soil (SP 0 R 0 ) resulted in ε sw = 3.69%, while the samples SP 0 R 5 , SP 0 R 10 , SP 0 R 20 and SP 0 R 30 exhibited lower values of 3.03%, 2.11%, 1.77% and 1.61%, respectively. Similar mix designs treated with PAM led to superior performance, as the aforementioned values dropped to 1.98%, 1.74%, 1.54%, 1.34% and 1.14%, respectively. Shrinkage/Swelling potential, ε sh or ε sw  The complete results of the soil reactivity tests, including the total suction measurements, are summarized in Table 9. As a result of GR inclusion, the initial (or as-compacted) suction ψ o exhibited a notable overall increase, with PAM-treated cases promoting higher values compared with similar untreated cases. The natural soil resulted in ψ o = 4.73 pF (where [pF] = 1 + log[kPa]), while the addition of 5%, 10%, 20% and 30% GR produced higher values of 4.75 pF, 4.78 pF, 4.77 pF and 4.76 pF, respectively. When treated with PAM, the aforementioned values further increased to 4.74 pF, 4.77 pF, 4.81 pF, 4.79 pF and 4.77 pF, respectively. Unlike the initial suction, both the shrinkage and swelling suctions, ψ sh and ψ sw , were inversely-proportional to the GR content; the effect of PAM, however, was directly-and inversely-proportional to ψ sh and ψ sw , respectively (see Table 9). The natural soil exhibited a total suction change of ∆ψ = ψ sh − ψ sw = 2.07 pF, which is higher than the standard 1.8 pF value commonly adopted in practice. As a result of GR inclusion, ∆ψ exhibited a notable increasing trend; it was measured as 2.09 pF, 2.09 pF, 2.28 pF and 2.28 pF for R c = 5%, 10%, 20% and 30%, respectively. Similar mix designs treated with PAM produced higher ∆ψ values of 2.11 pF, 2.11 pF, 2.14 pF, 2.32 pF and 2.30 pF, respectively. These trends can be attributed to the partial replacement of the hydrophilic soil grains with hydrophobic GR particles, as well as the lower molding/as-compacted moisture content of various GR-blended samples compared with that of the natural soil (e.g., see Figure 6a). Moreover, the effect of PAM on total suction, particularly for the as-compacted state, can be ascribed to its particle flocculation capacity, as well as the higher molding dry density (or lower void ratio) of PAM-treated samples compared with similar untreated cases (e.g., see Figure 6b).  Figure 9a,b illustrate the variations of the conventional and modified shrink-swell indices (I ssc and I ssm , respectively) against GR content for the tested samples. As is evident from Table 9, the actual total suction change ∆ψ was consistently greater than the standard 1.8 pF value; as such, by definition (see Equation (6)), one can conclude that I ssc > I ssm . The greater the GR content, the lower the shrink-swell indices, following a monotonically-decreasing trend, with PAM-treated cases outperforming similar untreated cases in terms of their lower shrink-swell indices. As typical cases outlined in Figure 9b, the samples SP 0 R 0 , SP 0 R 5 , SP 0 R 10 , SP 0 R 20 and SP 0 R 30 resulted in I ssm = 3.66 %pF −1 , 3.28 %pF −1 , 2.84 %pF −1 , 1.67 %pF −1 and 1.17 %pF −1 , respectively. When treated with PAM, the aforementioned values dropped to 2.14 %pF −1 , 1.97 %pF −1 , 1.58 %pF −1 , 1.40 %pF −1 and 0.82 %pF −1 , respectively.

Amending Mechanisms
Polymers, for the most part, alter the soil fabric through clay-polymer interactions [51]. Cationic polymers are readily adsorbed onto the negatively-charged clay particle surfaces through Coulombic (or electrostatic) attraction; this process induces localized charge reversal on each clay particle, thereby allowing localized areas with opposite charge between different clay particles to interact and form flocs [67,68]. Neutral (non-ionic) polymers, on the other hand, achieve adsorption through van der Waals and/or hydrogen bonding [67][68][69]. Although clay particles tend to repel anionic polymers due to charge repulsion, which would be the case for the anionic PAM used in this study, attraction can still be achieved through exchangeable, divalent cations in the clay-water medium, e.g., calcium (Ca 2+ ) and magnesium (Mg 2+ ), which act as so-called "bridges" between the polymer and the clay particle surfaces [53,67,70,71]. The development and propagation of these strong cationic bridges between adjacent clay particle surfaces in the matrix lead to a decrease in the thickness of the diffused double layers, which in turn induced aggregation and flocculation of the clay particles and hence   As demonstrated in Table A2, the shrink-swell index can be used to specify the soil degree of expansivity [59]-corresponding classifications based on the I ssc and I ssm indices are outlined in Figure 9a As it stands, the conventional shrink-swell index, computed based on ∆ψ = 1.8 pF, tends to overestimate the expansive potential of the test soil and various soil-GR blends, and thus can be deemed as a conservative approach [60]. The modified index, however, offers a more progressive and hence sustainable classification scheme.

Amending Mechanisms
Polymers, for the most part, alter the soil fabric through clay-polymer interactions [51]. Cationic polymers are readily adsorbed onto the negatively-charged clay particle surfaces through Coulombic (or electrostatic) attraction; this process induces localized charge reversal on each clay particle, thereby allowing localized areas with opposite charge between different clay particles to interact and form flocs [67,68]. Neutral (non-ionic) polymers, on the other hand, achieve adsorption through van der Waals and/or hydrogen bonding [67][68][69]. Although clay particles tend to repel anionic polymers due to charge repulsion, which would be the case for the anionic PAM used in this study, attraction can still be achieved through exchangeable, divalent cations in the clay-water medium, e.g., calcium (Ca 2+ ) and magnesium (Mg 2+ ), which act as so-called "bridges" between the polymer and the clay particle surfaces [53,67,70,71]. The development and propagation of these strong cationic bridges between adjacent clay particle surfaces in the matrix lead to a decrease in the thickness of the diffused double layers, which in turn induced aggregation and flocculation of the clay particles and hence favored an enhanced strength performance coupled with a reduced tendency for swell-shrink volume changes. It should be noted that the maximum strength benefits of flocculation are often achieved when polymers, and anionic PAMs in particular, cover a surface area equivalent to half the polymer's saturation capacity [72]. An increase in polymer concentration beyond this level causes the excess polymer material to act as a lubricant rather than a flocculant; this feature facilitates the sliding of soil aggregates across each other, and thus may adversely influence certain mechanical attributes, such as the stress-strain-strength response. This mechanism elucidates the observed reduction in the UCS (see Table 7), as well as the minor variations noted in the consistency limits (see Table 4) and the sediment volume features (see Table 5), for PAM concentrations greater than 0.2 g/L. Figure 10a,b illustrate typical SEM micrographs for the natural soil (SP 0 R 0 ) and the sample treated with 0.2 g/L PAM (SP 0.2 R 0 ), respectively. The microfabric of the natural soil sample, as outlined in Figure 10a, showed a partly-dense, non-uniform matrix. Moreover, a notable number of large interand intra-assemblage pore-spaces developed between and within the soil aggregates, respectively, were found to dominate the soil matrix; these pore-spaces facilitate the entrance of water into the sample during swelling [3]. As a result of PAM-treatment (see Figure 10b), the microfabric became more uniform in nature, signifying aggregation and flocculation of the clay particles (owing to the cationic bridging mechanism), and thus the development of a fully-dense matrix with a dominant edge-to-face flocculated fabric. Polymeric membranes were also clearly visible between and within the soil aggregates, which play a major role in reducing the number and extent of the inter-and intra-assemblage pore-spaces, thereby favoring significant improvements in the soil's UCS and volume change behaviors.
Much like fiber-reinforced soils, the GR inclusions are able to alter the soil fabric through improvements achieved in three aspects: (i) increase in non-expansive content; (ii) frictional resistance generated at soil aggregate-GR interfaces; and (iii) mechanical interlocking of soil and GR particles [1,3,4,26,33,34]. The swell-shrink capacity is primarily a function of the soil's expansive clay content. An increase in GR content substitutes a larger portion of the expansive clay content with non-plastic, hydrophobic rubber particles, thereby leading to a further decrease in the swell-shrink capacity (see Table 9). The generated interfacial frictional resistance is a function of the soil aggregate-GR contact area, with greater contact levels offering a higher shear resistance against external forces. The greater the number of included GR particles (i.e., increase in GR content), the greater the contact levels achieved between the GR particles and soil aggregates, and thus the higher the developed frictional resistance against compression and swell-shrink movements. The mechanical interlocking of soil aggregates and GR particles is achieved during sample preparation (or compaction); it may induce sample adhesion by immobilizing the soil aggregates undergoing shearing, swelling and shrinkage.
Quite clearly, the more pronounced the achieved mechanical interlocking, the higher the resistance against compression and swell-shrink movements. As such, this amending mechanism can also be ascribed to the GR content-the greater the GR content, the greater the number of potentially interlocked soil aggregates, and thus the higher the developed resistance against compression, swelling and shrinkage. In practice, however, the latter two amending mechanisms, interfacial frictional resistance and mechanical interlocking, only hold provided that the GR particles are well distributed in the soil medium-meaning that the GR particles do not cluster during compaction [1,27,36]. At high GR contents, the behavior at some points within the blended sample could be governed by a dominant GR-to-GR interaction; this effect, referred to as rubber-clustering, promotes a notable improvement in the sample's ductility/deformability while offsetting the desired soil-to-GR interaction capable of enhancing its UCS (follow the "Strength Path" in Figure 7a). Such adverse effects were evident for all samples containing 20% and 30% GR, as the previously-improved UCS dropped below that of the natural soil (e.g., compare the samples "SP 0 R 10 " and "SP 0 R 20 " in Figure 7a). When treated with PAM, the soil aggregate-GR connection interface can be further improved, as PAM facilitates the embedment of GR particles between the flocculated soil aggregates with increased efficiency; this leads to further improvements in the sample's UCS and swell-shrink capacity (see Figure 7b and Table 9). Much like fiber-reinforced soils, the GR inclusions are able to alter the soil fabric through improvements achieved in three aspects: (i) increase in non-expansive content; (ii) frictional resistance generated at soil aggregate-GR interfaces; and (iii) mechanical interlocking of soil and GR particles [1,3,4,26,33,34]. The swell-shrink capacity is primarily a function of the soil's expansive clay content. An increase in GR content substitutes a larger portion of the expansive clay content with non-plastic, hydrophobic rubber particles, thereby leading to a further decrease in the swell-shrink capacity (see Table 9). The generated interfacial frictional resistance is a function of the soil aggregate-GR contact area, with greater contact levels offering a higher shear resistance against external forces. The greater the number of included GR particles (i.e., increase in GR content), the greater the contact levels achieved between the GR particles and soil aggregates, and thus the higher the developed frictional resistance against compression and swell-shrink movements. The mechanical interlocking of soil aggregates and GR particles is achieved during sample preparation (or compaction); it may induce sample adhesion by immobilizing the soil aggregates undergoing shearing, swelling and shrinkage. Quite clearly, the more pronounced the achieved mechanical interlocking, the higher the resistance against compression and swell-shrink movements. As such, this amending mechanism can also be ascribed to the GR content-the greater the GR content, the greater the number of potentially interlocked soil aggregates, and thus the higher the developed resistance against compression, swelling and shrinkage. In practice, however, the latter two amending mechanisms, interfacial frictional resistance and mechanical interlocking, only hold provided that the GR particles are well distributed in the soil medium-meaning that the GR particles do not cluster during compaction [1,27,36]. At high GR contents, the behavior at some points within the blended sample could be

Concluding Remarks
The present study has arrived at the following conclusions.

•
The greater the PAM concentration, the higher the consistency limits and the lower the FSR up to 0.2 g/L PAM, beyond which the effect of PAM-treatment was found to be marginal. Hence, the optimum PAM concentration for particle flocculation was achieved at 0.2 g/L PAM.

•
The greater the PAM concentration, the higher the maximum dry density, while the variations in optimum moisture content were rather marginal. An increase in pore-fluid viscosity, as is the case with PAM-treated blends, induces contact lubrication in the soil matrix. During compaction, this feature facilitates reduced overall resistance to the movement and sliding of soil particles relative to each other, thereby allowing a closer packing of the soil particles and hence the development of a higher maximum dry density.

•
Further, the greater the PAM concentration, the higher the developed UCS, stiffness and toughness up to 0.2 g/L PAM, beyond which PAM-treatment was found to adversely influence these properties. An increase in PAM beyond 0.2 g/L, the optimum concentration, caused the excess PAM to act as a lubricant rather than a flocculant. During compression, this feature facilitated easier sliding of the soil particles relative to each other, thereby adversely influencing the previously-improved stress-strain-strength response.

•
As a result of GR inclusion, both the maximum dry density and the optimum moisture content exhibited a linear, monotonically-decreasing trend with increasing GR content. The reduction in the maximum dry density, in particular, advocates the use of GR as a sustainable, lightweight alternative for common quarried fill materials, such as sands and aggregates. • Further, the greater the GR content, the higher the developed UCS and toughness up to 10% GR, beyond which the dominant GR-to-GR interaction (i.e., rubber-clustering) adversely influenced the blended samples' UCS and toughness. The sample stiffness, however, exhibited a monotonically-decreasing trend with GR content. Moreover, reduction in the swell-shrink capacity, and thus the degree of expansivity/reactivity, was consistently in favor of higher GR contents.

•
The addition of PAM to the GR-blended samples enhanced the soil aggregate-GR connection interface, thereby producing further improvements in the samples' compactability, stress-strain-strength response and swell-shrink capacity. A maximum GR content of 20%, paired with 0.2 g/L PAM, managed to satisfy a major decrease in the swell-shrink capacity while improving the strength-related features, and thus was deemed as the optimum choice. ZAV Zero-air void Appendix A Figure A1 shows a photograph of the anionic PAM, in its granular form, used in the present investigation. Figure A1. Anionic PAM in its granular form.
Classification procedures for expansive soils based on the FSR, as proposed by Prakash and Sridharan [50], are summarized in Table A1. Very High Montmorillonite 1 Ratio of equilibrium sediment volume of 10 g oven-dried soil, passing 425 μm sieve, in distilled water to that of kerosene.
Classification procedures for expansive soils based on the shrink-swell index Iss, as suggested by Seddon [59], are summarized in Table A2.  (6); and 2 Free ground surface movement. Figure A1. Anionic PAM in its granular form.
Classification procedures for expansive soils based on the FSR, as proposed by Prakash and Sridharan [50], are summarized in Table A1. Classification procedures for expansive soils based on the shrink-swell index I ss , as suggested by Seddon [59], are summarized in Table A2.