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Water-repellent soils have a potential as alternative construction materials that will improve conventional geotechnical structures. In this study, the potential of chemically treated water-repellent kaolin clay as a landfill cover material is explored by examining its characteristics including hydraulic and mechanical properties. In order to provide water repellency to the kaolin clay, the surface of clay particle is modified with organosilanes in concentrations (CO) ranging from 0.5% to 10% by weight. As the CO increases, the specific gravity of treated clay tends to decrease, whereas the total organic carbon content of the treated clay tends to increase. The soil-water contact angle increases with an increase in CO until CO = 2.5%, and then maintains an almost constant value (≈134.0°). Resistance to water infiltration is improved by organosilane treatment under low hydrostatic pressure. However, water infiltration resistance under high hydrostatic pressure is reduced or exacerbated to the level of untreated clay. The maximum compacted dry weight density decreases with increasing CO. As the CO increases, the small strain shear modulus increases, whereas the effect of organosilane treatment on the constrained modulus is minimal. The results indicate that water-repellent kaolin clay possesses excellent engineering characteristics for a landfill cover material.
Landfill needs a final cover system to prevent the uncontrolled release of landfill gas and the infiltration of precipitated water into the waste [1,2]. Although conventional cover systems such as compacted clay liners, geomembranes, and geosynthetic clay liners have been successfully utilized [1,3], those systems may not provide a feasible solution in regions with arid climates [4,5]. Thus, the evapotranspiration cover system (ET) has been suggested as an alternative.
The ET cover system relies on the water storage capacity of the soil layer, rather than the hydraulic conductivity of the soil layer, to minimize the infiltration. The soil layer retains precipitated water until the water evaporates from the surface or transpires through vegetation . Two general types of ET cover systems have been used: a monolithic barrier and a capillary barrier. A monolithic barrier uses a single layer of fine-grained soil such as silt or clayey silt, whereas a capillary barrier consists of a fine soil layer over a coarser layer. Although a capillary barrier can retain more water than a monolithic cover with equal thickness [6,7,8], the retained water can infiltrate relatively quickly into the body of the landfill when a fine-grained soil layer within a capillary barrier becomes fully saturated [9,10].
One possible technique to enhance the ET cover system is to employ water-repellent soil material as an infiltration barrier layer . Since water on a hydrophobic surface forms distinct droplets, water-repellent soils can resist or retard water infiltration through the soil surface . Water-repellent soil can be made by natural or anthropogenic processes, such as wildfire, microbial activity, exudates from living plants, decomposition of litter, oil spills, and cultivation of crops [13,14,15,16]. Although natural water-repellent soils are commonly found throughout the world , they may be unsuitable engineering materials because of highly anisotropic and heterogeneous water-repellent characteristics and the likelihood that natural water repellants will not persist for long. Therefore, artificially created water-repellent soils by using wax , organosilanes [18,19], and other hydrophobic agents [11,20] have recently been investigated because they exhibit homogeneous water repellency and it is easy to control the degree of water repellency. Because artificial water-repellent sandy soils can be used as alternative construction materials for several purposes, such as surfaces for horse racing tracks , waterproofing layer of highways , water harvesting , and landfill barrier systems [22,23,24], many studies have been performed to characterize the engineering properties of artificial water-repellent sands. In contrast, there is a lack of research on artificially treated water-repellent clays as a construction material.
Clayey soils have typically been used as barriers to control water infiltration because of their low permeability. Additionally, water-repellent soils are well suited for controlling infiltration. Consequently, in this study, the potential of water-repellent clay used as a landfill cover material is explored by assessing engineering characteristics including hydraulic and mechanical properties. Kaolin clay was chemically treated with different concentrations of organosilane solutions to produce samples with different degrees of water repellency. These samples were subjected to a series of hydraulic and mechanical experiments to measure the soil-water contact angle, water infiltration time, infiltration rate, compaction characteristics, compressibility, and small strain shear modulus.
The kaolin clay used in this study was purchased from Lakwoo Industry Co. Ltd., Gyeongnam Province, Korea. The mineralogy of the clay was assessed using X-ray diffraction (XRD) (Philips, X’Pert MPD, Almelo, The Netherlands). The clay consists mainly of kaolinite, with a minor amount of halloysite (Figure 1). The chemical composition of the clay was measured using X-ray fluorescence (XRF) spectrometry (Philips, PW2404, Almelo, The Netherlands). The majority of the chemical elements are silicon (Si) and aluminum (Al) as shown in Table 1. The specific gravity (Gs), measured by a gas pycnometer (PMI, PYC-G100A-1, Ithaca, NY, USA), of the kaolin clay is 2.64, and the plastic and liquid limits of the soil are 23.6% and 35.9%, respectively. The median grain size (D50) of untreated kaolin is 10.35 μm. The specific surface area of the kaolin is 13.46 m2/g (methylene blue spot test) , and the pH value of the kaolin is 7.3 . The total organic carbon (TOC) content, measured with a TOC analyzer (Shimadzu, TOC-VCPH, Kyoto, Japan), of the kaolin is 0.062% ± 0.012%. The untreated kaolin was classified as clay with low plasticity (CL), in accordance with the Unified Soil Classification System .
To create a water-repellent clay, kaolin clay was treated with an organosilane (Zycosoil, Zydex industries, Vadodara, India) in this study. Figure 2 shows the chemical structure of Zycosoil. The composition of Zycosoil is 40% 3-(trimethoxysilyl)propyl dimethyloctadecyl ammonium chloride (organosilane) and 60% ethylene glycol (solvent) [18,28]. When Zycosoil is diluted with water and mixed with soil, the hydrolyzable group forms siloxane bonds with the soil surface, and the non-hydrolyzable group imparts hydrophobicity to the soil surface [18,29]. Note that the XRD patterns of the treated clays are similar to the XRD pattern of untreated clay.
The water-repellent clay was prepared according to the method of Lee et al. . The kaolin was thoroughly washed several times with deionized water to remove any contaminants and then dried in an oven (Hyundae Precision Industry, Seoul, Korea) for 24 h. 3 kg of the dried soil was mechanically blended with deionized water (6 L) for 24 h to ensure complete dispersion. In order to assign different degrees of water repellency, six different concentrations (CO) of Zycosoil (WZycosoil/Wwater = 0.5%, 0.75%, 1%, 2.5%, 5%, and 10%) were poured into the slurry (Table 2). After continuous stirring for 24 h, the treated clay was washed several times with deionized water to remove surplus organosilane and then dried in an oven for 24 h. Prior to experimentation, the oven-dried clay was ground with a mortar and pestle, and the ground soil was sieved with a #60 sieve.
Six different experiments were performed to explore the effect of water repellency on the following characteristics: soil-water contact angle, water infiltration time, water infiltration rate, compaction characteristics, constrained modulus, and small strain shear modulus.
Measurement of the solid-water contact angle is a direct method of assessing the degree of water repellency of a solid surface [30,31]. A homogeneous and absolutely flat surface is required to precisely measure the contact angle. Since it is impossible to obtain a sufficiently large flat area to measure a direct contact angle with a single soil particle, the sessile drop contact angle method (SDM) has been proposed .
One side of double-sided adhesive tape was attached to a slide glass, and then the oven-dried soil samples were sprinkled on the other side. The soil layer on the slide glass was compressed with a 100 g weight for 10 s, and then the slide was tapped carefully to remove unattached grains. After repeating this procedure twice, 10 drops of deionized water (2 ± 0.1 μL) were placed on the surface of the specimen with a micropipette (Axygen, AP-10, Corning, NY, USA) . Horizontal images of the water droplets were captured within 5 s with a digital camera (Canon, PowerShot G9, Tokyo, Japan).
The effect of water repellency and water pressure (WP) on infiltration time are explored by conducting an experiment as follows. Note that water infiltration time (WIT) is defined as the time until infiltrating water reaches the bottom of a specimen under a constant WP. To estimate the WIT, the soil samples were prepared in a cylindrical cell, 30 mm in inner diameter and 120 mm in height. The cell was made of polytetrafluoroethylene (PTFE) to prevent water from flowing between the soil sample and the wall . Two electrodes and a filter paper at the bottom of the cell were used to determine the moment when infiltrated water wetted the paper. The soil was scooped into the cell and then tapped to achieve a constant porosity (n) of approximately 0.5 and a constant soil height of approximately 60 mm . After the empty space on the soil in the cell was filled with deionized water, WP (10 kPa, 15 kPa, 20 kPa, or 30 kPa) was applied from the top using a pressure panel (Trautwein, M100000, Houston, TX, USA). Note the selected WPs in this study reflect the typical thickness of a fine-grained soil layer of ET cover systems (i.e., typically ranging from 0.4 m to 3 m) .
After the infiltrating water reaches the bottom of a specimen, the volume of outflow was measured over time to calculate the infiltration rate. Note that the infiltration rate was calculated for a given soil sample once a steady outflow was achieved . The specimen was then extracted from the cell to measure the water content for estimating the degree of saturation (S).
The compaction characteristics of the treated specimens were evaluated using a standard compaction mold (101.6 mm in diameter, Hyundae Precision Industry, Seoul, Korea) and a standard rammer (24.5 N, Hyundae Precision Industry, Seoul, Korea) . Since the water-repellent clays were not easily wetted, the soil samples were prepared by thoroughly mixing with a deionized water for 30 min and then stored in a sealed plastic bag for 24 h before the compaction test. This procedure assures a more homogenous distribution of water in the water-repellent soil specimens [35,36]. The wetted soil was placed in three layers into the mold and each layer was compacted by 25 blows of the rammer with a falling height of 305 mm. The weight of the compacted soil was measured, and then three soil samples were obtained from the top, middle, and bottom of the specimens in order to determine the water content. This compaction procedure was repeated for each soil sample to establish compaction curves. Compaction characteristics, such as optimum volumetric water content (θopt) and maximum dry unit weight (γd(max)), were determined from the compaction curves.
The constrained modulus and small strain modulus of the tested materials were explored using a zero-lateral strain (K0) oedometer cell . The oedometer cell, made of brass, is 74 mm in diameter and 63 mm in height, with a wall thickness of 16 mm. The bender elements were installed in the top cap and bottom plate to measure a shear wave velocity (Vs) of specimens. The soil samples were made of five layers. The dry soil was carefully scooped into the cell and densified by a static load of 7 kg within 10 s. The initial height of the soil specimens was approximately 45 mm. The vertical effective stress was incrementally doubled during each of the six loading steps until the vertical effective stress reached 625 kPa. Each loading step lasted for 1 h. Note that the rate of settlement prior to applying the next loading step was less than 0.001 mm/min. Settlement was measured using a linear variable differential transformer (LVDT) transducer (Macro sensors, GHSE 750-500, repeatability error <0.6 μm, Pennsauken Township, NJ, USA) with a DC power supply (Agilent, E3634A, Santa Clara, CA, USA) and a data logger (Agilent, 34970A, Santa Clara, CA, USA). In addition, the shear waves were measured at the end of each loading step using the following electronic peripherals. A signal generator (Agilent, 33220A, Santa Clara, CA, USA) provided a single sinusoidal signal as an input to the source bender element. The shear wave emitted from the source and propagated through the specimen was detected at the receiver bender element. The signal from the receiver was filtered and amplified by a filter amplifier (Krohn-Hite, 3364, Brockton, MA, USA). The filtered and amplified signal was digitized by an oscilloscope (Agilent, 54624A, Santa Clara, CA, USA). A total of 1024 signals were averaged to eliminate random noise. The shear wave velocity was calculated from the traveling distance, which is the tip-to-tip distance between the bender elements, and the first arrival time. The first arrival was identified from the recorded signal taking into consideration the near-field effect .
To examine the grafted pattern of organosilanes after treatment, field emission scanning electron microscopic (FESEM) and energy dispersive X-ray (EDX) analyses were carried out using a Hitachi S-4300 instrument. Figure 3 shows selected FESEM images of untreated and treated clays at CO = 1% and 10%, and Table 3 shows EDX results of the marked areas in Figure 3. As shown in Figure 3a, angular and flat shaped kaolin particles are observed. The EDX analysis of untreated clay (e.g., area U-1 and U-2 in Table 3) reveals that the majority of its chemical elements are oxygen (O), aluminum (Al), and silicon (Si), with some minor elements including sodium (Na) and calcium (Ca). In the case of the treated clays, organosilanes grafted onto the particle surfaces can be seen in the FESEM images (e.g., area C1-1 and C1-2 in Figure 3c, and area C10-2 in Figure 3e). Note that the silane-grafted areas are brighter than the non-grafted areas in the FESEM images because of the difference in the mass intensity of the coated platinum. Irregular spatial distribution patterns of grafted silanes are evident in Figure 3c–f. Some areas are covered with a large amount of silanes with amalgamated structures, as shown in areas C1-1 and C1-2, while others are covered with fewer silanes, as in area C1-4, or are not coated such as areas of C1-3, C10-1, and C10-3. The irregular spatial distribution patterns of grafted silanes would be related to heterogeneous surface minerals (Figure 3b) due to presence of low and high surface energy sites of the mineral, because the silylation relies on the reactivity of the clay mineral surface . As the CO increases, the treated clay is covered with a greater amount of silanes with amalgamated structures, such as in area C10-2. The EDX results for treated clay (Table 3) show the presence of additional chemical elements, as compared with the untreated clay. Since the organosilane contains organic carbon molecules (Figure 2), carbon (C) is the main addition to the treated clay, while minor chemical elements (such as magnesium (Mg) and iron (Fe)) are also added. As the CO increases from 0% to 1%, the atomic percentage of carbon in the particle surface increased to 11.90%–16.88%. Additionally, the atomic percentage of carbon in the treated clay with CO = 10% is 21.84%. Note that the different silane grafting pattern shown in Figure 3c,e also clearly supports the difference in the concentration of carbon within grafted silanes.
Grafting organosilane onto a soil particle may change the index properties of the soil, such as specific gravity (Gs), particle size, TOC, and Atterberg limits, although relevant findings have rarely been reported until now [11,40]. To explore the effects of grafting organosilane on the index properties of soil, the Gs and TOC of water-repellent clay were measured.
Figure 4a shows the variation in Gs of both untreated and treated soils according to CO. Since the Gs of the organosilane (=0.89 in this study) are much lower than that of the untreated kaolin (=2.638), the Gs of the treated soil decreases as CO increases (Figure 4a). The Gs value of organosilane grafted soil (Gs_prediction) can be predicted as follows:
where γw is the density of water (g/cm3), Msoil (or Vsoil), and Madded silanes (or Vadded silanes) are the mass (or volume) of untreated soil and added silanes in the reaction solution, respectively. Gs values show a relatively good agreement with the values of Gs_prediction at a reaction efficiency of 0.9. Figure 4b shows the measured TOC values as a function of CO. Note that inorganic carbons are not detected in either the untreated or treated clays. Since the organosilane contains organic carbons, the TOC of the treated soil increases with increasing CO. The TOC value of treated soil (TOCprediction) can be predicted, as in Equation (2) below, with the assumptions that all of the carbon elements in the organosilane are regarded as organic carbon and there are no reactions between organosilane molecules.
where MTOC of soil, MTOC of grafted silanes, and MTOC of added silanes are the mass of total organic carbon in the untreated soil, grafted silanes on the soil particles, and added silanes in the reaction solution, respectively. The measured TOC values were similar to the TOCprediction with an input of reaction efficiency = 0.9–1.0. These analyses (Figure 4) reveal that the efficiency of silylation, in this study, is about 0.9–1.0. Also, the almost constant reaction efficiency with increasing CO in Figure 4 indicates that: (1) the mass of grafted organosilanes on clay particles almost linearly increases with increasing CO; and (2) the end point of silylation is not reached until CO = 10%.
Figure 5 presents the soil-water contact angles of the tested water-repellent clays with an increase in CO from 0.5% to 10%. The soil-water contact angles tend to increase with increasing CO until CO = 2.5%, and then remain almost constant (≈134.0°) with a further increase in CO. Previous studies [20,41] also observed a similar trend, and Johnson and Dettre  reported that the advancing contact angle is almost constant when the coverage of non-wettable regions exceeds 40% of the total surface based on theoretical analysis for an idealized heterogeneous surface. Note a contact angle measured by SDM is often regarded as an advancing contact angle . Consequently, the almost constant values of the measured contact angle in Figure 5 may imply that the clay particles were sufficiently covered with organosilanes when the CO is approximately 2.5%. Note that a constant contact angle does not imply a constant amount of grafted organosilanes and degree of water repellency with further increase in CO.
The infiltration is mainly governed by two forces such as capillary and gravity forces . Note that the value of capillary force would be changed from negative value (i.e., hydrophilic soil) to positive value (i.e., hydrophobic soil) when the soil was treated by organosilane. Therefore, the phenomenon of water infiltration is significantly related to hydrostatic water pressure (WP) on the soil surface and soil properties such as porosity, fabric, and degree of water repellency [33,45]. If the WP is higher than the water-entry pressure (WEP) of the soil, then water immediately penetrates into the soil. In contrast, water permeation is delayed when the WP is lower than the WEP of the soil. The time for water infiltration into the soil is an important factor in estimating the hydrological consequences of rain , and the time is mainly affected by the degree of water repellency of the soil  and WP . However, the effects of water repellency and WP on the time required for water infiltration are not yet fully understood.
Figure 6 presents the variation of WIT and infiltration rate of tested materials with various CO and the WP values under similar porosities (n ≈ 0.5). As the WP increases from 10 kPa to 30 kPa, the WIT of the untreated clay slightly decreases from ~39 min to ~27 min. The WIT of the CO = 1% sample is similar to that of untreated clay. Note that the CO = 1% sample shows a very high WIT value (>2 months) at WP of 5 kPa, although the data is not included in Figure 6a. In contrast, the WITs of the other treated clays are dramatically altered with changes in WP. The WITs of the treated clays with CO = 2.5%, 5%, and 10% under WP = 10 kPa are 22,437 min, 26,888 min, and 7174 min, respectively. However, as the WP increases, the WIT of the CO = 2.5% sample decreases and converges with the WIT of untreated clay, whereas the WITs of the CO = 5% and 10% samples significantly decrease below the WIT of untreated clay.
The variation of the infiltration rate according to the applied WP can be seen in Figure 6b. The untreated clay shows an almost constant infiltration rate (4.44 × 10−6–6.28 × 10−6 cm/s), regardless of WP. The infiltration rate of the CO = 1% specimen at 10 kPa is slightly higher than that of the untreated clay, and then it gradually reaches the level of the untreated soil. The CO = 2.5%, 5%, and 10% specimens under 10 kPa pressure have a lower infiltration rate than that of untreated clay. As applied WP increases, the infiltration rates of these specimens tend to increase. The infiltration rate of the CO = 2.5% specimen gradually approaches the infiltration rate of untreated clay, whereas the infiltration rates of the CO = 5% and 10% specimens are higher than that of the untreated specimen at high WP.
The results of WIT and infiltration rate in Figure 6 are significantly related to the wetting patterns. Note that the wetting patterns of soil can be divided into two types: stable and unstable flows. When a soil is wettable, as is the case with untreated clay, a stable flow is observed with a uniform wetting front. Therefore, the wettable soil shows a high degree of saturation (S). In contrast, when a soil is non-wettable, as is the case with treated clays, an unstable flow is observed with an irregular and finger-like wetting front [48,49]. Therefore, the S value of non-wettable soil is low. Because the wetting front of tested specimens cannot be observed during WIT experiments, the S values of a disassembled specimen are employed as an indicator of the wetting patterns of the tested materials in this study.
Figure 7a,b shows representative pictures of disassembled specimens and their S values, respectively. Note that the CO = 2.5% specimen at 10 kPa was extracted by excavating because it was difficult to maintain its original shape during sample extraction from the cell. The experimental results indicate that a specimen with uniform wetting exhibits a high S (>95%), whereas a specimen with irregular wetting exhibits a low S (<77%). The treated clays can be divided into two types according to the variation of S with WP: (1) increasing S with an increasing applied WP (Type-I, such as in the CO = 2.5% specimen); and (2) decreasing S with an increasing applied WP (Type-II, such as in the CO = 5% and 10% specimens). It is reasonable to infer that the effect of water repellency on infiltration vanishes for Type-I soil when the WP exceeds WEP as reflected in very high S values in Figure 7. Thus, the WIT and infiltration rate of the specimen with CO = 2.5% approach to those of untreated kaolin (Figure 6). However, for Type-II soil, it seems that the water-repellent effect is not vanished even though the WP exceeds WEP. The low S values and the disassembled specimens in dry conditions (Figure 7) reflect the formation of finger-like unstable flow for Type-II soil when the WP exceeds WEP. In other words, the preferential flow pathways are formed for Type-II soil, so that the tested specimens with CO = 5% and 10% show very low S values due to the limited saturation along the flow pathways. Because water can flow easily through the preferential flow pathways, the infiltration rate of water-repellent soils can be greater than that of wettable (or untreated) soil, in case finger-like flows are formed . Thus, the specimens with CO = 5% and 10% show a lower WIT or higher infiltration rate than those of untreated kaolin (Figure 6).
The compaction curves (dotted lines) of the untreated and treated clays with zero air void (ZAV) curves (solid lines) are plotted in Figure 8a. The compaction curves of the treated soils are located below the compaction curve of untreated soil. This may be related to the combined effects of decreases both in Gs and in the degree of saturation of the water-repellent soils. The Gs reduction by organosilane treatment (Figure 4a) would induce a decrease in dry unit weight at a given porosity. The compaction curve of untreated clay approached the ZAV curve as the water content increased because the clay can be fully saturated . On the other hand, the treated clays show a significant gap between their compaction curves and ZAV curves even though the specimens have a high water content, reflecting that it is hard to achieve full saturation of treated clays during compaction.
The γd(max) and θopt are calculated from the compaction curve, and plotted as a function of CO in Figure 8b. Note that the mass-based water content is typically considered the optimal water content because of the ease of application in the construction field. However, since the mass-based water content is affected by the Gs of soil, the θopt is adopted to eliminate the effect of the different Gs values of treated clays on mass-based water content. As the CO increases, the γd(max) exponentially decreases, whereas the Gs of the treated sample almost linearly decreases (Figure 4), and the θopt decreases in an approximately linear manner.
To estimate the effect of the organosilane treatment on the compaction, the porosity at γd(max) (nopt), as shown in Figure 8c, is computed by using the Gs and the γd(max) (i.e., nopt = 1 − (γd(max)/(Gsγw))). Note that, if the organosilane treatment does not affect compaction of soil, the nopt of the treated samples will be theoretically the same as that of the untreated. The nopt increases with increasing CO until CO = 2.5%, and then it decreases with a further increase in CO. Additionally, all of the nopt values for the treated samples are higher than that of the untreated sample. This observation reflects that the organosilane treatment disrupts to achieve a dense state of specimen during the compaction test.
The relation between the nopt and the CO is presumably related to the combined effect of water repellency and friction resistance of particle contact. During the compaction test, water acts as a lubricant by developing water films around particles . However, for the treated samples, the water repellency will disrupt the development of water films around particles and induce a consequently high nopt. Since the measured contact angle tend to increase with increasing CO until CO = 2.5%, and then remain almost constant (Figure 5), the resulting nopt will increase as CO increases to 2.5%. In contrast, the friction resistance of particle contact will be decreased with an increase in CO [19,52], and the reduction in the friction resistance will promote achievement of a lower nopt with increasing CO. Therefore, for CO ≥ 2.5%, the nopt decreases with increasing CO.
In summary, the compaction characteristics of treated clays are considerably different from those of untreated clay in terms of water repellency, Gs of the soil, and friction of particle contact. Those factors consequently induce a low value of γd(max). Based on the compaction test results, water-repellent clay has some advantages as a cap material for landfill because of its light weight.
To evaluate the compressibility characteristics of the treated clays, a one-dimensional oedometer experiment was conducted. As shown in Figure 9a, all stress-strain curves of the treated clays are located slightly above the stress-strain curve of untreated clay. The treated clays (CO = 1%, 2.5%, and 5%) have almost the same stress-strain curves, whereas the CO = 10% specimen shows lower settlement than the others. Note that the initial porosities of the dry tested specimens, which were compacted with the same compaction energy, decrease with increasing CO, because organosilane grafting onto the soil surface encourages a dense packing of soil [19,52,53]. Hence, the compressibility characteristic (constrained modulus (M)) of the tested specimen is plotted with the initial porosity at each loading step (ni) (Figure 9b). Note that M (= dσ’v/dεv) is the slope of a compression curve where the x-axis is vertical strain (εv) and the y-axis is vertical effective stress (σ’v). Figure 9b shows the M values of the tested specimens with varying initial porosities under three different σ’v values. It can be observed in Figure 9b that, with an increase in applied σ’v, the M is increased due to the non-linear stress-strain behavior of soils (Figure 9a). Additionally, Figure 9b demonstrates that, under the same σ’v, the M value tends to increase with a decrease in porosity. Most notably, consistent with the previous studies [54,55], the M values of the tested materials can be a single function of the initial porosity (Figure 9b). These results imply that the effect of organosilane treatment on the compressibility is insignificant.
Figure 10 presents the relation between Gmax and vertical effective stress. Since the densities of each specimen were different, the shear modulus at small strain (Gmax) is used, instead of the shear wave velocity (Vs), to explore the effects of organosilane treatment on small strain properties. Note that the Gmax depends on the stiffness of inter-particle contacts and the inter-particle coordination, and it can be expressed as follows:
where ρ is mass density, Λ and ξ are experimentally determined factors. Λ is the value of the Gmax at 1 kPa, and ξ is the stress sensitivity of Gmax with . Generally, stiffer materials show greater Λ, but smaller ξ . As shown in Figure 10a, Gmax increases with increasing CO, although the Gmax of the CO = 5% sample at 625 kPa is slightly higher than the Gmax of the CO = 10% sample. Λ and ξ are plotted with CO in Figure 10b. It can be observed that the Λ factor increases with CO, whereas the ξ exponent decreases with an increase in CO, reflecting an increase in the stiffness of tested soils. Note that the initial porosity of the tested specimens decreases with an increase in CO; therefore, the tested materials with high CO will have higher inter-particle coordination (or better contacts between particles). This results in an increased Gmax of tested materials with an increase in CO.
To isolate/minimize the effect of the changed inter-particle coordination (or porosity) due to the grafting of organosilane on Gmax of tested soils, an untreated clay specimen was subjected to high compaction energy to achieve the same initial porosities of the treated clays (CO = 2.5% and 5% specimens). The filled and open rectangular symbols in Figure 10b indicate the Λ factor and the ξ exponent of the untreated clay, respectively. Although the initial porosity of the untreated clay is the same as that of the treated clay, the untreated clay shows lower Λ factor and ξ exponent values than the treated clay, and the difference between the untreated clay and the treated clay increases with CO. This reflects that the organosilane treatment enhances the stiffness (Gmax) of tested kaolin at a given porosity. Because the comparison of Gmax under the same porosity may guarantee very similar inter-particle coordination, this increased Gmax with an increase in CO may be attributed to the increased inter-particle contact stiffness. In other words, at small strain level, the contacts between kaolin and organosilane, or between organosilane and organosilane, could be stiffer than those between kaolin and kaolin.
In this study, the hydraulic and mechanical characteristics of chemically-treated water-repellent clay are investigated to explore its usefulness as an alternative landfill cover material. A series of laboratory experiments was conducted to measure Gs, TOC, soil-water contact angle, WIT, infiltration rate, compaction characteristics, compressibility, and small-strain shear modulus. The results of this study demonstrate the following:
This research was supported by a grant (16-RDRP-B076564-03) from Regional Development Research Program funded by Ministry of Land, Infrastructure and Transport of the Korean government and by the National Research Foundation of Korea (NRF) grant funded by the Korean government (MSIP) (NRF-2015R1A2A2A01006337).
Tae Sup Yun, Changho Lee, and Woojin Lee conceived and designed the experiments; Youngmin Choi performed the experiments; Youngmin Choi, Hyunwook Choo, and Changho Lee analyzed the results; All of the authors contributed to the discussions; Youngmin Choi and Woojin Lee wrote the manuscript.
The authors declare no conflict of interest.