António José Roque1, Paula F da Silva2, Rui Pedro Marques de Almeida1. 1. Laboratório Nacional de Engenharia Civil, Av. do Brasil, 101, 1700-066 Lisbon, Portugal. 2. GeoBioTec Research Centre & Departamento de Ciências da Terra, Faculdade de Ciências e Tecnologia, Universidade NOVA de Lisboa, 2829-516 Caparica, Portugal.
In 2015, the United Nations (UN) adopted the 2030 Agenda for Sustainable Development. One of the goals within the plan is Goal 11: “Make cities inclusive, safe, resilient and sustainable”, which states that half of humanity—3.5 billion people—lives in cities today and 5 billion people are projected to live in cities by 2030 [1]. Considering that cities already account for between 60 and 80% of energy consumption and generate as much as 70% of human-induced greenhouse gas emissions, a sustainable urbanization is central to the realization of the UN Sustainable Development Goals [2]. The current Coronavirus pandemic crisis further highlights the urgent need to address the environmental challenges, benefiting not only the environment, but also our society’s health and well-being [3]. A large majority of our society has finally realized that neither the pandemic nor destructive climate change are a natural disaster; they are, largely, the result of our behaviours and actions.It is known that the construction industry is one of the sectors that generates more waste in the world, both in volume and in weight [4, 5]. According to Kaza et al. [6], the world average generation of construction and demolition waste (CDW), is 1.68 kg/capita/day, which means a world production of about 4.8 billion Mg/year, which is more than the 3 billion Mg/year estimated by Akhtar and Sarmah [7]. In the European Union (EU-27), for example, in 2018, CDW accounts for 36% of all waste generated, which means about 834 million Mg [8]. On the other hand, construction industry consumes 40% of the materials entering the global economy [9, 10], which in Europe means consuming 12 to 18 million Mg/year of new construction materials [11]. Therefore, it is natural the general concern with, not only, reducing the quantity of CDW removed to landfills, the carbon footprint and the energy consumption in this industry, but also with the availability of natural aggregates and where to find, in the future, new aggregate sources [12], in particularly, regarding sands [13]. This framework has highlighted the need to find alternative materials.It is in this context, and with the prospect of economic recovery after COVID-19, that the construction industry will have to accelerate the transition to a greener and more sustainable economy, as exemplified by the joint declaration of the EU and China on September 14, 2020 [14].Concrete waste, which represents the largest percentage of CDW in many countries, and was estimated at 67% in the United States of America (USA) by Akhtar and Sarmah [7], and steel slag (SS), a by-product of steel and iron production, whose world production in 2018 reached about 600 million Mg [15], are, probably, ideal materials to replace natural crushed aggregates, given their fast production, high cost-efficiency of production in comparison to generating natural aggregates, great financial savings due to the elimination of the need to send them to landfill, as well as, their engineering and environmental properties that make them potentially suitable for applications in civil engineering, and particularly, in geotechnics.Both recycled concrete aggregates (RCA) and recycled steel slag aggregates (RSSA) have been used in construction since the early 1980s; mainly in the construction of unbound granular layers of road pavements (RCA: [16-22]; RSSA: [23-29]). Nevertheless, there are several studies (RCA: [21, 27–35]; RSSA: [27–29, 35]), who report the possibility of this recycling contributing to the reduction of the drainage capacity of the unbound granular layers, as well as the drainage structures (e.g., subdrains, catch basins and spillways) that may be associated with them [27]. The main cause for this may be the formation of tufa, a precipitate of insoluble calcium carbonate, and the recementation of cementitious materials that are not completely hydrated. Due to this behaviour, their use is not recommended, or it is even forbidden, in some states of the USA [36, 37]. However, there are also some studies concluding that tufa formation and recementation are not significant, especially if the percentage of fines is limited to a small percentage [19, 31, 32, 38, 39].Given the restrictions, or even prohibitions, on the use of RCA and RSSA in unbound granular layers of road pavements, very few studies have been carried out to assess their behaviour as drainage materials [16, 19, 32, 38], which has limited their recycling in drainage structures of geotechnical works (e.g., rainwater drainage layer in landfills, vertical sand drains, and back drainage of earth retaining walls) and road pavements (e.g., longitudinal edge drains, transverse and horizontal drains, permeable bases, and underdrains/deep drains).In this context, and considering that Freire et al. [40] and Gomes Correia et al. [41] showed that the two recycled aggregates selected for the study presented in this paper, respectively RCA and RSSA, do not release hazardous substances for public health and the environment, and have physical and mechanical properties that allow their recycling in unbound granular layers of road pavements and earth fills, it was considered opportune to assess their drainage capacity with the aim to use them in drainage structures of geotechnical works and road pavements. In addition to evaluating their drainage capacity to tap water, their behaviour to a leachate collected in a municipal solid waste (MSW) landfill, acidified in laboratory from pH 8.2 to 5.5, was also studied. To the authors’ best knowledge, the study of the performance of these recycled aggregates in contact with MSW landfill leachate has not yet been developed. Therefore, another important objective of this study was to assess the feasibility of using these recycled aggregates in the construction of the leachate collection and removal layer (LCRL) of the MSW landfills.The drainage capacity of RCA and RSSA to water and MSW landfill leachate was compared with that of two natural aggregates, a basalt, and a limestone. Despite studies carried out by Niemann and Hatheway [42] and Bennett et al. [43] concluded that typical landfill leachates would not dissolve significant amounts of carbonate minerals and their use is allowed in some countries, e.g., by the United Kingdom Environmental Agency [44], it continues to be forbidden in others, e.g., by the Portuguese Environment Agency [45] and South Australia Environment Protection Authority [46], or to be limited to a certain percentage, e.g., less than 8.5% in total weight by the Western Australian Environmental Protection Authority [47]. Although hard evidence that carbonate materials are truly unsuitable is lacking [48], there is a surprising paucity of research concerning the suitability of carbonate aggregate as drainage stone. Therefore, another goal of this study was to evaluate the drainage capacity of the limestone aggregate in contact with the acidified MSW landfill leachate.The study of the durability of these four aggregates in contact with tap water and the acidified MSW landfill leachate carried out by Roque et al. [49], showed that all of them belong to the “very high” durability class of the classification of Gamble [50].
Materials
Recycled and natural aggregates
The recycled aggregates studied coming from CDW and electric arc furnace SS. The CDW were produced by the Demotri company, of the Ambigroup Group, and their processing in a mobile recycling plant has produced the RCA used in this study. The SS are produced by the two iron and steel plants that exist in Portugal. Together, both plants generate around 250 thousand Mg of SS per year. The recycled aggregate that comes from SS processing is traded under the name Inert Steel Aggregate for Construction (ISAC). Figure 1 shows the RCA and ISAC sampling sites.
Fig. 1
Location of studied materials
Location of studied materialsThe selected natural aggregates were collected in a basalt quarry (BAS), exploited by the Alves Ribeiro company, and a limestone quarry (LIM), belonging to the Agrepor company. The locations of both quarries are also indicated in Fig. 1.The sampling of recycled and natural aggregates was carried out taking into account, on one hand, the dimensions which they were produced with, and, on the other hand, the required grain-size distributions for carrying out the study. For the RCA, concrete blocks with dimension less than 100 mm were sampled. At the laboratory, these blocks were crushed and sieved to produce the following grain-size fractions: 0.25/0.5 mm, 0.5/1 mm, 1/2 mm, 2/4 mm, 4/12.5 mm, 12.5/16 mm and 16/20 mm (Fig. 2). ISAC was collected in grain-size fractions of 0/6 mm and 0/40 mm (Fig. 2). For the BAS, five grain-size fractions were sampled, as follows: 0/4 mm, 4/12 mm, 10/16 mm and 12/20 mm (Fig. 2). LIM was collected in two grain-size fractions: 0/4 mm and 0/32 mm (Fig. 2).
Fig. 2
Grain-size fractions of recycled (RCA; ISAC) and natural (BAS; LIM) aggregates used in the preparation of specimens (scale ruler in cm)
Grain-size fractions of recycled (RCA; ISAC) and natural (BAS; LIM) aggregates used in the preparation of specimens (scale ruler in cm)Samples of the four aggregates were transported to the laboratory in nylon bags and stored at room temperature until the correspondent specimens were prepared to carry out the permeability tests.According to the macroscopic description of the four aggregates presented in Roque et al. [49], RCA is a heterogeneous and multiphase material, composed by natural aggregates of coarse-grained and fine-grained sizes, surrounded by a cementitious matrix, which is porous (presence of some pore ≤ 3 mm, dispersed heterogeneously) and light grey in colour; ISAC is a dense material, which presents a vesicular texture, a rough surface, small iron particles and has a black colour; BAS is a compact and melanocratic rock, with aphanitic texture; and LIM is a compact oolithic rock, yellowish to white in colour and contains veins and spherical nodules of calcite. The detailed description of the microscope examination of the four aggregates can be found by Roque et al. [49].The density (bulk density—ρ, and real density—ρ), porosity accessible to water (P) and maximum water absorption under vacuum conditions (w) of recycled aggregates (RCA and ISAC) and natural aggregates (BAS and LIM), obtained by Roque et al. [49], are shown in Table 1. According to Roque et al. [49], RCA is the least dense, the most porous and with the highest water absorption capacity, ISAC is the densest, BAS is the least porous and with the lowest water absorption capacity and LIM presents intermediate results compared to the other three aggregates.
Table 1
Physical properties of the recycled and natural aggregates (adapted from [49])
Material
ρb(Mg/m3)
ρr(Mg/m3)
Pe(%)
wmax(%)
RCA
ISAC
BAS
LIM
2.58
3.77
3.02
2.72
2.14
3.28
3.00
2.58
16.88
12.40
0.45
5.40
7.89
3.83
0.14
2.20
ρ bulk density, ρ real density, P porosity accessible to water, w maximum water absorption under vacuum conditions
Physical properties of the recycled and natural aggregates (adapted from [49])RCAISACBASLIM2.583.773.022.722.143.283.002.5816.8812.400.455.407.893.830.142.20ρ bulk density, ρ real density, P porosity accessible to water, w maximum water absorption under vacuum conditionsThe main chemical elements of the recycled aggregates, for which it was assessed the feasibility of their use in drainage structures of geotechnical works and road pavements, are included in Table 2.
Table 2
Main chemical elements of the recycled aggregates
Chemical element
RCA (%)
ISAC (%)
Aluminium oxide (Al2O3)
Calcium oxide (CaO)
Iron oxide (Fe2O3)
Magnesium oxide (MgO)
Phosphorus oxide (P2O5)
Silicon oxide (SiO2)
Sulphur oxide (SO3)
1.2
54.2
0.7
0.2
0.03
2.3
0.5
5.8
35.2
30.4
4.4
0.7
15.7
0.7
Main chemical elements of the recycled aggregatesAluminium oxide (Al2O3)Calcium oxide (CaO)Iron oxide (Fe2O3)Magnesium oxide (MgO)Phosphorus oxide (P2O5)Silicon oxide (SiO2)Sulphur oxide (SO3)1.254.20.70.20.032.30.55.835.230.44.40.715.70.7
Aqueous solutions
The aqueous solutions selected for the experimental program were water (W) from the Lisbon public supply network and a leachate (L) from a MSW landfill, operated by the Amarsul Company (AdP Group). Figure 1 shows the MSW landfill location and Table 3 presents the main chemical components of the leachate. Until the performance of the permeability tests, the L was stored in a cold room, at a temperature of about 4 °C.
Table 3
Main chemical elements of the MSW landfill leachate
Chemical element
Unit
Value
pH
Electric conductivity
Ammoniacal nitrogen
Total nitrogen
Biochemical oxygen demand (BOD)
Chemical oxygen demand (COD)
Total organic carbon (TOC)
Phenols
Total phosphorus
Bicarbonate (HCO3−)
Chloride (Cl−)
Fluoride (F−)
Nitrate (NO3−)
Nitrite (NO2−)
Sulphate (SO42−)
Sulphide (S2−)
Aluminium (Al)
Calcium (Ca)
Iron (Fe)
Magnesium (Mg)
Potassium (K)
Sodium (Na)
–
mS/cm
g/l
g/l
g/l
g/l
g/l
mg/l
mg/l
g/l
g/l
mg/l
mg/l
mg/l
mg/l
mg/l
mg/l
mg/l
mg/l
mg/l
g/l
g/l
8.2
34.6
4.6
3.6
1.6
10.0
1.86
0.96
44.0
21.0
4.9
1.5
< 5.0
< 0.015
360.0
6.4
2.28
34.0
7.0
43.0
3.13
3.1
Main chemical elements of the MSW landfill leachatepHElectric conductivityAmmoniacal nitrogenTotal nitrogenBiochemical oxygen demand (BOD)Chemical oxygen demand (COD)Total organic carbon (TOC)PhenolsTotal phosphorusBicarbonate (HCO3−)Chloride (Cl−)Fluoride (F−)Nitrate (NO3−)Nitrite (NO2−)Sulphate (SO42−)Sulphide (S2−)Aluminium (Al)Calcium (Ca)Iron (Fe)Magnesium (Mg)Potassium (K)Sodium (Na)–mS/cmg/lg/lg/lg/lg/lmg/lmg/lg/lg/lmg/lmg/lmg/lmg/lmg/lmg/lmg/lmg/lmg/lg/lg/l8.234.64.63.61.610.01.860.9644.021.04.91.5< 5.0< 0.015360.06.42.2834.07.043.03.133.1
Methods
Preparation of recycled and natural aggregates
From the grain-size fractions of each aggregate two mixtures were produced. One in the grain-size range of sand (0.25–2 mm) and the other in the grain-size range of fine gravel (2–20 mm). The plots of the gradation curves and the corresponding percentages of the different grain-size fractions for sand and fine gravel mixtures are shown in Fig. 3. These gradation curves are representative of the gradation curves used in the LCRL of the Portuguese MSW landfills. The maximum grain-size used was 20 mm to ensure a ratio of about 5 with the diameter of the column used in the permeability tests. According to the Unified Soil Classification System [51], the sand aggregates correspond to a SP poorly graded sand, and the fine gravel aggregates to a GP poorly graded gravel.
Fig. 3
Grain-size distribution curves of sand and fine gravel used in the preparation of specimens
Grain-size distribution curves of sand and fine gravel used in the preparation of specimensThe selection of these two grain-size ranges (sand and fine gravel) also allowed to evaluate the influence of the grain-size on the hydraulic performance of the aggregates, in particular of the two recycled aggregates, which has been evaluated in other works [12, 19, 30–32].
Specimen preparation
The sand and fine gravel aggregates used in the preparation of the specimens to be used in the permeability tests were dried in an oven at 60 °C, before being poured into a polyvinyl chloride (PVC) column, with the aid of a spoon. The dimensions of the column are, 9 cm in inner diameter and 25 cm in height, which correspond to the dimensions of the tested specimens. The filling of the column with the aggregates was accompanied by blows with a wooden mallet, applied to the upper ring of the wooden structure that supported the column. This procedure is intended to promote the rearrangement of the aggregates’ particles and the densification of their particulate medium. After the column filling was completed, the assemblage of aggregate and column was weighed, and the dry weight of added aggregate was recorded. For each aggregate, two specimens of sand and two specimens of fine gravel were prepared, in a total of 16 specimens. Figure 4 shows the column tops of the sand and fine gravel specimens obtained for the recycled aggregates RCA and ISAC.
Fig. 4
Top of sand and fine gravel specimens of the recycled aggregates, RCA and ISAC (scale ruler in cm)
Top of sand and fine gravel specimens of the recycled aggregates, RCA and ISAC (scale ruler in cm)Table 4 shows the dry unit weight of the tested specimens. The values varied between 14.9 and 15.2 kN/m3 for RCA, between 21.7 and 24.2 kN/m3 for ISAC, between 17.2 and 19.8 kN/m3 for BAS, and between 17.8 and 18.3 kN/m3 for LIM. The ISAC’s dry unit weight was the highest and that of the RCA the lowest. These results were already expected and are attributed to the iron particles present in the constitution of the ISAC aggregates [25, 52], and the mortar adhered to the RCA aggregates [13, 53, 54].
Table 4
Dry unit weight of the tested specimens
Material
Influent
Dry weight of specimen(g)
Dry unit weight(kN/m3)
RCA
Sand
Water
2363.3
15.1
Leachate
2361.4
14.9
Fine gravel
Water
2349.7
14.9
Leachate
2392.7
15.2
ISAC
Sand
Water
3799.3
24.2
Leachate
3769.8
24.0
Fine gravel
Water
3409.8
21.7
Leachate
3490.6
22.5
BAS
Sand
Water
2693.4
17.2
Leachate
2828.1
18.0
Fine gravel
Water
3079.5
19.6
Leachate
3105.5
19.8
LIM
Sand
Water
2813.0
17.9
Leachate
2805.6
17.8
Fine gravel
Water
2818.6
17.9
Leachate
2874.0
18.3
Volume of specimens: 1539.1 cm3
Dry unit weight of the tested specimensVolume of specimens: 1539.1 cm3
Leachate preparation
The pH of L collected at the MSW landfill was 8.2. To test the aggregates under chemically more aggressive conditions, the collected L was acidified in the laboratory, until reaching a pH value of 5.5. This value for the pH was defined considering the possibility that the pH of MSW landfill leachate can reach values of this order of magnitude during the operation period [55, 56].The acidification of L was achieved by adding 10 ml increments of a 50% hydrochloric acid (HCl) solution. For each litre of MSW landfill leachate, it was necessary to add, on average, about 100 ml of that solution.
Permeability testing
Permeability tests were carried out in a rigid-wall permeameter, at a controlled room temperature of about 20 °C. A constant head permeability test was adopted, as it is more suitable than a variable head permeability test for testing coarse soils or aggregates [38]. At the top and bottom of the specimens, previously prepared in the PVC column, a Perspex porous plate was placed. In the sand specimens, on the porous plate, a nylon net was also placed to minimize the migration of the finest particles. Each set was confined between a cover and a base, also in PVC. Both the cover and the base were equipped with two valves. Figure 5 shows the schematic of the setup used in the laboratory permeability tests to generate data for the experimental analyses for this study.
Fig. 5
Device used in the permeability tests
Device used in the permeability testsThe methodology adopted in the permeability tests intended to approximate the conditions existing in the laboratory to those existing in the MSW landfills, having been defined three distinct test phases. At Phase 1, a minimum volume of about 250 l of W or L percolated through the specimens should be collected. This volume is about three times greater than the volume that would be collected in a LCRL of a MSW landfill, considering an area equivalent to that of the test specimens. For this calculation, it was assumed that the annual production of L in a Portuguese MSW landfill is around 1 m3/m2, and that the operation period, up to closure, is projected for 12–15 years. At Phase 2, the permeameter was removed from the test device showed in Fig. 5, and placed in an oven, at a temperature of 45 °C, for a minimum period of 7 days. The placement of the permeameter in the oven at the temperature of 45 °C aimed to simulate the temperature that can be reached in a MSW landfill [57]. After removing the permeameter from the oven and before restarting the permeability test, it was allowed the necessary time for the specimens to reach room temperature. At this stage, a minimum volume of about 30 l of W or L percolated through the specimens should be collected. At Phase 3, which was limited to the four sand specimens percolated with L, the specimens remained in static contact with L for a minimum of 45 days. This phase aimed to promote the reactions between the sand aggregates and L, and to simulate the periods in which it is not possible to collect L due to the reasons associated with the operating conditions of the MSW landfills. At this last phase, a minimum volume of about 10 l of L percolated through the specimens should be collected.All permeability tests were carried out until the hydraulic conductivity (k) was approximately constant and with a hydraulic head of 0.30 m, which is usually regulated as the maximum height of L above the bottom clay liner of landfills [58, 59]. The permeability tests with this hydraulic head, which correspond to a hydraulic gradient of 2, also contributed to minimize the entrainment of finest particles of the aggregates.During the permeability tests, the effluent pH was monitored. At the end of the tests, the permeameters were drained and the aggregates placed on trays to dry in an oven at a temperature of 60 °C for 24 h. The dry material was weighed and submitted to grain-size distribution tests, according to the specification E 195 [60].
Results and discussion
Hydraulic conductivity of the aggregates
Figure 6 shows, on a semi-log scale, the variation of k as a function of the volume of W or L percolated through the sand and fine gravel specimens of the two recycled aggregates and two natural aggregates. Table 5 presents, for the 16 tested specimens, the values for k obtained at the different test phases (Phase 1: before oven, Phase 2: after oven, Phase 3: after prolonged static contact with L) as well as the total test time and the total volume of effluent collected.
Fig. 6
Hydraulic conductivity of sand and fine gravel aggregates to tap water and MSW landfill leachate: a RCA; b ISAC; c BAS; d LIM
Table 5
Hydraulic conductivity of the recycled and natural aggregates
Material
Influent
Time(day)
Effluent volume(l)
Hydraulic conductivity, k(× 10–4 m/s)
Phase 1(before oven)
Phase 2 (after oven)
Phase 3(after prolonged static contact)
RCA
Sand
Water
42
310
4
3
–
Leachate
73
298
4
3
2
Fine gravel
Water
28
300
25
25
–
Leachate
31
290
13
10
–
ISAC
Sand
Water
41
285
2
0.5
–
Leachate
73
300
4
3
2
Fine gravel
Water
28
310
19
19
–
Leachate
31
290
13
14
–
BAS
Sand
Water
48
315
9
18
–
Leachate
75
305
6
2
2
Fine gravel
Water
28
310
28
28
–
Leachate
31
290
19
17
–
LIM
Sand
Water
46
213
0.5
0.2
–
Leachate
75
308
6
5
3.5
Fine gravel
Water
28
307
17
17
–
Leachate
31
290
11
9
–
Hydraulic conductivity of sand and fine gravel aggregates to tap water and MSW landfill leachate: a RCA; b ISAC; c BAS; d LIMHydraulic conductivity of the recycled and natural aggregatesIn all permeability tests performed with the fine gravel specimens, percolated with W or L, the k value remained approximately constant at Phases 1 and 2. BAS was the most permeable fine gravel aggregate and LIM the least permeable fine gravel aggregate. At the two phases of the test, the following sequences were obtained:- BAS > RCA > ISAC > LIM, with W;- BAS > ISAC > RCA > LIM, with L.In the permeability tests carried out with the sand specimens, the k values obtained did not show the regularity that was observed in the fine gravel specimens.When percolated with W, the most significant variations were registered for BAS (Fig. 6c) and LIM (Fig. 6d) sand specimens. For BAS sand specimen, k value increased from about 140 l of collected effluent. For LIM sand specimen, k value decreased from about 120 l of collected effluent, which became more accentuated after placing the specimen in the oven. For the recycled aggregates, it was only at the beginning of Phase 2 that there was a change in the k value for the ISAC specimen, which decreased from around 2 × 10–4 m/s to about 0.5 × 10–4 m/s. In these tests, the sequence obtained was the same at the two phases, and equal to that obtained in the fine gravel specimens percolated with the same influent (W):- BAS > RCA > ISAC > LIM.In the permeability tests carried out with the sand specimens using L as influent, there was only a relevant change for k value in the BAS specimen, which decreased from around 7 × 10–4 m/s to about 1.5 × 10–4 m/s at the end of Phase 2 (after oven). In this case, the sequences at the three phases of the permeability tests were as follows:- Phase 1: BAS = LIM > ISAC = RCA;- Phase 2: LIM > ISAC = RCA > BAS;- Phase 3: LIM > ISAC = RCA = BAS.Figure 7 compares, also on a semi-log scale, the hydraulic performance of the sand and fine gravel aggregates percolated with W (Fig. 7a) or L (Fig. 7b). The value of k in the fine gravel specimens was always higher than in the sand specimens, consistent with what was expected. It should also be noted that the difference between the values of k obtained in the sand and fine gravel specimens percolated with W was greater than in the specimens percolated with L.
Fig. 7
Hydraulic conductivity of sand and fine gravel of recycled and natural aggregates: a permeated with tap water; b permeated with MSW landfill leachate
Hydraulic conductivity of sand and fine gravel of recycled and natural aggregates: a permeated with tap water; b permeated with MSW landfill leachateFigure 8 shows the influence of the influent, W or L, in the hydraulic performance of the aggregates of sand (Fig. 8a) or fine gravel (Fig. 8b). In sand specimens (Fig. 8a), k values in the permeability tests carried out with L tend to be higher than the ones performed with W. However, in the fine gravel specimens (Fig. 8b), the opposite is observed. It should be noted, additionally, that the extreme values of k in the fine gravel specimens are much closer (between 9 × 10–4 m/s and 28 × 10–4 m/s) than in the sand specimens (between 0.2 × 10–4 m/s and 18 × 10–4 m/s).
Fig. 8
Hydraulic conductivity of recycled and natural aggregates: a sand permeated with tap water and MSW landfill leachate; b fine gravel permeated with tap water and MSW landfill leachate
Hydraulic conductivity of recycled and natural aggregates: a sand permeated with tap water and MSW landfill leachate; b fine gravel permeated with tap water and MSW landfill leachateGiven that k values remained practically constant for the fine gravel recycled aggregates during the permeability tests, neither tufa formation nor recementation phenomena were observed, which can significantly reduce the drainage capacity of structures that incorporate them or that are adjacent to them, according to different studies carried out in the laboratory and in the field. In the tests carried out with the sand recycled aggregates, k values did not remain constant throughout the permeability tests; however, the observed changes are also not attributed to tufa formation or recementation. Indeed, on one hand, variations of k values were more frequent and more accentuated in natural aggregates than in recycled aggregates. On the other hand, the gradation curves of the aggregates obtained at the end of the permeability tests were very similar to the respective reference gradation curves (Fig. 9). If there had been relevant recementation, larger particles would also have formed [39].
Fig. 9
Grain-size distribution curves of sand and fine gravel of recycled (RCA; ISAC) and natural (BAS; LIM) aggregates, before and after permeability tests
Grain-size distribution curves of sand and fine gravel of recycled (RCA; ISAC) and natural (BAS; LIM) aggregates, before and after permeability testsTo maintain the drainage capacity of the unbound layers built with recycled aggregates coming from crushed concrete and SS, the experience acquired, both at the laboratory and in the field, recommends reducing the percentage of fines [19, 30, 32–34, 38] and proper processing [19], namely, the removal of free lime in the SS [28] and the exposure of crushed concrete to atmospheric conditions for an extended period [30, 38].Regarding the behaviour of LIM percolated with L, the variation of k values throughout the permeability tests does not indicate that the carbonate minerals have been dissolved, confirming the results obtained in previous studies [42, 43]. The control of the dry mass of the LIM specimens also allowed to verify that their reduction had very little significance at the end of the permeability tests (between 0.10% and 0.69%), and it was comparable with the loss of mass obtained in the remaining specimens (RCA: 0.24–1.35%; ISAC: 0.07–0.81%; BAS: 0.07–0.50%). These results can be explained by the fact that the natural chemical conditions favourable to the karstification (or chemical dissolution) of limestone and dolomite (CO2 + H2O + CaCO3 ↔ Ca2+ + 2HCO3) do not exist in the LCRL of landfills to promote their dissolution. On the other hand, the time required for the formation of karst areas from the dissolution of carbonates it is much longer than the useful lifetime designed for landfills.
pH monitoring of the effluent
The initial pH value of the influent W, which was around 8.2, increased significantly in the effluents collected in the permeability tests carried out with recycled aggregates. Table 6 shows that effluent pH values between 10.55 and 11.72 were obtained. These high alkalinity values were also mentioned in other studies (RCA: [19, 30, 34, 39, 61]; RSSA: [62]). According to Barca et al. [63], the high alkalinity of RSSA is due to the existence of reactive calcium oxides. In the case of RCA, Nam et al. [19] have considered that is due to the dissolution of calcium, sodium, and potassium hydroxides, which exist in the mortar. During the performance of the permeability test, the pH value of the collected W decreased very slightly in all specimens, with the most accentuated decrease, of 2.2 units, to be verified at the RCA fine gravel. In the remaining specimens, the decrease in pH was between 1.08 and 1.53 units. Similar evolution was also observed in other studies with RCA [31, 32, 34]. Regarding the RSSA, no reference was found to the variation in pH with the volume of effluent collected, in the literature reviewed. In natural aggregates, the pH value of the W collected was much lower than the effluent pH of the recycled aggregates, and it was only slightly higher than the initial pH value of the influent W, except in the case of BAS sand. During the permeability tests, the decrease in effluent pH varied between 0.34 and 1.62 units, being, therefore, less accentuated than in recycled aggregates.
Table 6
pH of the effluent collected in permeability tests
Material
Influent
pH of the effluent
Initial
Final
RCA
Sand
Water (pH = 8.2)
11.72
10.19
Leachate (pH = 5.5)
9.18
6.26
Fine gravel
Water (pH = 8.2)
11.30
9.10
Leachate (pH = 5.5)
8.81
5.64
ISAC
Sand
Water (pH = 8.2)
11.35
10.25
Leachate (pH = 5.5)
9.17
6.88
Fine gravel
Water (pH = 8.2)
10.55
9.47
Leachate (pH = 5.5)
8.57
5.58
BAS
Sand
Water (pH = 8.2)
9.44
7.82
Leachate (pH = 5.5)
6.06
5.32
Fine gravel
Water (pH = 8.2)
8.80
7.91
Leachate (pH = 5.5)
5.86
5.46
LIM
Sand
Water (pH = 8.2)
8.34
7.82
Leachate (pH = 5.5)
6.14
5.54
Fine gravel
Water (pH = 8.2)
8.50
8.16
Leachate (pH = 5.5)
6.20
5.50
pH of the effluent collected in permeability testsFor permeability tests carried out with influent L, where the initial pH was 5.5. Table 6 shows that only the effluent collected in recycled aggregates (RCA and ISAC) showed alkaline characteristics. However, during the permeability tests carried out on these aggregates, the effluent pH decreased until it presented acidic characteristics. In recycled aggregates, the effluent pH decreased between 2.29 and 3.17 units, and in natural aggregates, between 0.40 and 0.74 units.The set of results obtained with recycled aggregates shows that the pH of the effluent is higher in sand aggregates than in fine gravel aggregates, which is consistent with the smaller size of the sand particles and the increase in its specific surface. In natural aggregates, the pH of the effluent is approximately the same in sand and gravel aggregates.
Practical geotechnical applications
The k value typically required for the LCRL landfills is equal to, or greater than, 1 × 10–4 m/s [45, 59, 64]. Figure 7b shows that both sand and fine gravel aggregates percolated with L fulfilled the minimum requirement of k ≥ 1 × 10–4 m/s, although compared to most of the grading envelopes required [65], the grain-size fractions of the tested specimens are finer.Under normal conditions, in all other geotechnical applications and in the drainage layer of the final cover of landfills, the aggregates only contact with W at room temperature. Therefore, the k values obtained at Phase 1 of the permeability tests were taken into account to analyse the technical feasibility of using the tested aggregates, in particular the RCA and ISAC.Considering that the k required for the drainage layer of the final cover of landfills is typically similar to that required for their LCRL, it is noted that both grading fractions for all tested aggregates fulfilled the foreseen requirement. The exception in it is the LIM sand. It is important to re-emphasize that the k values were obtained with finer grading fractions than those usually required, so that the existing specifications will be, in some way, conservative.For drainage layers of road pavements, the required values for k are typically equal to, or greater than, 1 × 10–3 m/s [66, 67]. For these applications, only the fine gravel aggregates have k values with the required order of magnitude. Considering, however, that the nominal grain-sizes usually required [66-69] are larger than those of the tested fine gravel, it can be considered that their empirical designing is conservative for obtaining k ≥ 1 × 10–3 m/s.At the inside face of retaining walls, the material with drainage functions should typically present k > 1 × 10–5 m/s [70] and nominal grain-sizes of 20 mm. In this case, whatever the grading fraction of the tested aggregates, the minimum requirement is fulfilled.For vertical sand drains, no references were found on the values required for k, only grading envelopes, corresponding to clean sands. According to IDOT [71] and IP [72], these materials should have a percentage of fines (≤ 0.075 mm) less than 3% and 6%, respectively. FHWA [73] specified a percentage less than 4% for particles with an equivalent diameter less than or equal to 0.106 mm. The grading characteristics of the tested sand specimens and the obtained k values allow us to consider that the studied sand aggregates are suitable for building vertical sand drains.By the exposed, the presence of fines in aggregates to be applied in drainage structures should be very low, as they increase the possibility of tufa formation, the development of recementation phenomena, and clogging. Considering that RCA is very susceptible to the production of fines during storage, transport, and application [19], its handling should also be guided to minimize them.It should be pointed out, finally, that the two recycled aggregates are potentially corrosive to aluminium or galvanized iron pipes placed in direct contact with them, due to their high alkalinity [62]. In Germany, for example, aggregates applicable to road pavements must have a pH ≤ 10–13 [62]. Despite the high alkalinity of these recycled aggregates, the environmental hazard of the effluents generated from them is unlikely and restricted to a small region near the applied material, due to the usual natural dilution [34].
Conclusions
The results of the study of the drainage capacity of two recycled aggregates and two natural aggregates, percolated with a leachate coming from a municipal solid waste (MSW) landfill (acidified to pH 5.5) and tap water, are presented. The recycled aggregates, a recycled concrete aggregate (RCA) and an inert steel aggregate for construction (ISAC), respectively, coming from the processing of construction and demolition waste (CDW) and electric arc furnace steel slag (SS), and the natural aggregates, respectively, from basalt (BAS) and limestone (LIM) quarries. Considering that the main goal is to promote the use of recycled aggregates in the construction of drainage structures for geotechnical works and road pavements, the analysis of the results focused mainly on the hydraulic performance of recycled aggregates, supported in comparison to the hydraulic performance of natural aggregates.Contrasting to what has been observed in several published studies, there were no decreases in the hydraulic conductivity of the two recycled aggregates (RCA and ISAC), which presented a hydraulic performance similar to that of natural aggregates (BAS and LIM). On the other hand, the maintenance of the drainage capacity of recycled aggregates during the development of permeability tests confirms the conclusions of other studies referenced in this paper. According to those studies, it is important to eliminate, or reduce, the percentage of fines and reactive elements responsible for the formation of tufa and the development of the phenomena of recementation and clogging. It follows that a proper processing and handling of these recycled aggregates are crucial to their adequate hydraulic performance. In the results obtained, there is also no evidence of the inadequacy of the drainage capacity of the limestone aggregate for the construction of leachate collection of removal layer (LCRL) of the MSW landfills, as it is admitted in several countries, due to the possibility of dissolution of carbonate minerals. It was also observed that with finer grading ranges than those required by the regulations, hydraulic conductivity values equal to, or higher than those defined for these were obtained, indicating that the grain-size distributions or grading envelope required, mostly based on empirical principles, could be conservative.Considering the hydraulic performance obtained for the studied recycled aggregates (RCA and ISAC), complemented by the results obtained on their environmental, physical, and mechanical characteristics in previous Portuguese studies, it is concluded that under the laboratory-tested conditions, they will be suitable for the construction of drainage structures of geotechnical works (e.g., LCRL and stormwater drainage layers of landfills, vertical sand drains, and drains at the inside face of retaining walls) and road pavements (e.g., longitudinal edge drains, transverse and horizontal drains, permeable bases, and underdrains/deep drains). The study carried out also allows us to conclude that the LIM aggregate could be used in the construction of LCRL of MSW landfills.The results obtained in this study, by enabling the applicability of recycled concrete aggregates (RCA) and recycled steel slag aggregates (RSSA) in the drainage structures of geotechnical works and road pavements, will contribute to the preservation of natural resources and for the reduction of the disposal of CDW and SS in landfills, that is, for a more sustainable construction.
Authors: James O'Connor; Thi Bang Tuyen Nguyen; Tom Honeyands; Brian Monaghan; Damien O'Dea; Jörg Rinklebe; Ajayan Vinu; Son A Hoang; Gurwinder Singh; M B Kirkham; Nanthi Bolan Journal: J Hazard Mater Date: 2021-06-25 Impact factor: 10.588