3.1. IOT Samples Characterization and Analysis
In this item, the results of the sample characterization test.
Figure 3 shows the granulometric curves of the IOT sediment samples from Mariana (MA sample), Rio Doce (RD Sample), and Barra Longa (BL Sample).
Through the curves obtained, it is possible to observe that both samples have sandy characteristics with an insignificant portion of clay. According to Figueiredo et al. [
28], this fact is associated with the composition of the tailings from the Fundão Dam, which was a mixture of sandy tailings and mud. The diameters varied between 1 and 200 μm, with greater predominance in a range close to 15 μm and 100 μm. Such values are consistent with those obtained in other works of characterization of the tailings from the rupture of the Fundão dam carried out by other authors [
24,
25,
28].
Figure 4 shows the isotherm curves of the sedimented tailings samples, obtained by the analysis of nitrogen adsorption and desorption. According to other works found in the literature, the isotherms obtained have a type II profile. According to IUPAC (International Union of Pure and Applied Chemistry), these curves are characteristics of non-porous or macroporous materials [
64].
It is possible to see the presence of narrow and inclined hysteresis, classified as H3 type, indicative of non-rigid aggregates of lamellar particles, mainly mesopores/macropores in the form of slits or parallel plates [
65,
66].
Table 2 presents the specific surface area and porosimetry and it is possible to observe all the samples are similar regarding the pore volume and diameter values. As expected for this type of sample, the specific surface area values were low and similar. Such results are compatible with other studies carried out with ore tailings. Almeida et al. [
25] found specific surface area (SSA), and silt and clay size values, of 5.25, 5.66 and 20.77 m2 g−1, respectively.
Table 3 shows the results obtained in the specific mass, unit mass, void index and water absorption tests. Comparing the specific mass values found with the other results [
67,
68] it is possible to attest that they are compatible with silica-rich tailings with lower concentrations of iron due to the density closest to sand, which is 2.65 g/cm3. These results are consistent with those found in the mineralogical analysis, which showed quartz as the most present mineral in the samples, directly interfering with the specific mass results. The values obtained for the void ratio were similar. Relating to the characteristic granulometry of iron ore tailings, which presents a high concentration of particles of the same size, representing a uniform granulometric curve, a relatively high void volume index might be expected.
The values obtained in the water absorption test showed that the tailings from Mariana (MA sample) and Rio Doce (RD sample) have a low rate of water absorption, which is expected for tailings composed mainly of silica. The Barra Longa tailings (BL sample) showed a higher water absorption rate than the other samples, which may be related to clay minerals in the sample. Additionally, the BL sample showed a lower value of specific mass, which attests to the higher presence of clay minerals in the sample. According to Taiz et al. [
69], clayey soils retain a higher water content than sandy soils due to the larger surface area and smaller pores between particles. This statement can be confirmed by the specific surface area results obtained and shown in
Table 2.
Table 4 presents the results obtained from the XRF analyses. The oxides found in the samples match the mineralogical phases obtained by XRD. Furthermore, among the oxides found in the sedimentary tailings samples, the highest concentrations are quartz (SiO
2) and hematite (ɑ-Fe
2O
3). According to other authors [
29,
70], quartz and hematite are the main mineral components of tailings from the Fundão dam. Traces of manganese oxide, zinc, chromium, and sodium were also found.
Due to the possibility of contamination of these samples in the environment, since the rivers Gualaxo do Norte, Carmo, and Doce have been used, over the decades, for gold mining during the colonial period in Brazil, assays for the determination of inorganic constituents in the raw material, in addition to analysis of the leached and solubilized extracts are shown to be extremely important. The possibility of contamination was raised at the time of the accident [
8,
24,
71] but after five years, the pollutant load of these rivers may have been concentrated or dispersed, which may have impacted on the composition of these sediments.
Through the data obtained by the tests of determination of heavy metals in raw material and obtaining of leached and solubilized extracts, it was observed that the leaching and solubilization tests of metals (inorganic) presented results with values below the maximum limits prescribed by NBR 10004 standard [
48]. The leaching and solubilization tests of volatile and semi-volatile organics showed null results, i.e., below the detection limits of the technique adopted and below the maximum limits prescribed by NBR 10004 [
48]. Because of that, the data indicates that all the collected sediment tailings samples can be classified as Class II B - Non-Hazardous Inert [
48].
The X-ray diffractograms obtained from the sedimented tailings samples can be seen in
Figure 5. It was possible to observe the great similarity between the diffractograms of the analysed samples, with a predominant presence of Quartz phases, SiO2 (ICDD - 46-1045); Hematite, α - Fe
2O
3 (ICDD - 33-664); Goethite, α - FeO(OH) (ICDD - 74-2195); and Kaolinite, Al
2Si2O
5(OH)
4 (ICDD - 80-885). Although the intensity of the peaks of each mineral does not represent the amount, it can indicate which mineral is more present in the sample.
This result is consistent with those found in the literature [
25,
29,
67,
72,
73,
74] confirming the results obtained in the X-ray Fluorescence analysis. XRD analysis also allows to evaluate the amorphicity of the samples, which would make this material suitable for use as a pozzolanic mineral addition, which would increase the durability of cementitious matrices [
75] or as a precursor in alkali-activated materials [
19,
22,
76]. A crystalline material, as shown in the sedimented tailings samples, however, may have its reactivity improved through grinding and calcination [
77,
78,
79] depending on its use.
The images obtained through scanning electron microscopy (SEM) analysis may be seen in
Figure 6. Through the images, it was possible to observe that the particle size is compatible with the results obtained by laser granulometry, with a maximum diameter close to 200 μm. These results agree with other researchers [
24,
25] who found these same characteristics for sedimented tailings from the Fundão dam failure.
It is also possible to identify the presence of prismatic particles with sharp edges, presenting edges and vertices, and the presence of tabular and granular particles. According to Shettima et al. [
12] and Zhao et al. [
80], the particles of the first type may be associated with quartz particles. Particles of the second type may indicate the presence of hematite particles [
72,
75] According to Dedavid et al. [
81], the contrast of the images is related to the atomic number of the elements present in the sample. Thus, through the images obtained, it can be affirmed that quartz particles have larger granulometry when compared to ferrous mineral particles.
In the picture generated for the samples from Rio Doce and Mariana, it is possible to observe particles with rough and angular surfaces, which is expected for a material obtained during mineral processing, with comminution steps [
28]. In BL sample, it was possible to perceive a smaller number of particles of ferrous minerals represented by the light gray color. This can also be seen with the help of EDS images. It also shows predominantly dark-colored particles characteristic of quartz.
In general, the sedimented tailings samples were similar. Traditionally, however, Brazilian IOT, collected in dams, still has a high amount of iron [
72,
75] due to the still inefficient extraction processes practiced 30-40 years ago.
Through the characterization, it can be observed that this material, when exposed to the weather, underwent significant changes over time. Even so, it is a material stored for future use, as its permanence in the places where it is found changes the landscapes, the soil, and the waters, as reported by Brazilian researchers in post-accident publications [
8,
29,
30,
70,
82].
3.2. Soil-IOT Compatibility to Produce RE
Table 5 shows the soil samples characteristics. It was found that the clay contents and sand were quite different, with soil with a high clay content and fine particles. In this way, the need to correct the soil with the IOT-S became even more evident.
As it was carried out before the launch of the Brazilian rammed earth standard [
53] the results of the physical characterization of the soil were based on the parameters of the soil-cement standards and adobe, as well as recommendations from scientific literature, which determine values between 35% and 45% for the liquidity limit and between 7% and 30% for the plasticity index [
83]. In this sense, the results demonstrate that the soil analysis could benefit from stabilization since its value for the liquidity limit exceeds the recommendation.
The results of the compressive strength test are presented in
Table 6. From the values obtained, it is possible to infer that the addition of 5% cement to the soil and the stabilization with IOT proved to be adequate in comparison to the reference values (T0-0), which do not have the addition of any component. For the mixtures without the addition of cement, only with IOT, it was observed that the compressive strength values increase as there is an increase in the replacement of soil by sedimented tailing, in proportions of 10%, 20%, and 40%.
Regarding the compressive strength values found in the literature, it is important to say that the reference trace (T0-0), only with unstabilized soil, is outside the parameters of what is considered satisfactory for rammed earth, while the values of samples stabilized with IOT are within the recommended range. The adopted values range from 1.0 MPa to 2.0 MPa [
61,
84] for the compressive strength of rammed earth and earth constructions. In other research [
85] the results were between 1.0 and 2.5 MPa, consistent with the present study.
With the addition of cement, Eusébio [
86] used a content of 7% of the stabilizing material and obtained compressive strength greater than 2.0 MPa. Jayasinghe & Kamaladasa [
87] analyzed the compressive strength of rammed earth walls stabilized with cement contents in the range of 6.8 and 10% and observed that the stabilizing action of cement is more effective for sandy soils. However, they still obtained high resistance values for clayey soils.
It is important to point out that the highest values were for the mix with the highest amount of IOT (T40-0), which reached 1.80 MPa, followed by the mix with IOT and cement (T40-5). Because of that, there is a tendency to adequately stabilize with only IOT, without the addition of cement, which has been more effective, especially at higher levels of IOT addition (40%).
Finally, the Peruvian technical standard E.080 [
88] and the NZS 4297 standard [
89] present values of 1.0 MPa and 0.50 MPa, respectively, for compressive strength. In other words, the results found in this research are superior to the recommendations, including the Brazilian standard [
53] even though this study was developed before its launch.
The study showed a positive interaction between the soil, collected at MRBH, and the IOT collected in the Mariana region. This is probably due to the rocky origin common to both materials. The advantages can be seen, especially concerning the compressive strength of the rammed earth stabilized with IOT, without cement, compared to the rammed earth cylindrical specimens without any stabilization.