3.3. Chemical Composition of Crude Oil-Contaminated Soil and Neutralized Soil
Comparative analysis of the fractional composition of oil components in the crude oil-contaminated soil and the neutralized soil has shown (see
Table 3) that there are practically no low boiling point fractions (C
12–C
17) in the neutralized soil, but the content of high boiling point fractions (C
18–C
23) is significantly increased. This shows that neutralization of the crude oil-contaminated soil by the proposed method reduces its toxicity significantly.
It should alsobenoted that the neutralization of the crude oil-contaminated soil involves an oxidation process whereby low-boiling-point acetylene hydrocarbons are converted to high-boiling-point hydrocarbons—paraffinic and naphthenic hydrocarbons, bitumen, and asphaltenes (
Table 4).
In the neutralization of the crude oil-contaminated soil, the total content of oil components and metals was decreased—the content of oil components was decreased by more than 260 times. The metal content was decreased from 2.4 times (Mo) to 20,000 times (V); the content of highly toxic metals (Pb, Cr, and As) was reduced by 6, 3, and 1500 times, respectively (
Table 5).
Table 6 shows the chemical composition of solid particles for the crude oil-contaminated soil and the neutralized soil. The solid particles of the soil generally consist of silica oxide (SiO
2—50.2%), calcium oxide (CaO—19.4%), and ferrum oxide (Fe
2O
3—15.2%), the total content of which is 84.8% (almost 85%). The rest of solid particles for soil (15.2%) is presented by magnesium oxide (MgO—4.8%), potassium oxide (K
2O—4.1%), aluminum oxide (Al
2O
3—3.1%), sodium oxide (Na
2O—2.1%), and phosphorus oxide (P
2O
5—1.1%). As can be seen from this table, the neutralization process does not practically change the chemical composition of the soil.
3.4. IR-Spectra
The interpretation of the IR-spectra of the investigated soils (
Figure 6) was performed according to [
32,
33,
34]. There were absorption peaks at 1364.9 cm
−1, 1362.1 cm
−1,and 1358.5 cm
−1 in IR-spectra of the crude oil-contaminated soil, the neutralized soil, and the neutralizer, respectively, characterizing the symmetrical deformation vibration of
C–H bond in methyl (
CH3) groups. More intense absorption peaks were found at 1477.9 cm
−1, 1478.5 cm
−1,and 1483.1 cm
−1,corresponding to the
C–H bond deformation vibration in methylene (
CH2) groups. Two groups of absorption peaks at 2856.1 cm
−1, 2859.2 cm
−1, 2892.8 cm
−1, and 2923.3 cm
−1, 2925.6 (2959.7) cm
−1, 2967.4 cm
−1 indicate valence vibrations of the
C–H bond in methyl and methylene groups. A comparison of the corresponding absorption intensities showed that after the neutralization, the methyl and methylene group contents were reduced by an average of 30–40%.
It is known that the symmetrical deformation vibration of the
C–H bond in methyl groups is shown at about 1375 cm
−1, but in the composition of complex compounds, it moves towards low frequencies and has a higher intensity due to the neighborhood with the carbonyl group (
C=
O) [
33]. Absorption peaks at 1797.2 cm
−1 and 1790.9 cm
−1 correspond to the valence vibration of the carbonyl group of a high-molecular hydrocarbons fragment. The neutralizer had no absorption peaks in this energy range. In addition, the absorption degree of the carbonyl group in the crude oil-contaminated soil is 29% higher than in the neutralized soil, which can give information onthereduction of asphaltenes content after neutralization.
Absorption peaks of 1415.3 cm
−1, 1415.5 cm
−1, and 1411.3 cm
−1 on the spectra of the crude oil-contaminated soil, the neutralized soil, and the neutralizer indicate the presence of carbonate-anion
. Content of the carbonate-anion is less in the neutralized soil by 33% than in the crude oil-contaminated soil. This can be explained by the decomposition of carbonates during the neutralization process:
The remainder of the anion is in the neutralized soil in the form of metal carbonates, mainly calcium carbonate, since the calcium content is substantially higher than that of sodium, potassium, and magnesium (
Table 6):
The presence of carboxylic acids (-COOH) having an internal hydrogen bond is confirmed by peaks at 1649.9 cm−1 (crude oil-contaminated soil), 1652.7 cm−1 (neutralized soil), and 1651.8 cm−1 (neutralizer). The availability of the carboxylic acid absorption band is due to the presence of humic additives in the reaction mixture. At the same time, their content is more by 47% and 29% in the neutralizer and the crude oil-contaminated soil, respectively, than in the neutralized soil.
The presence of acetylene compounds is confirmed by valence vibrations of C≡C bonds in monosubstituted alkynes and disubstituted alkynes, in which the substituents are different, by absorption peaks, respectively: 2139.5 cm−1 (crude oil-contaminated soil), 2140.1 cm−1 (neutralized soil), 2141.7 cm−1 (neutralizer),and 2195.3 cm−1 (crude oil-contaminated soil), 2196.4 cm−1 (neutralized soil), 2197.8 cm−1 (neutralizer). At the same time, it turned out that the number of bonds of C≡C in mono- and the disubstituted alkynes in the crude oil-contaminated soil and the neutralized soil is the same and almost three times less than in the neutralizer.
Absorption peaks at 2025.9 cm−1 and 2062.0 cm−1 (crude oil-contaminated soil), 2025.8 cm−1 and 2062.6 cm−1 (neutralized soil), and 2025.8 cm−1 and 2062.6 cm−1 (neutralizer) fall into the band of overtones (2222–2000 cm−1), characterizing the combination of antisymmetric deformation and torsional vibrations of groups. The content in the neutralizer is, on average, two times more than that of the crude oil-contaminated soil and the neutralized soil.
Peaks at 870.9 cm−1 (crude oil-contaminated soil), 860.7 cm−1 (neutralized soil), and 854.0 cm−1 (neutralizer) fall into the absorption band 900–675 cm−1,corresponding to out-of-plane deformation vibrations of C–H bonds in mono- and polynuclear aromatic compounds. The amount of this type of bond in the crude oil-contaminated soil is more than 50% higher than that of the neutralizer and the neutralized soil.
Thepresence of heterocyclic aromatic compounds is indicated by the presence of peaks at their band absorption spectra 1100–1000 cm−1 and 1580–1520 cm−1. The first of them, which characterizes deformation vibrations of the C–H bond in heterocyclic aromatic compounds, includes peaks at 1061.0 cm−1 (crude oil-contaminated soil), 1070.2 cm−1 (neutralized soil), and 1068.5 cm−1 (neutralizer). In the range of 1070.2 cm−1, which characterizes valence vibrations of bonds C=C, C=N in heterocyclic aromatic compounds, peaks occurred at 1567.4 cm−1 (crude oil-contaminated soil), 1573.1 cm−1 (neutralized soil), and 1575.1 cm−1 (neutralizer). After neutralization, the first kind of bond is reduced by 20%, and the second kind remains practically constant. This fact suggests that, in the neutralization process, the content of heterocyclic aromatic compounds with substituted nitrogen atoms is not changed, but heterocycles, the amount of heterocyclic compounds with substituted atoms of other elements (e.g., O, S, V, Ni, Ti), are decreased.
The presence of silicates was found in the neutralizer (954.7 cm−1) and the neutralized soil (954.8 cm−1). These peaks characterize vibrations in Si–O–Si bonds (970–940 cm−1).
The crude oil-contaminated soil contains unsaturated toxic hydrocarbons that react with the neutralizer. At the same time, the reaction of the current processes attheneutralization of the crude oil-contaminated soil can be described by the following equation:
where
are hydrocarbons and heterocyclic compounds before neutralization;
are hydrocarbons and heterocyclic compounds after neutralization.
Thus, when neutralizing the crude oil-contaminated soil, heavy oil fractions can be subjected to chemical degradation with the formation of low-toxic hydrocarbons.
3.5. Stabilized Soils
In order to study the possibility of the use of the neutralized soil in road construction, nine mixtures of stabilized soil were considered (
Table 7). As can be seen, the first three mixtures contained 60% of crushed stone, 15% of sand, and 25% of neutralized soil. Their Portland cement content was 6%, 7%, and 8%, respectively. They also contained different amounts of humectant. The other six mixtures did not contain sand. In the second and third triple of mixes, the content of crushed stone and the neutralized soil was 50%, 50%, and 30%, 70%, respectively. The content of Portland cement was equal to 9%, 10%, and 11%.
For visual reference, the granulometric curves of the neutralized soil and one of the stabilized soil mixes are represented in
Figure 7.
Engineering characteristics of the stabilized soils are given in
Table 8, from which it can be clearly seen that all strength indicators are increased with the increase of crushed stone and Portland cement content in the mixtures. As expected, compression strength is decreased in all cases as the number of freeze and thaw cycles is increased. The reduction in strength after 10, 15, and 25 cycles of freezing and thawing is, on average, 16%, 38%, and 53%, respectively.
According to the regulatory document [
35], all public roads in the Republic of Kazakhstan are divided into five categories depending on traffic intensity (
Table 9). The higher the road category, the stronger and more durable the materials used for their pavements. At the same time, for the roads of I–IV categories, the surface (first) layer of pavement is arranged from an asphalt concrete. As the multiyear design practice shows, the pavement of a IIIcategory road has two layers of asphalt concrete with a total thickness of 10 to 12 cm, and roads of I and IIcategories have three layers of asphalt concrete with a total thickness of 15 to 18 cm.
Stabilized soils on roads of the I–IV category roads can be used as a base layer material and a subbase layer material, and on V category roads as a pavement material [
36].
Table 10 shows the conditions for the use of the stabilized soils with the neutralized soil of different compositions.
Figure 8 shows a map of the isoline of the minimal temperature of −30 °C on the territory of Kazakhstan. A joint analysis of these tables and the maps shows that the stabilized soil containing 70% of the neutralized soil and 9–10% of Portland cement cannot be used in road construction in Kazakhstan. The stabilized soils of all other compositions can be used as a material of the base layer for pavements. At the same time, only the stabilized soils of I-1 and I-2 (60% crushed stone, 15% sand, 25% neutralized soil, and 7–8% of Portland cement) can be used for roads of the III, IV, and V categories and all others can only be used for roads of the IV and V categories. According to climatic requirements, only mixtures of I-1 and I-3 are allowed to be used in the areas with minimum temperatures below −30 °C, and the remaining mixtures can only be used up to −30 °C.
3.6. Experimental Section
An important stage in the implementation of new materials and technologies into road construction is the construction of an experimental section. The possibility for the implementation of the proposed technologies and materials was checked during the construction of an experimental section.
In November 2014, near the city of Zhanaozen (Mangistau region), an experimental road section was built using the stabilized soil with the neutralized soil. The test section had a length of 75 m and a pavement with a width of 3.5 m made from the stabilized soil. The stabilized soil had the following composition: crushed stone 5–20 mm fraction (50%), neutralized soil (40%), Portland cement of M 400 grade (10%), and water with humectant (12%).
Crushed stone was supplied from the “Shetpe” quarry and the neutralized soil from a storage site of the JSC “Ozenmunaigas”. The “Shetpe” quarry is located near Shetpe village, which is 139 km away from Zhanaozen city.
The technology for the construction of the pavement was implemented in the following sequence: the mixing of the crushed stone, the neutralized soil, and Portland cement was performed at the storage site; the mixture of crushed stone, neutralized soil and Portland cement was brought to the experimental section and distributed on the surface of the subgrade (
Figure 9); water with humectant was distributed by a highway tank truck produced by the Kamsk automobile plant (tank volume was 16 m
3); mixing of the mixture and water on the surface of the subgrade was performed by a grader (
Figure 10); pavement material—graded mixture of the stabilized soil with the neutralized soil—was compacted by a smooth drum roller, produced by Rascat (Ural automobile plant, 3 tons;
Figure 11).
As a result of the subsequent implementation of the above technology, a 15-cm thick pavement was built (
Figure 12).
Successful implementation of the project in the experimental section showed the full possibility for the use of the neutralized soil in road construction. Meanwhile, conventional machinery and road equipment wereused for transportation, mixing, leveling, and compaction.