Soil pH is important for enzyme activity (
9,
27). The selection of pH depends on the organisms used for biodegradation (
28). In the present study, after three days, pH values were decreased to 2.2 and 1.1 for consortium types A and B, respectively. The decrease in pH could attribute to the intermediate material produced by the consortium. In most studies, researchers reported that alkane degradation occurs at neutral pH. The pH of soil according to soil composition and history ranged from around 2.5 to around 10 (
29). Schauer pointed out in his review that the oxidation rates of hydrocarbons varied only slightly at pH values between 5 and 8, whereas oxidation and even toxicity of organic acids, microbial hydrocarbon metabolism products, were clearly dependent on pH (
30). In another study, Rhodococcus erythropolis strain NTU-1 was incubated in fed-batch bioreactor for bioremediation of diesel and petroleum. After six days of incubation with diesel, the pH decreased from 7 to 4.3, while in incubations with petroleum, the pH decreased from 7 to 5. In addition, pH changes were related to cell growth (
31). It is known that pH changes of the medium affect the net charge of polysaccharides, phosphates, and amino groups on a cell’s surface (
32). Also, results of the study of Dastgheib et al. showed that biodegradation of polycyclic aromatic hydrocarbons with
Alcanivorax dieselolei strain QTET was extremely unstable at high pH. The range of its pH tolerance was limited (pH 6 to 8) and its optimum growth was at neutral pH (
33).
Dissolved oxygen is essential for biodegradation (
23). Because there is a high concentration of hydrogen and carbon, yet small amounts of oxygen in petroleum compounds (
34), 3 to 4 mL of dissolved oxygen are required to oxidize 1 mL of hydrocarbons to CO
2 and H
2O (
35). For aerobic bacteria, stoichiometrically, 3.1 mg/mL of oxygen is needed for the biodegradation of 1 mg/mL of hydrocarbons, regardless of the total mass of bacteria (
36). In this study, after three days, the dissolved oxygen for consortium types A and B decreased to 4 and 2.1 mg/L, respectively. In agreement with other reports, such as that of Venkata Mohan et al. (
5) and Juneson et al. (
37), the activity of microorganisms and the rate of oxygen uptake increased.
Temperature has a noticeable effect on the capability of microorganisms for degradation of petroleum hydrocarbons. In addition, with rising temperature, solubility of oxygen is reduced, and consequently metabolic activity of aerobic microorganisms is also reduced. Most oil-degrading organisms are active in the meso-thermal ranges (20°C to 35°C) and have the best degradation rates at these temperatures (
35). Some exceptions exist; for example, Rueter et al. (
38) described a slightly thermophilic anaerobic strain (TD3) that degrades alkane under sulphate-reducing conditions; Klug and Markovetz (
39) reported on thermophilic bacteria, which can degrade n-tetradecane. Also, industrial alkane degradation at high temperatures (e.g. 65°C to 70 °C) has been reported (
40). Based on the current results, the temperature for consortium types A and B increased to 3.5°C and 1.5°C, respectively after three days. There was a direct relationship between temperature and activity of microorganisms, thus microorganisms activity increases with increasing temperature and conversely (
41).
The findings of this study indicate that After three days, the number of active bacteria for consortium types A and B increased to 9 × 10
4 and 99 × 10
4 CFU/mL, respectively (
Table 2). Genthner et al. reported that almost all PAHs are degraded at 15°C and at an oxygen level of 4 ppm, and at 40°C most PAHs are degraded at 0 ppm oxygen level (
42). The increase in the number of active bacteria can be due to further adaptation of bacteria to the bioreactor and greater growth. In addition, it can concluded that bacteria type A were more compatible with oil hydrocarbons than type B. Genthner et al. reported that almost all PAHs are degraded at 15°C and at an oxygen level of 4 ppm, and at 40°C most PAHs are degraded at 0 ppm oxygen level (
42). A few researchers showed that the number of active bacteria was 5.25 × 10
5, 1.76 × 10
6 and 5.11 × 10
5 cells per mL of soil. Besides, they showed that these species can degrade n-hexadecane up to a concentration of 120 ppm and a consortium of species could degrade n-hexadecane faster than they do separately (
43).
Maximum simultaneous bioremediation of n-hexadecane by consortium type A and B was 17.61 and 13.22 percent. In addition, maximum simultaneous bioremediation of n-dodecane by consortium type A and B was 28.55 and 19.24 percent (
Table 3). On the other hand, the bioremediation of n-hexadecane by consortium type A on days one, two, and three was 1.99, 2.17, and 4.39 percent greater than type B. The bioremediations of n-dodecane by consortium type A on days one, two, and three was 4.33, 2.67, and 10.94 percent greater than type B (
Table 3). Based on the results, it can be concluded that consortium type A had better adaptation with bioreactor conditions than type A. In addition, bioremediation of n-dodecane during the three days of operation cycle was greater than n-hexadecane (
Table 3). Considering the molecular formula of n-dodecane (C
12H
26), with lower carbon and hydrogen than n-hexadecane (C
16H
34), it can be suggested that the bacteria had a higher potential for bioremediation of n-dodecane than n-hexadecane. In Lopez et al.’s study, the findings showed that bioremediation was significantly influenced by different bioavailability (
44). Also, Sun et al. (
45) studied the simultaneous bioremediation of n-hexadecane and phenol. They found the strains were capable of simultaneous bioremediation of phenol and n-hexadecane in the mineral medium. However, the strains preferred phenol to n-hexadecane. Also, the coexistence of phenol and n-hexadecane was outperformed in the growth of strains in comparison with when they were used individually (
45). A simulation test was conducted to study biodegradation of aromatic hydrocarbons (phenanthrene and anthracene) and aliphatic hydrocarbon (n-hexadecane) by native microorganisms, when the soil contained the test hydrocarbons individually or in coexistence. The results showed that coexistence of phenanthrene and n-hexadecane could serve as a co-metabolic substrate and promote biodegradation of phenanthrene, lessening the half-life of phenanthrene by 44% in comparison with when phenanthrene existed individually (
46).
5.1. Conclusions
The results showed that the maximum simultaneous bioremediation of n-hexadecane and n-dodecane by consortium type A was 17.61 and 28.55 percent, respectively. In addition, the maximum simultaneous bioremediation of n-hexadecane and n-dodecane by consortium type B was 13.22 and 19.24 percent, respectively. Bioremediation of n-hexadecane and n-dodecane by bacterial consortium Type A (isolated from contaminated soil with oil) was significantly greater than type B (isolated from compost). In general, the bioremediation of n-dodecane during three days of the reactor’s running cycle was greater than n-hexadecane. The findings of this study showed the simultaneous bioremediation of n-hexadecane and n-dodecane in an S-SBR, using two types of bacterial consortium (type A and B) during a three-day period, was relatively satisfactory.