Concentration and Distribution Characteristics of Σ16PAHs
In this experiment, 6 groups of coal samples from different mining areas were collected. The vitrinite reflectance (R0, max) of the coal seam where the coal samples are located are 0.60% (HDG), 1.21% (ML), 1.47% (TL), 1.84 (XM) % (XM), 2.73% (SJZ), 3.30% (GSY).
Table 3 summarizes the results for the concentrations of the Σ16PAHs in the samples. Fig. 3 shows that at the beginning, the concentrations of Σ16PAHs increase and reach the maximum 133012.45 ng/g at Tunlan Mine (R0,max=1.47%) before rapidly decreasing in higher rank coal. The degree of coal metamorphism affects the degree of aromatization. The less degree of coal metamorphism tends to be, the smaller aromatic ring coal has. Furthermore, the side chain contains more oxygen functional groups, that means the degree of aromatization is not enough, so the concentration of extracted Σ16PAHs is low. With the increase of metamorphism degree, the degree of condensation of aromatic ring is improving, the functional groups of side chain are gradually reducing, the degree of aromatization is increasing, the structure of aromatic molecules is increasing and the concentration of extracted Σ16PAHs is increasing.
When R0,max > 1.47%, the concentrations of these Σ16 PAHs tend to decrease with increase of the metamorphic degree. Especially when R0,max > 2.70%, the concentration of Σ16PAHs extracted tend to be little(6923.99~1896.84ng/g). The reason is that when the coal rank rises to a certain level (R0,max > 1.47%), the higher metamorphism degree tends to be, the greater aromatization in it gets. At the same time aromatic rings condense tighter in three-dimensional network of macromolecules. Therefore, the concentration of extracted Σ16PAHs gets little when the coal rank rises. In this process, the concentrations of Σ16PAHs with different-numbered rings continue to decrease due to the increasing degree of aromatization and 2-6 rings PAHs are condensed into higher-ring PAHs (> 6 rings).
In Fig. 4, with the increase of the degree of metamorphism, the concentrations of 3-6 rings PAHs increase and then decrease, which reach the maximum in Tunlan Mine (R0,max=1.47%). But the concentrations of 2 ring PAHs were a linear relationship with the rise of coal rank. In low-level metamorphic coal, the concentrations of PAHs are mainly composed of 3-4 rings PAHs. In medium-level metamorphic coal, the concentrations of PAHs are mainly composed of 5-6 rings PAHs, as low molecular weight PAHs condense into high molecular weight PAHs with the increase of aromatization degree.
Toxicity Change Analysis
Different types of PAHs have different properties and cause different degrees of damage to the environment (Table 4). The toxicity of the 16 PAHs is expressed in terms of the toxic equivalent (TEQ), which is calculated according to the formula TEQ=∑(ε × TEF), where ε represents the concentration of the PAHs with units of m /kg, and TEF (Toxic Equivalency Factor) is a TEQ factor. The TEF of BaP is defined as 1, and the other values are calculated based on it (Nisbet et al., 1992; Tsai et al., 2004).
The TEQ is calculated by the TEF equation. The TEQ of raw coal is illustrated in Fig. 5 With the increase of the degree of metamorphism, the TEQ tended to increase and then decreases. The highest TEQ of raw coal was found at degree of metamorphism of 1.47%.
The highest TEQ in raw coal was found at R0,max=1.47%, which was 32.71. Further, the minimum TEQ in raw coal was discovered at R0,max=3.30%, which was 0.013. Table 4 shows that the 2~3 rings PAHs and the 4 ring Pyr are not carcinogenic, but other PAHs have strong carcinogenicity and the TEF is larger. As is shown in fig. 5, when R0,max=1.47%, the concentrations of FluA (2735.80ng/g), BaA (1986.74ng/g), Chr (11231.72ng/g), BbF (6848.59ng/g), BkF (10778.73ng/g), BaP (15316.22ng/g), DbA (13917.34ng/g), BghiP (28535.81ng/g) and In[1,2,3-cd]P (10776.58ng/g) reach the maximum. Therefore, the concentrations of 4-6 rings PAHs determine the toxicity of PAHs.
Guide for Identification of the Origin of PAHs
The ratios Flua / (Flua + Pyr), An t/ (AnT + Phe) and BaA / (BaA + Chr) are commonly used as reliable approaches to distinguish between petrogenic and pyrogenic sources of PAHs (Suman et al., 2016; Wang et al., 2011; Li et al., 2015; Yu et al., 2017).
It could be concluded that the raw coal source of Flua / (Flua + Pyr) ranges from 0.237 to 0.340, Yunker et al. (2002a) suggested that Flua / (Flua + Pyr) ratio< 0.4 is characteristic of a petroleum origin, a ratio between 0.4 and 0.5 indicates liquid fossil fuel combustion, while a ratio >0.5 indicates coal combustion. Wen et al.(2018) suggested that Flua / (Flua + Pyr) ratio ranged from 0.34−0.97 in low-temperature combustion. In the collected samples, the ratio of Flua / (Flua + Pyr) was 0.237−0.340 with an average of 0.299 (Table 5),which were consistent with the ratio range of coal non-combustion in the literature (Yunker et al., 2002a).
A proportion of Ant/(Ant+Phe) > 0.1 suggests a dominance of petroleum, while a ratio < 0.1 reflects combustion. Meanwhile, a ratio of BaA/(BaA+Chr) < 0.2 indicates petroleum sources, 0.2 < BaA / (BaA + Chr) < 0.35 mean petroleum combustion, including liquid fossil fuels, vehicles, and crude oil combustion, and BaA / (BaA + Chr) > 0.35 indicates that the source of PAHs are coal, grass and wood combustion (Yunker et al., 2002a). Wen et al. (2018) suggests that Ant / (Ant + Phe) and BaA / (BaA + Chr) are almost 1 in low-temperature combustion. The proportions of Ant / (Ant + Phe) are less than 0.1 and BaA / (BaA + Chr) are less than 0.2 in the collected samples in the paper, which conforms to the definition of the source of petroleum in the literature.
In few cases, the values of above three ratios are not in agreement among them. Generally, the sources of PAHs in an environment can result different and occasional, we calculate a total index as the sum of single indices (discussed earlier) respectively normalized for the limit value (low-temperature sources high-temperature sources) reported in literature (Mannino et al., 2008; Orecchio, 2010): total index = Flua / (Flua + Pyr) / 0.4 + Ant / (Ant + Phe)/0.1 + InP / (InP + BghiP) / 0.2 + BaA / (BaA + Chr) / 0.2. The high-temperature process (combustion), the total index of which are greater than 4, was generally thought to be the source of PAHs. Otherwise, petroleum products were considered to be the main source of PAHs. Wen et al. (2018) suggested that total index ranged from 20.10~22.43 in low-temperature combustion.
According to the general index formula, the total index of PAHs in raw coal collected ranged from 3.17 to 3.74 with a mean of 3.59, both less than 4, which are consistent with the source of PAHs in the literature (Suman et al., 2016; Yu et al., 2017).
The range for diagnostic ratios of Flua / (Flua + Pyr), Ant / (Ant + Phe), BaA / (BaA + Chr) and total index from coal in the paper could be compared with petroleum origin, coal combustion and low-temperature combustion of coal gangue from previous work as seen in Table 6, in which, they are in apparent different range.