3.1 Determination and characteristic of the leachate leakage
The resistivity inversion results of the landfill site are showed in Fig. 2 and Fig. 3. Previous studies reported that the appearance of low resistivity could be explained by high iron concentrations in leachate (Rosqvist et al., 2003; Kjeldsen et al., 2002). The landfill body is mostly composed of domestic garbage, which is easily corroded to produce leachate with strong conductivity and low resistance. While the resistivity of quartz sandstone, siltstone and other bedrock is higher. The overall decline in resistivity can be influenced by soils formed from altered or broken rocks and cracks and other geological structures (Lopes et al., 2012; Meju, 2000). Low resistance zone appeared under the landfill body in survey lines of S001-S004 and S010-S021 (Fig. 2). It was inferred that the anomalies were caused by tomographic relief based on the site topography and geomorphology characteristics. The uniform curves of apparent resistivity reflected the regular contact between the body and stratum, indicating that there is no leachate leakage under the impervious barrier.
Compared with the inversion sections of lines S005-S009 and S022-S025 (Fig. 3), the low-resistance areas were narrow and went down deeper (lines of S005-S009), and the contact areas between the waste body and the quartz sandstone were unclear (lines of S022-S025). Obviously, the leachate diffused vertically, and the landfill impervious layer was broken. Through analyzing of the multiple anomalies with low resistance occurred in different survey lines, it is inferred that leakage areas are existing in the middle of the landfill site with a depth of 15-20m (lines of S005 ~ 009), the middle area near the anti-seepage dam with a depth about 17-22m (lines of S022 ~ 025), and the south area of the dam with a depth about 15-22m (lines of S024 ~ 025).
For further information about the possible influence of leachate leakage on surrounding environment, untreated leachate from the regulating tank was analyzed specially (Table 3). Base on the standard for pollution control on the landfill site of municipal solid waste (GB16889-2008), all the measured values of parameters (except As.) exceeded the emission limits of water pollutants, and NH3-N, CODMn which reflect the main pollution factors of household waste far exceeded the standard by dozens or hundreds of times. The Nemerow index method was used to evaluate the leachate pollution in the landfill site, with the calculated values of 83.6 (Table 3). This result indicates that the leachate in the landfill site had a great pollution potential to the surrounding environment as the main pollution source, this could be attributed to the leachate gathering caused by the horizontal and vertical block by impervious barrier (Ye et al., 2021). Therefore, it is necessary to regularly monitor the site anti-seepage system to avoid the failure of the system and long-term collection and infiltration of leachate, which would cause underground soil and water pollution.
Table 3
Composition and quality assessment of landfill leachate
Indicator
|
pH
|
CODMn
|
NH3-N
|
As
|
Hg
|
Pb
|
Cd
|
Cr
|
Fe
|
Mn
|
NPI
|
Unit
|
-
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
/
|
Measured Value
|
5.5
|
6651
|
2648
|
0.099
|
0.0098
|
8.05
|
0.265
|
7.74
|
10.36
|
0.47
|
83.60
|
Referenced Value#
|
/
|
100
|
25
|
0.1
|
0.001
|
0.1
|
0.01
|
0.1
|
/
|
/
|
“#”: It was referred to the standard for pollution control on the landfill site of municipal solid waste (GB 16889 − 2008).
Table 4
Statistical analysis of pollutant concentration and water quality evaluation
Indicator
|
Depth
|
pH
|
TDS
|
Total hardness
|
CODMn
|
NH3-N
|
SO42−
|
Cl−
|
F−
|
Hg
|
Fe
|
Mn
|
Cu
|
Zn
|
NO2-N
|
NO3-N
|
Water
Quality
|
NPI1
|
NPI2
|
Unit
|
m
|
/
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
mg/L
|
LS102
|
0
|
6.64
|
12.6
|
7.95
|
0.80
|
0.06
|
0.484
|
0.569
|
-
|
0.0002
|
0.002
|
0.003
|
-
|
0.004
|
-
|
0.295
|
Ⅲ
|
-
|
-
|
Grade
|
|
Ⅲ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅱ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅲ
|
Ⅰ
|
Ⅱ
|
Ⅰ
|
Ⅰ
|
Ⅱ
|
Ⅰ
|
LS101
|
1.5
|
6.51
|
26.3
|
15.22
|
1.11
|
0.13
|
4.622
|
0.746
|
-
|
0.0001
|
0.102
|
0.037
|
-
|
0.002
|
-
|
3.629
|
Ⅲ
|
-
|
-
|
Grade
|
|
Ⅲ
|
Ⅰ
|
Ⅰ
|
Ⅱ
|
Ⅲ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅱ
|
Ⅱ
|
Ⅰ
|
Ⅰ
|
Ⅱ
|
Ⅱ
|
SK01
|
0.24
|
6.01
|
41.57
|
27.89
|
2.31
|
0.291
|
11.43
|
1.973
|
0.066
|
0.0003
|
2.763
|
0.626
|
-
|
0.016
|
-
|
0.542
|
Ⅴ
|
19.46
|
6.61
|
Grade
|
|
Ⅳ
|
Ⅰ
|
Ⅰ
|
Ⅲ
|
Ⅲ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅲ
|
Ⅴ
|
Ⅳ
|
Ⅰ
|
Ⅰ
|
Ⅱ
|
Ⅰ
|
SK02
|
2.98
|
6.7
|
107.77
|
84.68
|
0.79
|
0.69
|
32.78
|
1.84
|
-
|
0.0006
|
0.007
|
0.235
|
0.002
|
-
|
-
|
1.278
|
Ⅳ
|
5.37
|
1.68
|
Grade
|
|
Ⅲ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅳ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅲ
|
Ⅰ
|
Ⅳ
|
Ⅰ
|
Ⅰ
|
Ⅱ
|
Ⅰ
|
SK03
|
0.22
|
6.25
|
64.91
|
49.25
|
0.86
|
0.489
|
25.52
|
4.096
|
-
|
0.0001
|
0.031
|
0.236
|
0.007
|
0.024
|
-
|
1.182
|
Ⅳ
|
8.75
|
1.68
|
Grade
|
|
Ⅳ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅲ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅳ
|
Ⅰ
|
Ⅰ
|
Ⅱ
|
Ⅰ
|
SK04
|
2.18
|
5.80
|
92.79
|
50.07
|
1.30
|
0.742
|
30.23
|
14.77
|
0.039
|
0.0001
|
0.072
|
1.181
|
0.002
|
0.034
|
0.121
|
9.787
|
Ⅳ
|
23.19
|
8.39
|
Grade
|
|
Ⅳ
|
Ⅰ
|
Ⅰ
|
Ⅱ
|
Ⅳ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅳ
|
Ⅰ
|
Ⅰ
|
Ⅱ
|
Ⅲ
|
SK05
|
1.86
|
6.51
|
16.72
|
9.59
|
1.01
|
0.379
|
2.04
|
4.617
|
0.167
|
0.0002
|
0.057
|
0.06
|
0.012
|
0.024
|
0.037
|
2.058
|
Ⅲ
|
8.65
|
0.55
|
Grade
|
|
Ⅲ
|
Ⅰ
|
Ⅰ
|
Ⅱ
|
Ⅲ
|
Ⅰ
|
Ⅰ
|
Ⅰ
|
Ⅲ
|
Ⅰ
|
Ⅲ
|
Ⅱ
|
Ⅰ
|
Ⅱ
|
Ⅱ
|
Maximum
|
2.98
|
5.80
|
12.60
|
7.95
|
0.79
|
0.060
|
0.484
|
0.569
|
-
|
0.0001
|
0.002
|
0.003
|
-
|
-
|
-
|
0.295
|
|
|
|
Minimum
|
0
|
6.70
|
107.77
|
84.68
|
2.31
|
0.742
|
32.780
|
14.77
|
0.167
|
0.001
|
2.763
|
1.181
|
0.012
|
0.034
|
0.121
|
9.789
|
|
|
|
Mean
|
-
|
6.35
|
51.81
|
34.95
|
1.17
|
0.397
|
15.301
|
4.087
|
-
|
0.000
|
0.433
|
0.340
|
0.006
|
0.017
|
-
|
2.682
|
|
|
|
Class Ⅲ standard value2
|
|
|
1000
|
450
|
3.0
|
0.5
|
250
|
250
|
1.0
|
0.001
|
0.3
|
0.1
|
1.0
|
1.0
|
1.0
|
20
|
|
|
|
Over standard rate (%)
|
-
|
28.6
|
-
|
-
|
-
|
28.57
|
-
|
-
|
-
|
-
|
14.29
|
14.29
|
-
|
-
|
-
|
-
|
57.14%
|
|
|
“1”: It was referred to the background values of sample LS01 (GB 16889 − 2008);
“2”: It was referred to the class Ⅲ standard for groundwater quality (GB/T 14848 − 2017).
3.2 Characteristics of groundwater quality and pollution
Tested parameters of groundwater from the upstream to the downstream in the studied area are shown in Table 4. The concentrations of volatile phenols, cyanide, As, Cr, Pb and Cd in all samples, as well as fluoride, Cu and nitrite in some samples were below the detection limits. The pH values in groundwater ranged from 5.80 to 6.70, with the rate of 28.57% exceeding the class Ⅲ standard for groundwater quality (GB/T 14848 − 2017). And the concentrations of NH3-N, Fe and Mn ranged from 0.06 to 0.74 mg/L, 0.002–2.763 mg/L, and 0.003–1.181 mg/L, with the rate of 28.57%, 4.29%, and 14.29% exceeding standard, respectively. The maximum concentrations were 1.48, 9.21, and 11.81 times of the values of class Ⅲ water quality standard, respectively. In addition, the groundwater quality at ZK02, ZK03 and ZK04 sampling points reached the Class Ⅳ standard, and the main pollutants were pH, NH3-N and Mn. While SK01 reached Class Ⅴ water quality standard, its pH and Mn reached Class Ⅳ standard and Fe reached to Class Ⅴ standard, which showed the extremely poor groundwater quality.
Generally speaking, leachate generated from upstream site may infiltrate and pollute groundwater downstream, and furthermore lead to the concentrations of Fe, NH3-N, NO3-N and other compositions exceeding the standard values (Xu et al., 2021). As shown in Fig. 4, all parameters of borehole samples (ZK01 to ZK05) were higher than that of background wells (LS01 and ZK02), suggesting that the groundwater system in the landfill has been polluted. According to the locations of each sampling point, the linear distance to landfill site from far to near was ZK03 < ZK04 < ZK02 < ZK01 < ZK05, and the sampling depth from shallow to deep was ZK03 < ZK01 < ZK05 < ZK04 < Zk02. But the concentration of indicators did not change regularly with the distance and depth, indicating that there were other contributing factors in the pollution process (Varol et al., 2018). It was pointed out that the impact of landfill on groundwater quality depended on waste composition, soil accumulation, rainfall, hydraulic gradient and the geological environment of the landfill (Singh et al, 2008), which should be further investigated.
The highest concentration of Fe was found at ZK01, secondly at LS01 of background well. Contents of Fe and Mn in quartz sandstone in the study area were 4.47% and 0.21%, respectively. The excess of Fe in groundwater may be related to the underlying strata. The highest concentration of Mn was found at ZK04, followed by ZK01 to ZK03, but little at the background sites. ZK04 was sampled beneath the damaged anti-seepage dam and closest to the waste body, indicating that the Mn pollution in groundwater possibly mainly originated from landfill leakage rather than underlying bedrock. The concentrations of NH3-N were higher in samples of ZK02 to ZK04, followed by ZK05 and ZK01, and a small amount was also detected in the background wells. NH3-N was diffused taking landfill as the center and accumulated downstream controlled by rock fractures, hydraulic gradient and damaged dam.
To have a better comparison about the comprehensive groundwater pollution, the Nemerow pollution index method was used based on the parameter concentrations of background well at LS01 and the class Ⅲ standard for groundwater quality (GB/T 14848 − 2017). The results (Table 4) showed that, relative to the local background value, groundwater of all monitoring sites in the landfill were heavily polluted (NPI > 3), with a descending order of ZK04 (NPI = 23.19) > ZK01 (NPI = 19.46) > ZK03 (NPI = 8.75) > ZK05 (NPI = 8.65) > ZK02 (NPI = 5.31). While compared with the class Ⅲ standard (GB/T 14848 − 2017), only ZK01 and ZK04 belonged to severe polluted condition (NPI > 3), samples of ZK02 and ZK03 were in slight polluted risk (1.0 < NPI ≤ 2.0), and ZK05 was clean (NPI ≤ 0.7). The order of NPI for samples was ZK04 (NPI = 8.39) > ZK01 (NPI = 6.61) > ZK03 (NPI = 1.68) = ZK02 (NPI = 1.68) > ZK05(NPI = 0.55). The two calculated results displayed a great difference about the comprehensive pollution degree of groundwater. But groundwater at ZK01 and ZK04 was seriously polluted in either case. Nemerow pollution index method would highlight the impact of maximum value on pollution degree (Xie et al., 2023; Ye et al., 2021), Fe and Mn in the sites of ZK04 and ZK01 seriously exceeded the standard, which results in that the indexes of samples ZK04 and ZK01 were much higher than that of others.
3.3 Correlations between groundwater parameters
3.3.1 Correlation analysis (CA)
The correlation analysis result of each parameter in groundwater of landfill site was shown in Fig. 5. pH was negatively correlated with most of the parameters, especially with Mn (r=-0.897) and Zn (r=-0.778). Podlasek et al. (2023) also reported a similar relationship in the leachate parameters of different landfills. A large number of studies have confirmed that pH could affect the solidification of heavy metals in soils, and the solubility of heavy metals would increase with the decrease of pH value (Wijesekara et al., 2014; Lindamulla et al., 2022; Wdowczyk and Szymanska-Pulikowska., 2021). There were significant positive correlations between total mineralization, total hardness, NH3-N and SO42− in groundwater (r = 0.834 ~ 0.982). Similar results were also reported by Zhao et al (2016) and Zhou et al (2022), that the total dissolved solids in groundwater was significantly related with SO42− and Ca2+. Moreover, some studies believed that EC was highly associated with NH3-N (Mohammad-Pajooh et al., 2017), and sensitive to changes of TDS in leachate (Gupta and Paulraj, 2017). The high values of these parameters indicated high contents of dissolved inorganic and organic compounds (Gupta and Paulraj, 2017).
Remarkably, positive correlation appeared in CODMn and Fe (r = 0.949). CODMn reflects the pollution degree of water by reducing organic matter or inorganic matter, which can activate metals such as Fe and Mn in soil and enhance the migration ability of these metals into the groundwater by rainfall, resulting in serious Fe and Mn pollution (Xia et al., 2002). In addition, weak correlations between HMs should be noted, possibly due to their low concentration in leachate (Engelmann et al, 2017). However, Cl− was positively related with Mn (r = 0.839) and Zn (r = 0.822), suggesting their similar source (Abunama et al, 2021).
3.3.2 Principal component analysis (PCA)
The relevance of parameters can be revealed by PCA to supplement the obstacles by CA, for minimizing the loss of data analysis (Mishra et al., 2016; Vahabian et al., 2019). Because the sample size was too small for source analysis in this study, PCA analysis aimed to reduce the variables that characterize groundwater quality (Wdowczyk and Szyma 'nska-Pulikowska, 2021).
PCA extracted five principal components from the parameters of groundwater, which accounted for 98.89% of the total variance (Table 5). Among them, PC1 accounts for 29.31% of the total variance loaded strongly by the total salinity, total hardness, NH3-N and SO42−, followed by Hg and sampling depth. Researches have pointed out that inorganic parameters such as EC, TDS, COD and NH4+ were dominant in PC1, resulting in great data differentiation (Podlasek et al., 2023; Ergene et al., 2022). PC2 accounts for 26.85% of the total variance, which exhibits strong loading of Cl−, Mn and NO3-N. The CODMn and Fe have extremely strong loads on PC3, accounting for 17.23% of the total variance. PC4 is much concerned with Cu and F−, and accounts for 13.39% of the total variance. PC5 is related to strong negatively loadings of NO2-N and account for 12.11%.
Table 5
The PCs distinguished from the chemical characteristics of groundwater
Variables
|
Factor 1
|
Factor 2
|
Factor 3
|
Factor 4
|
Factor 5
|
depth
|
0.58
|
0.22
|
-0.36
|
0.18
|
0.63
|
pH
|
-0.11
|
− .77*
|
-0.55
|
-0.02
|
0.30
|
TDS
|
0.95**
|
0.25
|
-0.04
|
-0.16
|
-0.02
|
Total hardness
|
0.99**
|
-0.01
|
-0.06
|
-0.14
|
-0.05
|
CODMn
|
-0.10
|
0.20
|
0.96**
|
-0.01
|
0.09
|
NH3-N
|
0.88**
|
0.41
|
-0.07
|
0.24
|
-0.02
|
Cl−
|
0.29
|
0.92**
|
-0.05
|
0.19
|
-0.06
|
Hg
|
0.64
|
-0.56
|
0.14
|
-0.02
|
0.48
|
F−
|
-0.24
|
0.13
|
0.22
|
0.892**
|
0.28
|
Fe
|
-0.07
|
-0.10
|
0.99**
|
-0.03
|
0.03
|
Mn
|
0.39
|
0.81*
|
0.42
|
-0.08
|
-0.02
|
Cu
|
0.01
|
-0.03
|
-0.29
|
0.928**
|
-0.22
|
Zn
|
0.07
|
0.73
|
0.16
|
0.53
|
-0.39
|
NO2-N
|
0.26
|
0.17
|
-0.17
|
0.07
|
-0.93**
|
NO3-N
|
0.16
|
0.95**
|
-0.17
|
-0.08
|
0.15
|
SO42−
|
0.93**
|
0.27
|
-0.04
|
-0.12
|
-0.20
|
Eigenvalues
% of variance
|
29.31
|
26.85
|
17.23
|
13.39
|
12.11
|
Cumulative %
|
29.31
|
56.16
|
73.39
|
86.78
|
98.89
|
3.4 Health risk assessment
Carcinogens likes As, Cr and Cd in samples were all lower than the detection limit (Table 4), and the carcinogenic risk through drinking was ignored. Based on the RBCA model, the non-carcinogenic risks of Fe, Mn, Hg, Cu, Zn, NH3-N, F−, Cl−, NO2-N and NO3-N in the landfill groundwater were evaluated (Table 6). It can be seen that the total non-carcinogenic risk levels of the drillhole samples all exceeded the maximum acceptable limit of 1, except for the background wells. The total hazard quotient through groundwater drinking in the study area was much higher in an order of LS102 < LS101 < ZK02 < ZK01 < ZK03 < ZK05 < ZK04. The closer sampling points to the waste body, the higher the risk to human by water drinking. The HQs of single parameter were in descending order of Cl− > Mn > NO3-N > Fe > Hg > F− > NH3-N > NO2-N > Cu > Zn. Only the HQs of Cl− in samples of ZK03 to ZK05 were greater than 1, while that of other parameters at different sampling points were lower than 1. It should be noted that the HQ of Mn at the ZK04 point was close to 1. To sum up, Cl− and Mn are the main pollutants causing non-carcinogenic risk in the study area, and landfill leachate pollution would bring harm to the area below the dam, which decreases with the increased distance from the waste body.
Table 6
Health risk assessment results based on RBCA model
Sample
sites
|
NH3-N
|
Cl−
|
F−
|
Hg
|
Fe
|
Mn
|
Cu
|
Zn
|
NO2-N
|
NO3-N
|
Total hazard
quotient
|
LS102
|
2.33E-03
|
2.14E-01
|
0.00E + 00
|
2.51E-02
|
2.51E-04
|
2.46E-03
|
0.00E + 00
|
5.02E-04
|
0.00E + 00
|
6.94E-03
|
2.52E-01
|
LS101
|
5.05E-03
|
2.81E-01
|
0.00E + 00
|
1.26E-02
|
1.28E-02
|
3.03E-02
|
0.00E + 00
|
2.51E-04
|
0.00E + 00
|
8.54E-02
|
4.27E-01
|
ZK01
|
1.13E-02
|
7.43E-01
|
4.14E-02
|
3.77E-02
|
3.47E-01
|
5.13E-01
|
0.00E + 00
|
2.01E-03
|
0.00E + 00
|
1.28E-02
|
1.71E + 00
|
ZK02
|
2.68E-02
|
6.93E-01
|
0.00E + 00
|
7.53E-02
|
8.79E-04
|
1.92E-01
|
1.88E-03
|
0.00E + 00
|
0.00E + 00
|
3.01E-02
|
1.02E + 00
|
ZK03
|
1.90E-02
|
1.54E + 00
|
0.00E + 00
|
1.26E-02
|
3.89E-03
|
1.93E-01
|
6.59E-03
|
3.01E-03
|
0.00E + 00
|
2.78E-02
|
1.81E + 00
|
ZK04
|
2.88E-02
|
5.56E + 00
|
2.45E-02
|
1.26E-02
|
9.04E-03
|
9.67E-01
|
1.88E-03
|
4.27E-03
|
4.56E-02
|
2.30E-01
|
6.89E + 00
|
ZK05
|
1.47E-02
|
1.74E + 00
|
1.05E-01
|
2.51E-02
|
7.16E-03
|
4.91E-02
|
1.13E-02
|
3.01E-03
|
1.39E-02
|
4.84E-02
|
2.02E + 00
|