| Literature DB >> 30081526 |
Hong Wang1, Lei Nie2, Yan Xu3, Chao Du4, Tao Zhang5, Yuzheng Wang6.
Abstract
Transportation activities such as fuel consumption, vehicle wear and road deicing can detrimentally affect the groundwater quality of fragile roadside wetland environments including. Nineteen parameters (Cu, Pb, Zn, Cd, Cr, Ni, Hg, As, pH, TDS, Ca2+, Mg2+, Na⁺, K⁺, SO₄²-, Cl-, HCO₃-, NO₃- and F-) were determined in groundwater samples from turfy swamps impacted by highway traffic from Jiangyuan (JY), Longquan (LQ), and Huangsongdian (HSD). Our results indicate that the metals Cu, Pb, Zn, Cr, Cd, the ions Na⁺, K⁺ and Cl- in groundwater were negatively affected by highway transportation, and the maximum affected distance of these pollutants varied from 15 to 100 m. The content of most of these pollutants in roadside groundwater decreased exponentially with the distance from the highway, as did the heavy metal pollution index HPI and Cd. The values of HPI and Cd in these three sites ranged from 46.8 to 78.4 and -4.9 to -2.9, respectively. The low pollution levels of heavy metals are related to the strong adsorption capacity of turfy soil towards metals. In any case, road transport activities increased the Cu, Pb, Zn, Cr, Cd, Na⁺, K⁺ and Cl- content in roadside groundwater in turfy swamp. With the increase of highway operation time, it will inevitably have a great influence on the groundwater quality of these wetlands. Therefore, the long-term monitoring is necessary to protect the sustainable development of turfy swamp.Entities:
Keywords: groundwater quality; heavy metals; highway transportation; turfy swamp
Mesh:
Substances:
Year: 2018 PMID: 30081526 PMCID: PMC6121959 DOI: 10.3390/ijerph15081652
Source DB: PubMed Journal: Int J Environ Res Public Health ISSN: 1660-4601 Impact factor: 3.390
Figure 1Study area and sampling sites in the Changbai Mountain area, Jilin Province.
Storage requirements and test methods for groundwater samples.
| Parameter | Sampling Volume | Container Material | Preservation Method | Test Method |
|---|---|---|---|---|
| Cu, Pb, Zn, Cd, Ni | 500 mL | P | Add concentrated HNO3 and adjust pH to 1–2 | ICP-MS |
| Cr | 100 mL | P | Add NaOH and adjust pH to 8–9 | ICP-MS |
| Hg | 250 mL | B | Add concentrated HNO3 and adjust pH to 1–2 | Atomic florescence spectrum |
| As | 250 mL | B | Add concentrated H2SO4 and adjust pH to 1–2 | ICP-MS |
| Ca2+, Mg2+, Na+, K+, SO42−, Cl−, HCO3−, F− | 500 mL | P | Original preservation | Ca2+, Mg2+, Na+, K+: ICP-AES |
| NO3− | 100 mL | P | Original preservation | Ion chromatography method |
P. Polypropylene bottles; B. Borosilicate bottle; Original preservation: After sampling, no chemical reagents are added.
Descriptive statistics of heavy metal concentrations (μg L−1) in groundwater of turfy swamps.
| Cu | Pb | Zn | Cd | Cr | Hg | Ni | As | |
|---|---|---|---|---|---|---|---|---|
| JY site | ||||||||
| Mean | 48.5a | 23.2ab | 100.0ab | 1.57a | 5.0a | 0.7b | 8.9a | 8.7a |
| SD | 7.4 | 5.0 | 10.6 | 0.18 | 1.4 | 0.1 | 1.0 | 0.8 |
| Min | 35.2 | 15.4 | 80.3 | 1.26 | 3.4 | 0.5 | 7.7 | 7.2 |
| Max | 61.5 | 30.5 | 118.3 | 1.91 | 7.3 | 0.8 | 10.8 | 9.9 |
| CV (%) | 15.2 | 21.5 | 10.6 | 11.5 | 26.8 | 6.5 | 8.5 | 8.6 |
| LQ site | ||||||||
| Mean | 58.3a | 26.3a | 114.2a | 1.75a | 5.4a | 0.08b | 6.9b | 3.1b |
| SD | 10.5 | 5.1 | 8.0 | 0.22 | 0.7 | 0.001 | 0.8 | 0.3 |
| Min | 43.3 | 17.6 | 97.3 | 1.41 | 4.23 | 0.07 | 5.8 | 2.4 |
| Max | 78.1 | 34.1 | 126.8 | 2.33 | 6.81 | 0.08 | 8.3 | 3.6 |
| CV (%) | 18.1 | 19.2 | 17.0 | 13.1 | 13.0 | 3.5 | 10.8 | 10.2 |
| HSD site | ||||||||
| Mean | 20.6b | 16.5b | 91.0b | 1.27b | 6.6a | 3.0a | 6.9b | 8.0a |
| SD | 1.9 | 0.8 | 8.1 | 0.12 | 1.4 | 0.1 | 0.4 | 0.6 |
| Min | 17.3 | 15.3 | 79.0 | 1.14 | 4.1 | 2.4 | 6.3 | 7.3 |
| Max | 23.6 | 18.1 | 106.2 | 1.51 | 9.2 | 3.6 | 7.9 | 9.7 |
| CV (%) | 9.3 | 5.1 | 8.9 | 9.93 | 21.2 | 8.3 | 6.5 | 7.6 |
| ACV (%) | 14.2 | 15.3 | 12.2 | 11.50 | 20.3 | 6.1 | 8.6 | 8.8 |
| Class III | 1000 | 50 | 1000 | 5 | 50 | 1 | 20 | 10 |
The data with different superscript lower case letters have significant differences (p < 0.05) in the columns; JY. Jingyu site; LQ. Longquan site; HSD. Huangsongdian site; CV. Coefficient of variation; ACV. Average CV; Class III. The water used for the second level reserve of groundwater source for drinking in China.
Descriptive statistics of hydrochemical parameters concentrations (mg L−1) in groundwater of turfy swamps.
| pH | TDS | Ca2+ | Mg2+ | Na+ | K+ | SO42− | Cl− | HCO3− | NO3− | F− | |
|---|---|---|---|---|---|---|---|---|---|---|---|
| JY site | |||||||||||
| Mean | 5.6 | 186.8 | 15.6 | 7.2 | 3.1 | 1.4 | 12.4 | 4.4 | 202.1 | 0.43 | 0.11 |
| SD | 0.5 | 3.1 | 0.9 | 0.7 | 0.7 | 0.5 | 0.5 | 0.6 | 3.1 | 0.05 | 0.02 |
| Min | 4.4 | 180.0 | 14.3 | 6.5 | 2.3 | 0.9 | 11.9 | 3.4 | 195.2 | 0.37 | 0.09 |
| Max | 6.3 | 191.0 | 17.3 | 8.9 | 4.6 | 2.6 | 13.3 | 5.6 | 207.5 | 0.52 | 0.15 |
| CV (%) | 9.0 | 1.6 | 5.9 | 9.3 | 21.7 | 36.2 | 4.0 | 13.2 | 1.6 | 12.83 | 9.14 |
| LQ site | |||||||||||
| Mean | 5.9 | 271.6 | 35.7 | 5.0 | 2.8 | 1.2 | 11.3 | 8.1 | 204.8 | 0.56 | 0.06 |
| SD | 0.7 | 11.5 | 2.2 | 0.6 | 0.5 | 0.4 | 0.7 | 1.6 | 4.6 | 0.03 | 0.001 |
| Min | 4.4 | 255.1 | 31.9 | 4.2 | 1.8 | 0.7 | 10.4 | 5.4 | 196.3 | 0.44 | 0.04 |
| Max | 6.9 | 296.3 | 38.3 | 6.5 | 3.4 | 1.9 | 12.3 | 10.4 | 210.6 | 0.74 | 0.07 |
| CV (%) | 12.5 | 4.2 | 6.1 | 11.9 | 18.2 | 30.5 | 6.2 | 19.6 | 2.3 | 5.01 | 7.63 |
| HSD site | |||||||||||
| Mean | 6.2 | 198.4 | 36.6 | 5.2 | 2.8 | 1.1 | 11.1 | 3.9 | 132.5 | 0.33 | 0.31 |
| SD | 0.4 | 4.2 | 1.5 | 0.7 | 0.5 | 0.2 | 0.7 | 1.0 | 3.9 | 0.02 | 0.01 |
| Min | 5.6 | 189.3 | 34.1 | 3.6 | 1.9 | 0.9 | 9.4 | 3.0 | 126.5 | 0.29 | 0.29 |
| Max | 6.7 | 204.0 | 38.5 | 6.0 | 3.7 | 1.5 | 12.3 | 5.7 | 138.3 | 0.37 | 0.33 |
| CV (%) | 6.8 | 2.1 | 4.1 | 9.4 | 19.5 | 18.7 | 6.6 | 25.1 | 2.9 | 7.47 | 4.35 |
| ACV (%) | 9.4 | 2.7 | 5.4 | 10.2 | 19.8 | 28.4 | 5.6 | 19.3 | 2.2 | 8.44 | 7.04 |
| Total | 5.9 | 218.9 | 29.3 | 5.8 | 2.9 | 1.2 | 11.6 | 5.5 | 179.8 | 0.44 | 0.16 |
| Class III | 6.5–8.5 | 1000 | 150 | 200 | 250 | 250 | 20 | 1.0 |
JY. Jingyu site; LQ. Longquan site; HSD. Huangsongdian site; CV. Coefficient of variation; ACV. Average CV; Class III. The water used for the second level reserve of groundwater source for drinking in China.
Figure 2Cluster tree and scatter plots and of the 19 groundwater physicochemical indexes showing interrelationships among them.
Pearson correlation coefficients between the affected parameters and distances in groundwater.
| Site | Cu | Pb | Zn | Cd | Cr | Na+ | K+ | Cl− |
|---|---|---|---|---|---|---|---|---|
| JY | −0.698 * | −0.666 * | −0.397 * | −0.822 * | −0.671 * | −0.438 | −0.528 * | −0.407 * |
| LQ | −0.797 ** | −0.871 ** | −0.385 | −0.349 * | −0.554 | −0.541 | −0.606 * | −0.386 |
| HSD | 0.208 | −0.160 | −0.411 * | −0.427 | −0.306 | −0.488 * | −0.476 | −0.450 * |
| Whole | −0.340 * | −0.440 ** | −0.264 * | −0.341 * | −0.416 * | −0.456 ** | −0.484 ** | −0.288 ** |
* Correlation is significant at the 0.05 level (two-tailed); ** Correlation is significant at the 0.01 level (two-tailed).
Figure 3Regression curves of highway-related pollutants concentrations in groundwater in turfy swamp.
The background contents of Cu, Pb, Zn, Cr, Cd, Na+, K+, Cl− in groundwater in different turfy swamp sites.
| Site | Cu | Pb | Zn | Cd | Cr | Na+ | K+ | Cl− |
|---|---|---|---|---|---|---|---|---|
| JY | 43.6 | 18.7 | 94.9 | 1.3 | 3.9 | 2.8 | 1.1 | 4.0 |
| LQ | 46.2 | 17.4 | 110.1 | 1.7 | 6.0 | 2.3 | 0.9 | 7.2 |
| HSD | 20.6 | 16.5 | 85.6 | 1.2 | 5.0 | 2.4 | 1.0 | 3.2 |
Figure 4Relationship between HPI and C values and distance to the highway edge.
Correlation coefficients for the distance and metal concentrations with indices values.
| JY | LQ | HSD | ||||
|---|---|---|---|---|---|---|
| HPI |
| HPI |
| HPI |
| |
| Distance | −0.750 * | −0.739 * | −0.854 ** | −0.868 ** | 0.038 | 0.047 |
| Cu | 0.778 ** | 0.798 ** | 0.912 ** | 0.910 ** | 0.258 | 0.221 |
| Pb | 0.976 ** | 0.976 ** | 0.980 ** | 0.983 ** | 0.599 * | 0.646 * |
| Zn | 0.660 * | 0.666 * | 0.621 * | 0.620 * | 0.213 | 0.338 |
| Cd | 0.718 ** | 0.694 * | 0.642 * | 0.623 * | 0.739 ** | 0.608 * |
| Cr | 0.821 ** | 0.812** | 0.621* | 0.622 * | 0.612 * | 0.715 ** |
| Hg | 0.203 | 0.183 | 0.289 | 0.282 | 0.291 | 0.333 |
| Ni | 0.179 | 0.256 | −0.456 | −0.460 | 0.307 | 0.352 |
| As | 0.049 | 0.082 | −0.128 | −0.140 | 0.513 | 0.562 |
* Correlation is significant at the 0.05 level (two-tailed); ** Correlation is significant at the 0.01 level (two-tailed).