| Literature DB >> 35270394 |
Lei Dong1,2,3, Li Lin1,2, Xiong Pan1,2, Sheng Zhang1,2, Zhanao Lv1,2, Changqing Mi1,2.
Abstract
Phthalate esters (PAEs) are endocrine-disrupting chemicals that pose potential risks to human health. Water and sediments are crucial carriers and storage media for the migration and transformation of PAEs. In this study, six congeners of PAEs were measured in water and sediment samples to elucidate their spatial distribution, congener profiles, and ecological risks in the middle-lower Hanjiang River during the wet and dry seasons. The concentration of the Σ6PAEs ranged from 592 to 2.75 × 103 ng/L with an average of 1.47 × 103 ng/L in surface water, while the concentration of the Σ6PAEs ranged from 1.12 × 103 to 6.61 × 103 ng/g with an average of 2.69 × 103 ng/g in sediments. In general, PAE concentrations were ranked as sediment > water, and dry season > wet season. DEHP and DBP were the dominant PAEs in the middle-lower Hanjiang River in surface water and sediments. SPSS analysis showed that dissolved organic carbon (DOC) in surface water was significantly correlated with the concentration of DBP, DEHP, and the ∑6PAEs, while organic matter (OM) was significantly correlated with the concentration of the ∑6PAEs in sediments. The concentrations of PAEs were irregularly distributed and varied significantly in surface water and sediments. Compared with other regions at home and abroad, the pollution levels of surface water and sediments in the middle-lower Hanjiang River were relatively low and not enough to have a negative impact on the local water's ecological environment. However, the supervision of land-based discharge should still be strengthened.Entities:
Keywords: Hanjiang River; distribution; phthalate esters; sediments; suspended sediment; water
Mesh:
Substances:
Year: 2022 PMID: 35270394 PMCID: PMC8910556 DOI: 10.3390/ijerph19052702
Source DB: PubMed Journal: Int J Environ Res Public Health ISSN: 1660-4601 Impact factor: 3.390
Figure 1Map showing sampling sites in the middle-lower Hanjiang River. DJD: Danjiangkou Dam, WPZD: Wangpuzhou Dam, XJD: Xinji Dam, CJYD: Cuijiaying Dam, YKD: Yakou Dam, NRSD: Nianpanshan Dam, XLD: Xinglong Dam.
Geographical information and water quality parameters at the sampling sites from the middle-lower Hanjiang River.
| Station | Sampling Sites | Sampling Position | Parameters (Wet Season/Dry Season) | |||
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| pH | DO (mg/L) | T | ORP (mv) | |||
| S1 | 0.5 km under Danjiangkou Dam | N32°33′24.2”, E111°29′23.9” | 8.30/7.80 | 10.8/10.2 | 26.2/12.8 | 71.6/181 |
| S2 | Danjiangkou urban section | N32°32′1.77”, E111°30′12.9” | 7.60/8.00 | 9.13/10.5 | 22.6/9.80 | 112/197 |
| S3 | Hydrological Station of Huangjiagang | N32°30′14.9”, E111°31′2.5” | 7.81/7.92 | 9.32/10.4 | 23.1/9.41 | 114/148 |
| S4 | Laohekou urban section | N32°21′36.8”, E111°39′46.7” | 7.31/7.91 | 5.02/9.9 | 27.1/11.3 | 147/95.1 |
| S5 | Qing River | N32°3′51.5”, E112°10′15.9” | 6.13/9.60 | 6.21/10.4 | 26.4/10.9 | 122/139 |
| S6 | Tangbai River | N32°4′43.3”, E112°12′42.4” | 6.61/7.70 | 7.50/10.6 | 30.1/8.31 | 87.6/176 |
| S7 | Zhongxiang urban section | N31°11′39.1”, E112°34′27.0” | 8.60/7.91 | 7.92/10.8 | 26.2/10.3 | 117/175 |
| S8 | Zhupi River | N30°53′26.5”, E112°33′1.29” | 8.72/7.54 | 7.91/9.9 | 25.5/7.30 | 124/184 |
| S9 | Downstream of Xinglongba gate | N30°36′38.9”, E112°40′47.0” | 8.22/8.13 | 8.62/11.5 | 25.7/8.72 | 65.3/155 |
| S10 | Qianjiang urban section | N30°30′32.3”, E112°53′9.5” | 8.40/7.90 | 7.52/11.4 | 24.8/8.61 | 56.8/183 |
| S11 | Xiantao urban section | N30°22′46.5”, E113°27′1.26” | 8.21/8.02 | 7.63/11.7 | 25.3/8.20 | 88.6/205 |
| S12 | Hanchuan urban section | N30°38′26.8”, E113°50′38.8” | 7.74/7.92 | 5.71/11.2 | 26.2/9.12 | 46.2/174 |
| S13 | Upstream of Wuhan | N30°35′34.7”, E114°8′51.4” | 7.62/7.83 | 5.11/11.6 | 27.1/7.70 | 45.1/198 |
| S14 | Midstream of Wuhan | N30°34′13.2”, E114°14′34.5” | 7.52/7.84 | 4.83/11.3 | 26.7/8.52 | 63.9/214 |
| S15 | Downstream of Wuhan | N30°33′54.1”, E114°17′21.9” | 7.61/8.13 | 4.74/11.1 | 27.3/8.32 | 40.8/182 |
The concentrations of PAEs in the surface water of the middle-lower Hanjiang River (ng/L).
| PAEs | Wet Season | Dry Season | ||||||
|---|---|---|---|---|---|---|---|---|
| Range | Mean ± SD a | Median | DR b ( | Range | Mean ± SD | Median | DR ( | |
| DMP | 6.20–361 | 45.6 ± 89.2 | 15.5 | 100 | ND–84.4 | 22.7 ± 27.6 | 9.00 | 60.0 |
| DEP | 40.4–423 | 130 ± 96.7 | 103 | 100 | 128–553 | 253 ± 118 | 196 | 100 |
| DBP | 266–1.21 × 103 | 596 ± 282 | 452 | 100 | 567–1.48 × 103 | 1.01 × 103 ± 320.8 | 1.11 × 103 | 100 |
| BBP | ND c–17.4 | 3.70 ± 4.70 | 2.80 | 73.3 | ND–90.6 | 25.9 ± 33.0 | 15.6 | 80.0 |
| DEHP | 85.5–748 | 369 ± 210 | 338 | 100 | 140–861 | 427 ± 206 | 408 | 100 |
| DNOP | ND–36.0 | 13.7 ± 10.2 | 11.3 | 93.3 | ND–162 | 51.3 ± 44.2 | 44.9 | 80.0 |
| ∑6PAEs | 592–2.03 × 103 | 1.16 × 103 ± 451 | 1.15 × 103 | 100 | 1.31 × 103–2.75 × 103 | 1.79 × 103 ± 406.1 | 1.65 × 103 | 100 |
a standard deviation. b detection rate. c concentration was lower than the LOQ.
The sampling sites and concentrations of the middle-lower Hanjiang River.
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| S1 | 6.20 | 40.4 | 266 | 0.90 | 266 | 13.2 | 592 |
| S2 | 22.5 | 104 | 814 | 5.60 | 717 | 18.6 | 1.68 × 103 |
| S3 | 8.40 | 242 | 317 | 0.60 | 97.1 | 9.70 | 675 |
| S4 | 10.2 | 171 | 1.21 × 103 | 17.4 | 615 | 5.80 | 2.03 × 103 |
| S5 | 13.9 | 70.0 | 407 | 0.90 | 152 | 3.90 | 648 |
| S6 | 15.5 | 147 | 878 | ND | 386 | 9.70 | 1.43 × 103 |
| S7 | 11.8 | 108 | 628 | 2.80 | 245 | 12.8 | 1.01 × 103 |
| S8 | 361 | 83.6 | 452 | 8.10 | 338 | 36.0 | 1.28 × 103 |
| S9 | 15.4 | 54.3 | 824 | 7.20 | 748 | 6.50 | 1.66 × 103 |
| S10 | 16.7 | 94.0 | 446 | ND | 265 | 11.3 | 832 |
| S11 | 33.7 | 103 | 406 | ND | 385 | 34.9 | 963 |
| S12 | 27.0 | 78.3 | 1.00 × 103 | 4.20 | 445 | 17.8 | 1.57 × 103 |
| S13 | 59.6 | 423 | 524 | 4.30 | 238 | 16.1 | 1.26 × 103 |
| S14 | 12.8 | 168 | 411 | 4.20 | 548 | ND | 1.15 × 103 |
| S15 | 68.6 | 65.6 | 362 | ND | 85.5 | 10.0 | 592 |
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| S1 | 51.6 | 180 | 1.29 × 103 | 90.6 | 516 | 88.5 | 2.22 × 103 |
| S2 | 9.00 | 196 | 691 | 43.2 | 401 | 35.9 | 1.38 × 103 |
| S3 | ND | 264 | 913 | ND | 271 | 57.2 | 1.51 × 103 |
| S4 | 84.4 | 183 | 615 | ND | 409 | 21.9 | 1.31 × 103 |
| S5 | 33.3 | 372 | 859 | 78.2 | 312 | ND | 1.65 × 103 |
| S6 | ND | 438 | 715 | 5.90 | 140 | 23.0 | 1.32 × 103 |
| S7 | ND | 226 | 1.11 × 103 | 15.6 | 228 | 33.0 | 1.61 × 103 |
| S8 | 42.8 | 128 | 1.35 × 103 | 22.7 | 263 | 44.9 | 1.85 × 103 |
| S9 | 6.70 | 180 | 1.38 × 103 | 87.9 | 461 | 85.2 | 2.20 × 103 |
| S10 | 13.0 | 226 | 1.48 × 103 | 6.00 | 861 | 162 | 2.75 × 103 |
| S11 | ND | 180 | 570 | 16.1 | 731 | 83.9 | 1.58 × 103 |
| S12 | ND | 186 | 579 | 0.30 | 722 | 88.8 | 1.58 × 103 |
| S13 | 64.3 | 171 | 1.25 × 103 | 6.10 | 408 | ND | 1.90 × 103 |
| S14 | 35.8 | 317 | 1.18 × 103 | ND | 258 | ND | 1.79 × 103 |
| S15 | ND | 553 | 1.18 × 103 | 16.0 | 421 | 45.0 | 2.21 × 103 |
Figure 2Distribution and composition of the ∑6PAEs in the surface water of the middle-lower Hanjiang River. (A) distribution of the ∑6PAEs in the wet season; (B) distribution of the ∑6PAEs in the dry season; (C) composition of the ∑6PAEs in the wet season; (D) composition of the ∑6PAEs in the dry season.
PAE concentrations in surface water and sediments from various sites in China and abroad.
| Phase | Locations | Sampling Time | Sites | Numbers | DBP | DEHP | ΣPAEs | Mean of ΣPAEs | Reference |
|---|---|---|---|---|---|---|---|---|---|
| Water (ng/L) | Humber River, UK | 1995–1996 | 6 | — d | — | 740–18.0 × 103 | — | — | (Long et al., 1998) |
| Kaveri River, India | 2012 | 16 | 6 | 250 | 514 | 313–4.64 × 103 | — | (Selvaraj et al., 2015) | |
| Jiangsu section of the Yangtze River | 2004–2005 | 15 | 6 | 105–286 | ND–836 | 178–1.47 × 103 | 902 | (He et al., 2011) | |
| The mid-lower reaches of the Yellow River | 2004 | 12 | 5 | ND–26.0 × 103 | 347–31.8 × 103 | — | — | (Juan et al., 2006) | |
| Jiulong River, China | 2014 | 35 | 6 | 30.0–1.77 × 103 | 6.20 × 103–1.24 × 103 | 3.48 × 103–17.7 × 103 | 6.12 × 103 | (Li et al., 2017) | |
| Songhua River, China | 2011 | 11 | 6 | 1.69 × 103–11.8 × 103 | 2.26 × 103–11.6 × 103 | 9.93 × 103–45.6 × 103 | 19.8 × 103 | (Gao et al., 2014) | |
| Changjiang River Estuary, China | 2015 | 81 | 16 | — | — | 180–3.42 × 103 | 944 | (Zhang et al., 2018) | |
| Three Gorges Reservoir, China | 2015 | 20 | 6 | 12.1–724 | 1.70–394 | 4.00–1.17 × 103 | 398 | (Lin et al., 2018) | |
| Sediment (ng/g) | Humber River, UK | 1995–1996 | 6 | — | — | 840–31.0 × 103 | — | — | (Long et al., 1998) |
| Cochin Estuary, India | 2013 | 15 | 6 | ND–3.65 × 103 | 6.00–349 | 44.0–4.01 × 103 | 2.25 × 103 | (Ramzi et al., 2018) | |
| Changjiang River Estuary, China | 2015 | — | — | 480.0–29.9 × 103 | 12.9 × 103 | (Zhang et al., 2018) | |||
| Songhua River, China | 2017 | 19 | 6 | 1.73 × 103–22.5 × 103 | 4.81 × 103–18.9 × 103 | 6.83 × 103–36.3 × 103 | 18.4 × 103 | (Wang et al., 2020) | |
| Three Gorges Reservoir | 2015 | 20 | 6 | 82.9–4.05 × 103 | 10.9–1.11 × 103 | 177–4.74 × 103 | 2.23 × 103 | (Lin et al., 2018) | |
| Xijiang River, China | 2016 | 12 | 6 | — | — | 21.0–71.0 | — | (Tang et al., 2018) |
d no data.
The concentrations of PAEs in sediments of the middle-lower Hanjiang River (ng/g).
| PAEs | Wet Season | Dry Season | ||||||
|---|---|---|---|---|---|---|---|---|
| Range | Mean ± SD | Median | DR ( | Range | Mean ± SD | Median | DR ( | |
| DMP | 2.30–22.9 | 10.8 ± 4.80 | 11.4 | 100 | 11.9–191 | 49.3 ± 51.9 | 33.4 | 100 |
| DEP | 34.0–368 | 132 ± 84.9 | 107 | 100 | 2.00–620 | 196 ± 1150 | 183 | 100 |
| DBP | 159–2.12 × 103 | 921 ± 506 | 835 | 100 | 400–4.33 × 103 | 2.01 × 103 ± 1.05 × 103 | 1.87 × 103 | 100 |
| BBP | ND–21.1 | 5.40 ± 6.10 | 2.70 | 93.3 | ND–12.8 | 5.90 ± 4.30 | 6.60 | 80.0 |
| DEHP | 580–1.89 × 103 | 1.11 × 103 ± 400 | 1.06 × 103 | 100 | 341–1.41 × 103 | 735 ± 359 | 600 | 100 |
| DNOP | 44.2–417 | 140 ± 126 | 81.3 | 100 | ND–232 | 63.8 ± 72.9 | 34.8 | 80.0 |
| ∑6PAEs | 1226.9–3.38 × 103 | 2.32 × 103 ± 715 | 2.25 × 103 | 100 | 1.12 × 103–6.61 × 103 | 3.06 × 103 ± 1.46 × 103 | 3.05 × 103 | 100 |
Figure 3Distribution and composition of the ∑6PAEs in the sediments of the middle-lower Hanjiang River. (A) distribution of the ∑6PAEs in the wet season; (B) distribution of the ∑6PAEs in the dry season; (C) composition of the ∑6PAEs in the wet season; (D) composition of the ∑6PAEs in the dry season.
Figure A1Concentration distribution trend of the water quality index (WQI) in the wet season from the middle-lower Hanjiang River.
Correlation coefficients between concentrations of PAEs and water quality indexes (WQI) in water samples of the middle-lower Hanjiang River.
| PAEs | TP | CODMn | Chl- | TN | NH4-N | DOC | DBP | DEHP | |
|---|---|---|---|---|---|---|---|---|---|
| PAEs | 1 | ||||||||
| TP | 0.003 | 1 | |||||||
| CODMn | 0.010 | 0.958 ** | 1 | ||||||
| Chl- | 0.127 | 0.747 ** | 0.795 ** | 1 | |||||
| TN | 0.025 | 0.965 ** | 0.922 ** | 0.822 ** | 1 | ||||
| NH4-N | 0.006 | 0.921 ** | 0.846 ** | 0.763 ** | 0.972 ** | 1 | |||
| DOC | 0.814 ** | 0.214 | 0.238 | 0.380 | 0.253 | 0.251 | 1 | ||
| DBP | 0.906 ** | −0.168 | −0.120 | 0.031 | −0.156 | −0.207 | 0.737 ** | 1 | |
| DEHP | 0.835 ** | −0.174 | −0.165 | −0.063 | −0.131 | −0.092 | 0.647 ** | 0.667 ** | 1 |
** Correlation is significant at the 0.01 level (2-tailed).
Figure A2Concentration distribution trend of TN, TP, and organic matter in sediments in the wet season from the middle-lower Hanjiang River.
Correlation coefficients between concentrations of PAEs and water quality indexes (WQI) in sediment samples of the middle-lower Hanjiang River.
| PAEs | OM | TN | TP | DBP | DEHP | |
|---|---|---|---|---|---|---|
| PAEs | 1 | |||||
| OM | 0.700 ** | 1 | ||||
| TN | −0.133 | 0.132 | 1 | |||
| TP | 0.234 | 0.398 | 0.690 ** | 1 | ||
| DBP | 0.768 ** | 0.370 | −0.337 | −0.021 | 1 | |
| DEHP | 0.781 ** | 0.678 ** | −0.185 | 0.159 | 0.273 | 1 |
** Correlation is significant at the 0.01 level (2-tailed).
Figure A3Correlation coefficients between the ∑6PAEs and OM of sediments in the wet season from the middle-lower Hanjiang River.
Figure A4Correlation coefficients between DEHP and OM of sediments in the wet season from the middle-lower Hanjiang River.
AWQC for human health set by the USEPA for PAEs (μg/L).
| PAEs | Human Health AQQC for | This Study | ||
|---|---|---|---|---|
| The Consumption of Water + Organism | The Consumption of | (Wet Season) × 10−3 | (Dry Season) × 10−3 | |
| DMP | 2.00 × 103 | 2.00 × 103 | 6.20–361 (mean 45.6) | ND-84.4 (mean 22.7) |
| DEP | 600 | 600 | 40.4–422 (mean 130) | 128-553 (mean 253) |
| DBP | 20.0 | 30.0 | 266–1.21 × 103 (mean 596) | 570-1.48 × 103 (mean 1.01 × 103) |
| BBP | 0.100 | 0.100 | ND-17.4 (mean 3.70) | ND-90.6 (mean 25.9) |
| DEHP | 0.320 | 0.370 | 85.5–748 (mean 369) | 140-861 (mean 427) |
Annual average hydrological parameters at the Huangzhuang hydrological stations in the middle-lower Hanjiang River.
| Period | Runoff | SS Load | SS Concentration | SS Grain Size |
|---|---|---|---|---|
| 1950–2010 | 475 | 0.477 | 1.00 | 52.0 |
| 2011 | 513 | 0.0540 | 0.104 | 38.0 |
| 2012 | 433 | 0.0370 | 0.0850 | 44.0 |
| 2013 | 326 | 0.0150 | 0.0470 | 27.0 |
| 2014 | 215 | 0.00700 | 0.0340 | 22.0 |
| 2015 | 364 | 0.0170 | 0.0480 | 51.0 |
| 2016 | 242 | 0.0130 | 0.0550 | 19.0 |
| 2017 | 446 | 0.0610 | 0.138 | 19.0 |
| 2018 | 380 | 0.0200 | 0.0520 | 25.0 |