| Literature DB >> 34343201 |
Zeinah Elhaj Baddar1, Erin Peck1, Xiaoyu Xu1.
Abstract
The objective of this study was to explore the effects of time, seasons, and total carbon (TC) on Copper (Cu) and Zinc (Zn) deposition in the surface sediments. This study was performed at the H-02 constructed wetland on the Savannah River Site (Aiken, SC, USA). Covering both warm (April-September) and cool (October-March) seasons, several sediment cores were collected twice a year from the H-02 constructed wetland cells from 2007 to 2013. Total concentrations of Cu and Zn were measured in the sediments. Concentrations of Cu and Zn (mean ± standard deviation) in the surface sediments over 7 years of operation increased from 6.0 ± 2.8 and 14.6 ± 4.5 mg kg-1 to 139.6 ± 87.7 and 279.3 ± 202.9 mg kg-1 dry weight, respectively. The linear regression model explained the behavior and the variability of Cu deposition in the sediments. On the other hand, using the generalized least squares extension with the linear regression model allowed for unequal variance and thus produced a model that explained the variance properly, and as a result, was more successful in explaining the pattern of Zn deposition. Total carbon significantly affected both Cu (p = 0.047) and Zn (p < 0.001). Time effect on Cu deposition was statistically significant (p = 0.013), whereas Zn was significantly affected by the season (p = 0.009).Entities:
Year: 2021 PMID: 34343201 PMCID: PMC8330884 DOI: 10.1371/journal.pone.0255527
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.240
Concentration of Cu and Zn in the surface sediment averaged by year, data presented as mean concentration ± standard deviation and (minimum—maximum) concentrations (mg kg-1 dry sediment).
| Year | Total Cu (mg kg-1) | Total Zn (mg kg-1) |
|---|---|---|
| 2007 | 6.0 ± 2.8 (4.0–8.0) | 14.6 ± 4.5 (11.4–17.7) |
| 2008 | 18.5 ± 13.2 (6.0–32.2) | 34.3 ± 18.9 (14.0–51.4) |
| 2009 | 119.9 ± 139.9 (4.4–349.9) | 177.2 ± 186.2 (7.8–4635) |
| 2010 | 50.2 ± 28.2 (11.7–85.3) | 90.6 ± 52.0 (23.6–170.3) |
| 2011 | 43.7 ± 23.4 (19.8–93.1) | 62.6 ± 33.9 (4.0–106.2) |
| 2012 | 129.7 ± 61.1 (27.0–195.9) | 204.4 ± 96.0 (43.6–296.2) |
| 2013 | 139.6 ± 87.7 (33.5–274.2) | 279.3 ± 202.9 (60.5–674.4) |
For year 2007, n = 2, 2008, n = 3, 2009, n = 5, and for years 2010–2013, n = 8.
Model parameters for Cu and Zn.
| Metal | Model | Random term/variance covariate structure | Fixed term ( | Coefficient | |
|---|---|---|---|---|---|
| Cu | lm | Cu | Intercept | 226.5 | 0.013 |
| Year | 0.11 | 0.013 | |||
| Log10TC | 258.30 | 0.047 | |||
| Year: Log10TC | -0.13 | 0.048 | |||
| Zn | gls | VarIdent (Year) | Intercept | 1.51 | <0.001 |
| VarIdent (Season) | Season/Cool | -0.17 | 0.0093 | ||
| VarFixed (Log10TC) | Log10TC | 1.04 | <0.001 |
lm: Linear model, gls: Linear model with generalized least squares extension.
Fig 1Relationship between log10TC and log10Cu.
Fig 2Conditioning plot showing the pattern of log10Cu deposition in surface sediments (mg kg-1) throughout the years 2007–2013 in the warm vs the cool seasons.
Fig 3The effect of the interaction between year and log10TC on log10Cu.
Fig 4Relationship between log10TC and log10Zn.
Fig 5Conditioning plot showing the pattern of log10Zn deposition in surface sediments (mg kg-1) throughout the years 2007–2013 in the warm vs the cool seasons.