4.7 Article

An investigation of the effects of elevated phosphorus in water on the release of heavy metals in sediments at a high resolution

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 575, Issue -, Pages 330-337

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2016.10.063

Keywords

Diffusive gradients in thin films; Phosphorus; Heavy metals; Precipitation; DGT-induced fluxes in sediments

Funding

  1. National Natural Science Foundation of China [41322011, 51479068, 41571465]
  2. National High-level Personnel of Special Support Program

Ask authors/readers for more resources

Excessive phosphorus (P) input plays an important role on the release of heavy metals in sediments under the eutrophic environment. In this study, a microcosm experiment with 40-day incubation using homogenized sediments was performed to investigate this aspect at a millimeter resolution. Diffusive gradient in thin films (DGT) and dialysis (Peeper) techniqueswere employed to simultaneously measure labile and dissolved P, Pb, Cd, Zn, Co and Ni in sediments at a millimeter scale, respectively. The results showed that an increase of water P from 0.02 mg L-1 to 0.20 and 2.4 mg L-1 generally led to intensified decrease of DGT-labile metals from the 10th to 20th days after the onset of incubation. The decrease in dissolved metals in pore water also appeared on the 20th day. The degree of decrease in the five metals was in the order of Pb > Cd > Zn > Co > Ni, which has a negative correlation with the solubility constants (K-sp) of each metal-P precipitate. This indicated that the negative effect was caused by the precipitation of metal P. On the 40th day during incubation, the concentrations of DGT-labile metals had different increasing pattern compared to those on the 20th day. The extent of metal recovery was positively correlated with the change of desorption rate constant (k(-1)) and negatively correlated with the change in the characteristic time (T-c) to reach equilibrium from DGT perturbation derived from DGT-induced fluxes in sediments (DIFS) modeling. This suggested that the recovery of metal lability from elevated water P was a result of the increased releases of metals from sediment solids. (C) 2016 Elsevier B.V. All rights reserved.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available