4.5 Article

Combined use of high-resolution dialysis, diffusive gradient in thin films (DGT) technique, and conventional methods to assess trace metals in reservoir sediments

Journal

ENVIRONMENTAL MONITORING AND ASSESSMENT
Volume 193, Issue 8, Pages -

Publisher

SPRINGER
DOI: 10.1007/s10661-021-09247-z

Keywords

Sediment; water interaction; Black precipitate; Ecological risk assessment; Water quality

Funding

  1. National Key Research and Development Program of China [2017YFC0405203, 2016YFC0401703]
  2. National Science Foundation of China [52039003, 51779072, 51809102]
  3. Major Science and Technology Program for Water Pollution Control and Treatment [2017ZX07204003]

Ask authors/readers for more resources

The study revealed that the black water events in Tianbao reservoir were mainly caused by high concentrations of TFe, Mn, and P in the sediments, as well as high organic matter from Eucalyptus plantation surrounding the reservoir and strong thermal stratification leading to hypoxia in the hypolimnion. The movement of Fe2+, Mn2+, S2-, P, and DOC at the water-sediment boundary due to their redox interactions resulted in the production of black substances in the hypolimnion, contributing to the phenomenon of black water reservoir.
Recently, reservoirs in southern China are witnessing incidents involving black water, which are harmful to the aquatic ecosystem. This study unravels the cause of the black water events by studying the occurrence and the ecological risks of contaminants (Pb, Cu, Cd, Zn, Ni, TFe, Mn, S, P, and DOC) in sediments of Tianbao reservoir. Due to the significantly high concentration of TFe, Mn, and P in the sediments, the study further used the thin film diffusion gradient (DGT) technology and high-resolution dialysis method to investigate the movement of Fe2+, Mn2+, S2-, and reactive P within the sediments. The ecological risk assessment (threshold effect level and probable effect level) showed that the sediments had a low concentration of Pb, Cu, Cd, Zn, and Ni. High organic matter from the Eucalyptus plantation surrounding the reservoir, as well as the intense thermal stratification of the reservoir, caused the hypolimnion to be hypoxic (DO < 2 mg/L). The diffusion fluxes at the water-sediment boundary (WSB) demonstrated a significant movement of Fe2+, Mn2+, and PO43- from the sediments into the overlying water, while the movement of S2- was in both directions due to hypoxia. A high correlation Fe-DOC (r = 0.9), Fe-S (r = 0.8), and Mn-S (r = 0.7) and the redox interaction of Fe2+, Mn2+, S2-, P, and DOC at the hypoxic WSB caused the production of black substances in the hypolimnion contributing to the so-called black water reservoir.

Authors

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

Reviews

Primary Rating

4.5
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available