Burial of microplastics in freshwater sediments facilitated by iron-organo flocs

Microplastics are ubiquitous in standing freshwater bodies, consequently lakes and reservoirs may be important sinks for these contaminants. However, the mechanisms governing the deposition of microplastics and their interactions with the sediments are understudied. We demonstrate how aggregation-based transport facilitates the sinking and infiltration of buoyant microplastics into freshwater reservoir sediments by employing experiments with intact sediment cores. Buoyant polyethylene microplastics were rapidly (1–4 h) incorporated into sinking iron-organic aggregates, followed by swift deposition into sediments. Ingression of microplastic bearing flocs into sediments was completed within 6 days and led to stable deposition of the incorporated particles for at least 2 months. Most microplastics were deposited in the top 2 cm of the sediments and few particles (5–15%) were re-released into the water. Our results show at least 85% burial of microplastics, indicating the significant role of freshwaters with low flow velocities in reducing microplastic loads to the oceans.

Investigating the toxicity of tropical reservoir sediments using the Allium test

Water pollution is a global environmental issue, and aquatic sediments are important compartments that might act as sinks or sources of contaminants. Once in the environment, inorganic contaminants such as metals can cause cytogenotoxic effects that damage genetic material and harm the aquatic community. Biological assays such as the Allium test can be used to investigate potential cytogenotoxicity of contaminated sediments based on the alterations of cell cycle indexes and chromosomal aberration frequencies. Therefore, we aimed to assess the toxicity of sediments from four Brazilian reservoirs using the Allium test. Sediments were sampled and elutriates were prepared in a simulating sediment resuspension in the water column. The Allium test was applied to the elutriates, and the metals copper, chromium, cadmium, lead, zinc, and iron were quantified. The elutriates derived from reservoir sediments were able to reduce the mitotic and anaphase index, increase the prophase and metaphase index, and boost chromosomal aberrations compared to the negative control. The cytogenotoxic effects observed may be linked to the presence of copper, zinc, and iron. Therefore, our results showed that the Allium test was a sensitive tool for warning the occurrence of genotoxic contaminants in sediment elutriates from four Brazilian reservoirs.

The Impact of Cascade Large Deep Reservoir on the Migration and Deposition of Cadmium in Lancang River

Metal pollution is a global environmental problem. In order to understand the effects of the cascade hydropower development on Cd in reservoir sediments, this study investigated the migration and deposition mechanisms of Cd in reservoir sediments by using the film diffusion gradient technique (DGT) for the cascade large deep reservoirs of the Lancang River (LCR), Nuozhadu (NZD) and Xiaowan (XW). The results show that: (1) Strong correlations amongst the deposition processes of Cd, Mn and S were found in the sediments of the NZD reservoir; weak correlations between the deposition processes of Cd and Mn were found in the sediments of the XW reservoir. (2) Part of labile Cd in the pore water of the NZD reservoir was supplemented by silt and sand, and another part was inherent in the pore water; most of labile Cd in the pore water of the XW reservoir was inherent in the pore water, and minimal replenishment of sediment was noted. (3) Mn is the main factor controlling the migration of Cd in the NZD reservoir. This paper provides an effective resource for understanding the migration and deposition of Cd in the sediments of large deep reservoirs along the LCR.

Post-depositional alteration of stable isotope signals by preferential degradation of algae-derived organic matter in reservoir sediments

Post-depositional degradation of organic matter (OM) in freshwater sediments is crucial for driving the biogeochemical dynamics and influencing the consequential carbon burial. This process also often causes diagenetic alterations on paleoenvironmental proxies. Yet, mechanisms behind the degradation of sedimentary OM and the depth-related variations in stable isotope ratios can only be explained in part. Degradation of sedimentary OM in two drinking water reservoirs with contrasting trophic states (eutrophic versus mesotrophic) and catchment land-use (agriculture versus forestry) were studied with a combination of typical chemical treatments to group sedimentary organic matter into four different biochemical fractions, i.e., carbohydrates, proteins, lignins and lipids. Our results show that the degradation of sedimentary OM was mainly driven by preferential degradation of aquatic proteins and carbohydrates. In a subsequent step, lipids seemed to be degraded. This process entails more pronounced reduction of sedimentary OM and associated depth variations in δ13C and δ15N in the eutrophic reservoir of agricultural catchment, when compared to the mesotrophic reservoir with a forest dominated catchment. Moreover, changes in the relative proportions of biochemical components in sedimentary OM have more pronounced impact on δ15N isotope values relative to the ones of δ13C. Our findings also suggest that algae-derived OM is primarily responsible for the post-depositional alterations of elemental and isotopic compositions of sedimentary OM. This may be of importance for estimates of carbon sinks in lakes and reservoirs.