Effect of different irrigation methods on the toxicity and bioavailability of microcystin-LR to lettuce and carrot.

The use of cyanobacteria-polluted water for irrigation has become an increasing concern due to the potential contamination of microcystins (MCs). However, the effects of MCs on plant performance and food safety under different irrigation methods are not well understood. In this study, we investigated the effects of microcystin-LR (MC-LR) on the growth, food quality, and safety of lettuce and carrot using four irrigation methods (spray irrigation and three types of drip irrigation with different distances from the plant stem). Our results showed that exposure to 10 µg L-1 MC-LR negatively affected plant growth and food quality in treatments with spray irrigation (TS) and drip irrigation directly to the stem (TD0), but not in treatments with drip irrigation away from the plant stem (TD10 and TD20). Using soil as a filtration system, the bioavailability of MC-LR in soil was reduced in TD10 and TD20, resulting in less bioaccumulation in plant edible tissues. The estimated daily intake (EDI) values of TS and TD0 in both lettuce and carrot cultivation exceeded the tolerable daily intake (TDI) limit proposed by WHO, whereas the EDI values of TD10 and TD20 could be effectively reduced below the TDI limit. This study highlights the importance of drip irrigation away from the plant stem as a practical measure to mitigate the effects of cyanobacteria-polluted water in agricultural production.

Using soil amendments to reduce microcystin-LR bioaccumulation in lettuce.

Contamination of microcystins (MCs) in plant-soil system have become a serious problem worldwide, however, it remains largely unknown how to alleviate the potential risk of consuming MCs-contaminated plants. In the present study, attapulgite, biochar and peat were used as soil amendments to reduce MCs bioaccumulation in lettuce. Lettuce irrigated with 10 µg L-1 microcystin-LR (MC-LR) were growing in two different kinds of soils with or without soil amendments. Results showed that all soil amendments effectively reduced MC-LR bioaccumulation in lettuce roots and leaves. Compared with the control treatment, the MC-LR concentrations in leaves in treatments with attapulgite, biochar and peat decreased by 41.5%, 30.6%, 57.0% in soil A and 38.9%, 43.2%, 54.7% in soil B, respectively. Peat application was most effective in reducing MC-LR bioaccumulation. The decreased soil free MC-LR concentrations were positively correlated with MC-LR concentrations in lettuce, indicating decreased bioavailability of MC-LR by soil amendments. It is noteworthy that soil total MC-LR concentration in peat treatment significantly decreased by 33.3% and 29.4% in soil A and soil B, respectively, compared with the controls. According to the results from high-throughput sequencing, peat amendment increased the α-diversity of soil bacterial community and boosted the abundance of Sphingomonas and Methylobacillus (dozens of MC-degrading bacteria belong to these genera). This was in line with the results of soil total MC-LR concentration. It can be speculated that peat application directly and/or indirectly promoted microbial degradation of MC-LR in soils. This work proposed an effective way to alleviate the potential risks of MCs contamination in plant-soil system.

Behavior and fate of microcystin-LR in soils amended with biochar and peat.

Activities such as irrigation with cyanobacteria-polluted water can lead to microcystins (MCs) migration from soil surface to the deeper layers, which could pose a potential risk to ground drinking water safety. The present study evaluated the sorption, degradation and leaching behavior of microcystin-LR (MC-LR) in two different soils amended with biochar and peat. Results showed that both biochar and peat could significantly increase MC-LR sorption in both soils. The Freundlich unit capacity coefficient (Kf) of 2% biochar treatment were 2-3 times higher than those of the control treatment. Amendment of 2% peat greatly boosted the biodegradation of MC-LR, whereas amendment of 2% biochar significantly reduced the biodegradation of MC-LR in both soils. The half-lives of MC-LR were 4.99 d (Control), 5.59 d (2% Biochar) and 3.50 d (2% Peat) in soil A and 6.66 d (Control), 6.93 d (2% Biochar) and 5.13 d (2% Peat) in soil B, respectively. All the amendments, except treatment 1% Peat, could significantly reduce the recovery rates of MC-LR in the leachate of columns with both soils. Amendment of 2% biochar and 2% peat reduced the recovery rates of MC-LR by 15.87% and 8.6% in soil A and 18.4% and 10.3% in soil B, compared with the controls. This work provides a better understanding of the environmental behavior of MC-LR in soils with different amendments, which is also meaningful for groundwater protection in cyanobacterial-polluted areas.

Effects of hydrodynamics processes on phosphorus fluxes from sediment in large, shallow Taihu Lake.

The turnover of phosphorus (P) in lake sediments, a major cause of eutrophication and subsequent deterioration of water quality, is in need of deep understanding. In this study, effects of resuspension on P release were studied in cylindrical microcosms with Y-shape apparatus. The results indicated that there was a positive correlation between flux of suspended substance across sediment-water interface (F(SS)) and the wind speed, and an increasing F(SS) during each wind process followed by a steady state. The maximal F(SS) under light, moderate, and strong wind conditions were 299.9 +/- 41.1, 573.4 +/- 61.7, and 2093.8 +/- 215.7 g/m2, respectively. However, flux of P across sediment-water interface (F(P)) did not follow a similar pattern as F(SS) responding to wind intensity, which increased and reached the maximum in initial 120 min for light wind, then decreased gradually, with maximal flux of 9.4 +/- 1.9 mg/m2. A rapid increase of F(P) at the first 30 min was observed under moderate wind, with maximal flux of 11.2 +/- 0.6 mg/m2. Surprisingly, strong wind caused less F(P) than under light and moderate wind conditions with maximal flux of 3.5 +/- 0.9 mg/m2. F(SS) in water column declined obviously during the sedimentation process after winds, but F(P) varied with wind regime. No obvious difference was detected on F(P) after 8 h sedimentation process, compared with the initial value, which means little redundant P left in the water column after winds.

[Effects of sediment resuspension on aqueous nutrient loading in grass type zone of Lake Taihu].

Internal nutrient loading caused by sediment resuspension is becoming a key issue in studying water eutrophication of shallow lakes. A Y-shape apparatus was used to simulate sediment resuspension and sedimentation process under hydrodynamic conditions in situ in grass type zone of Lake Taihu, and effects on aqueous nutrient loading were investigated. The results indicated that, in the light and moderate wind processes, content of ammonia nitrogen and phosphate had remarkably reduced with the increase of the amount of suspended sediments in water column, with the maximal change of -0.140 g x m(-2) and -1.59 mg x m(-2) at the sediment-water interface for the two nutrients respectively, and in the strong wind process, concentration of aqueous phosphate had a significant increase, with the maximal flux of 0.81 mg x m(-2) at the sediment-water interface, while concentration of aqueous ammonia nitrogen showed a small decrease. And in the later sedimentation process after wind, content of aqueous ammonia nitrogen was lower than that before the light and moderate wind processes, but approximated to that before the strong wind process. Content of aqueous phosphate was close to that before the light and moderate wind processes, but had a marked increase compared to that before the strong wind condition, with the maximal increment of 1.36 mg x m(-2). Consequently, sediment resuspension and sedimentation processes impact nutrients loading of overlaying water evidently. Comparison of the results with those from non-grass type zone in Lake Taihu illustrates that the presence of aquatic macrophytes played some roles in reducing the release of nutrients during the sediment resuspension process.