Yao Yu, Li Dujun, Chen Ying, Liu Huaji, Wang Guoxiang, Han Ruiming
School of Environment, Nanjing Normal University, Nanjing, 210023, China; Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing, 210023, China; Jiangsu Engineering Lab of Water and Soil Eco-remediation, Nanjing Normal University, Nanjing, 210023, China.
School of Environment, Nanjing Normal University, Nanjing, 210023, China; Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing, 210023, China; Jiangsu Engineering Lab of Water and Soil Eco-remediation, Nanjing Normal University, Nanjing, 210023, China.
Environ Res. 2021 Oct;201:111525. doi: 10.1016/j.envres.2021.111525. Epub 2021 Jun 27.
The Mechanisms driving phosphorus (P) release in sediment of shallow lakes is essential for managing harmful algal blooms (HABs). Accordingly, this study conducted field monitoring of labile P, iron (Fe), sulfur (S), and dissolved manganese (Mn) in different biomass of algae in Lake Taihu. The in-situ technique of ZrO-Chelex-AgI (ZrO-CA) diffusive gradients in thin-films (DGT) and high-resolution dialysis sampler (high resolution-Peeper (HR-Peeper)) were used to measure labile P, Fe, S, and dissolved Mn, as well as their apparent diffusion fluxes at the sediment-water interface (SWI). In addition, the distribution of iron-reducing bacteria (IRB) and sulfate-reducing bacteria (SRB) in sediments was also detected. Results showed that high HABs biomass promoted the reduction of sulfate into labile S, however, IRB is the dominant species. Thus, labile Fe concentrations greatly exceeded labile S concentrations across all sites, indicating that microbial iron reduction (MIR) is the principal pathway for ferric iron reduction. Furthermore, the simple relationship analysis revealed the principal influence P migration and transformation is the Fe-P in high algal biomass sites, while Fe and Mn redox reactions did not significantly influence labile P mobilization in low algal areas.
驱动浅水湖泊沉积物中磷(P)释放的机制对于管理有害藻华(HABs)至关重要。因此,本研究对太湖不同藻类生物量中的活性磷、铁(Fe)、硫(S)和溶解态锰(Mn)进行了现场监测。采用ZrO-Chelex-AgI(ZrO-CA)薄膜扩散梯度原位技术(DGT)和高分辨率透析采样器(高分辨率-Peeper(HR-Peeper))来测量活性磷、铁、硫和溶解态锰,以及它们在沉积物-水界面(SWI)的表观扩散通量。此外,还检测了沉积物中还原铁细菌(IRB)和硫酸盐还原细菌(SRB)的分布。结果表明,高藻华生物量促进了硫酸盐还原为活性硫,但IRB是优势菌种。因此,所有采样点的活性铁浓度大大超过活性硫浓度,表明微生物铁还原(MIR)是三价铁还原的主要途径。此外,简单的关系分析表明,在高藻类生物量区域,磷迁移和转化的主要影响因素是铁磷,而在低藻类区域,铁和锰的氧化还原反应对活性磷的迁移没有显著影响。