Nanjing University of Finance & Economics, Institute of Innovation & Entrepreneurship, Nanjing, 210023, PR China; Key Laboratory of Watershed Geographic Sciences, Nanjing Institute of Geography & Limnology, Chinese Academy of Sciences, Nanjing, 210008, PR China.
College of Oceanography, Hohai University, Nanjing, Jiangsu, 210098, PR China.
J Environ Manage. 2021 Sep 15;294:112930. doi: 10.1016/j.jenvman.2021.112930. Epub 2021 Jun 9.
The interplay between hydrological and biogeochemical processes in riparian wetland was recognized to lead directly to the temporal variations of surface water quality. However, the effects of flooding and vegetation on the release and entrapment of heavy metals and nutrients in riparian wetland remain poorly understood. The study aimed at investigating the influences of flooding and vegetation on the hydrochemical and Fe-redox change in the soil porewater and shallow groundwater, in Poyang lake riparian wetland through hydrochemical monitoring and diffusive gradient technology (DGT). The hydrochemical profiles and results of PCA analysis on the temporal datasets both demonstrated that vegetation had significant influences on the hydrochemistry of rhizosphere depth zone (RDZ) and shallow groundwater depth zone (SGZ). The Ca, K, Na, Mg, Mn and DOC at RDZ of both plants showed significant increasing trends from pre-to post-flooding while were observed minor change at the SGZ. The extracted PC1-PC3 from PCA analysis suggested that mineral dissolution and fermentation were dominating processes that explained 64.1% of the hydrochemical variability under the wetting-drying cycle. The synchronous changes of Fe(II), SO, DOC and ORP were found to occur at the SGZ of Carex, implying the likely occurrence of Fe- and S- redox reactions. The Fe(II) DGT profiles evidenced the temporal iron reduction and oxidation occurring at the rhizosphere following the wetting-drying cycle, as also reflected by the high opposite Fe and DO association through PCA analysis. The high resolution temporal-spatial Fe(II) distribution suggested also the interface between lake water and groundwater was relatively stable under flooding. These results highlight that the release of dissolved Fe(II) from the wetland rhizosphere driven by flood may result in the release of Fe-associated heavy metals from riparian wetland to surface water, and hence pose potential threats to the surface water quality. Thereby, the flow and flood should be properly controlled and vegetation effects need to be carefully considered in the water resources management of lake-floodplain system.
河岸湿地水文和生物地球化学过程的相互作用直接导致了地表水水质的时间变化。然而,洪水和植被对河岸湿地中重金属和养分的释放和截留的影响仍知之甚少。本研究旨在通过水化学监测和扩散梯度技术(DGT)研究洪水和植被对鄱阳湖河岸湿地土壤孔隙水和浅层地下水水化学和 Fe 氧化还原变化的影响。水化学剖面和时间数据集的 PCA 分析结果均表明,植被对根际带(RDZ)和浅层地下水带(SGZ)的水化学有显著影响。植物 RDZ 中的 Ca、K、Na、Mg、Mn 和 DOC 在洪水前后均表现出显著的增加趋势,而 SGZ 则变化较小。PCA 分析提取的 PC1-PC3 表明,在干湿循环过程中,矿物溶解和发酵是解释水化学变异性的主要过程,占 64.1%。在莎草 SGZ 中发现 Fe(II)、SO42-、DOC 和 ORP 同步变化,表明可能发生 Fe 和 S 氧化还原反应。Fe(II)DGT 剖面表明,随着干湿循环的进行,根际发生了铁的还原和氧化,PCA 分析也反映了 Fe 和 DO 之间的高反相关关系。高分辨率的时空 Fe(II)分布也表明,在洪水期间,湖水和地下水之间的界面相对稳定。这些结果表明,洪水驱动的湿地根际溶解 Fe(II)的释放可能导致河岸湿地中与 Fe 相关的重金属向地表水释放,从而对地表水水质构成潜在威胁。因此,在湖泊-洪泛平原系统的水资源管理中,应适当控制水流和洪水,并仔细考虑植被的影响。