College of Environmental Sciences and Engineering, State Environmental Protection Key Laboratory of All Materials Flux in Rivers, Peking University, Beijing 100871, China; National Engineering Laboratory for Lake Pollution Control and Ecological Restoration, Chinese Research Academy of Environmental Sciences, Beijing 100012, China.
College of Environmental Sciences and Engineering, State Environmental Protection Key Laboratory of All Materials Flux in Rivers, Peking University, Beijing 100871, China.
Water Res. 2022 Jun 1;216:118350. doi: 10.1016/j.watres.2022.118350. Epub 2022 Mar 22.
How to maintain harmful algal blooms under phosphate-limitation is still an open question in mesotrophic/eutrophic lakes. Little evidence for the importance of suspended particulate matter (SPM) in mediating phosphorus cycling and contributing to eutrophication has been generated for aquatic ecosystems, especially in coupled river-lake systems. In this study, we examined phosphorus transport and redistribution in a river-lake system in the Lake Erhai basin by establishing the relations between phosphorus distribution and phosphorus sorption behavior on SPM, and predicted how changes in the quality and quantity of SPM might influence phosphorus cycling by laboratory experiments and modeling. During the wet seasons, TP pool shifted from being dominated by total dissolved phosphorus (TDP) in the Miju River and estuary regions (73±5%) to being dominated by total particulate phosphorus (TPP) (74±11%) in Lake Erhai. The detritus-SPM in the Miju River as a P-sink and phytoplankton-SPM in Lake Erhai as a P-source buffered TDP levels during the wet seasons, which attributed to P activity and phytoplankton-POC of SPM. Increasing SPM concentrations could enhance the P-buffering. When C ≤ 5 μmol/L and phytoplankton-SPM ≥ 16 mg/L, P release increased by 50%-300%; when C ≥ 5 μmol/L and detritus-SPM ≥ 16 mg/L, P removal could exceed 30%. This study highlights two distinctive roles of SPM in regulating P cycling during transport from rivers to lakes. Especially the phytoplankton-SPM to buffer phosphate-limitation during algal blooms should not be ignored, which could provide theoretical references for the mechanism of continued algal blooms in mesotrophic lakes.
在富营养化湖泊中,如何在磷限制条件下维持有害藻类水华仍然是一个悬而未决的问题。水生生态系统,特别是在河流-湖泊耦合系统中,很少有证据表明悬浮颗粒物(SPM)在介导磷循环和导致富营养化方面的重要性。在这项研究中,我们通过建立磷分布与 SPM 磷吸附行为之间的关系,研究了洱海流域河流-湖泊系统中的磷输运和再分配,并通过实验室实验和模拟预测了 SPM 质量和数量的变化如何影响磷循环。在雨季,TP 库从弥苴河和河口地区以总溶解磷(TDP)为主(73±5%)转变为以总颗粒磷(TPP)为主(74±11%)。弥苴河中碎屑-SPM 作为 P 汇和洱海浮游植物-SPM 作为 P 源,缓冲了雨季 TDP 水平,这归因于 SPM 的磷活性和浮游植物-POC。增加 SPM 浓度可以增强 P 缓冲能力。当 C ≤ 5 μmol/L 且浮游植物-SPM ≥ 16 mg/L 时,P 释放增加 50%-300%;当 C ≥ 5 μmol/L 且碎屑-SPM ≥ 16 mg/L 时,P 去除率可超过 30%。本研究强调了 SPM 在调节从河流到湖泊的输运过程中磷循环的两个独特作用。特别是在藻类水华期间,浮游植物-SPM 对缓冲磷酸盐限制的作用不容忽视,这可为富营养化湖泊中藻类持续水华的机制提供理论参考。