Key Laboratory of Algal Biology, Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan 430072, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Key Laboratory of Algal Biology, Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan 430072, China; University of Chinese Academy of Sciences, Beijing 100049, China.
J Environ Manage. 2024 Oct;369:122295. doi: 10.1016/j.jenvman.2024.122295. Epub 2024 Aug 30.
Global climate warming and human activities have increased the magnitude and frequency of Microcystis surface blooms, posing significant threats to freshwater ecosystems and human health over recent decades. Heavy rainfall events have been reported to cause the disappearance of these blooms. Although some studies have employed turbulence models to analyze the movement characteristics of Microcystis colonies, the impact of rainfall is complex, comprehensive investigations on their vertical migration induced by short-term rainfall are still necessary. Utilizing monitoring data from eutrophic ponds and controlled simulation experiments, this study examines the short-term impacts of rainfall on the vertical distribution of Microcystis in the water column. Our findings indicate that rainfall contributes to the disappearance of Microcystis blooms by reducing the quantity of small to medium-sized colonies (0-100 μm) at the surface, subsequently decreasing the overall Microcystis biomass. As rainfall intensity increases, larger colonies migrate deeper into the water column. At a rainfall threshold of 666 mm, the difference in the median volume diameter (DV50) of Microcystis colonies between the surface and bottom reaches a minimal value of 3.09%. Post-rainfall, these colonies rapidly ascend, aggregate into larger formations, and re-establish surface blooms. The greater the rainfall, the smaller the resultant Microcystis biomass, albeit with larger aggregated colony sizes. When rainfall exceeds 222 mm, the recovery rate of surface Microcystis biomass remains below 100%, decreasing to 19.48% at 666 mm of rainfall, while the median volume diameter (DV50) of the colonies increases to 139.07% of its pre-rainfall level. Furthermore, compared to pre-rainfall conditions, the photosynthetic activity of the surface Microcystis colonies was enhanced and the secretion of EPS was increased under heavy rainfall conditions. Our results identify a critical response time of 30 min for Microcystis colonies to rainfall, after which the response ceases to intensify. These insights are crucial for predicting post-rain Microcystis bloom dynamics and aiding management authorities in timely interventions.
全球气候变暖及人类活动加剧了微囊藻水华的暴发规模和频率,近几十年来对淡水生态系统和人类健康构成了重大威胁。强降雨事件已被报道可导致水华的消失。尽管一些研究采用了紊流模型来分析微囊藻聚集体的运动特征,但降雨的影响较为复杂,因此仍有必要对其在短期降雨条件下的垂直迁移进行综合研究。本研究利用富营养化池塘的监测数据和控制模拟实验,考察了降雨对水柱中微囊藻垂直分布的短期影响。结果表明,降雨通过减少水面中小型微囊藻聚集体(0-100μm)的数量,从而降低整体微囊藻生物量,导致微囊藻水华的消失。随着降雨强度的增加,较大的聚集体向水柱深处迁移。在降雨量阈值为 666mm 时,微囊藻聚集体表面和底部的中值体积直径(DV50)差异达到最小值 3.09%。降雨后,这些聚集体迅速上升,聚集形成更大的聚集体并重新形成水华。降雨量越大,形成的微囊藻生物量越小,尽管聚集体的尺寸更大。当降雨量超过 222mm 时,水面微囊藻生物量的恢复率仍低于 100%,在降雨量为 666mm 时降至 19.48%,而聚集体的中值体积直径(DV50)增加到降雨前的 139.07%。此外,与降雨前相比,在强降雨条件下,表面微囊藻聚集体的光合作用增强,EPS 的分泌增加。本研究确定了微囊藻聚集体对降雨的关键响应时间为 30min,之后响应不再加剧。这些结果对于预测降雨后微囊藻水华动态和帮助管理部门及时干预具有重要意义。