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Factors influencing cyanobacteria blooms: review of the historical monitoring data to assess management options for Lake Horowhenua

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DataCite Commons2024-02-18 更新2024-07-29 收录
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https://tandf.figshare.com/articles/dataset/Factors_influencing_cyanobacteria_blooms_review_of_the_historical_monitoring_data_to_assess_management_options_for_Lake_Horowhenua/20478736
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Factors influencing cyanobacterial blooms in Lake Horowhenua, Aotearoa/New Zealand, have been deduced from over 40 yrs routine monitoring data, detailed studies and high frequency (15-min interval) data from an in-lake monitoring buoy. Lake Horowhenua is currently hypertrophic but flips between a winter clear-water, macrophyte dominated phase (<i>Potamogeton crispus),</i> and a turbid phytoplankton dominated phase with substantial cyanobacterial (<i>Microcystis sp.</i>) blooms from mid-summer to autumn. Nitrogen for growth comes from agriculture and horticulture via groundwater and spring-fed streams. Phosphorus is released from the sediment when the weed beds die back. These nutrients stimulate the growth of <i>Microcystis sp.</i>, until the water temperature falls below 15°C. <i>Microcystis sp</i> can raise the pH to over 10, which releases P from the sediment, sustaining its growth. High pH transforms non-toxic ammonium-N released from the sediment to toxic unionised NH<sub>3</sub>, which may contribute to fish kills in summer/autumn. Management strategies cannot use P-inactivation agents for cultural reasons and eradicating the macrophyte beds by spraying would cause the lake to permanently flip to a turbid state. Management of the macrophyte beds with a weed harvester is being trialled to allow a gradual replacement of <i>P. crispus</i> with indigenous species from the seed bank in the sediment.

本研究基于新西兰奥特亚罗瓦地区霍罗温湖(Lake Horowhenua)逾40年的常规监测数据、专项研究成果,以及湖内监测浮标采集的高频(15分钟间隔)监测数据,推导得出影响该湖蓝藻水华的相关因素。霍罗温湖目前处于重度富营养状态,其生态状态在两种模式间切换:冬季为清水态,以大型水生植物菹草(*Potamogeton crispus*)占优;仲夏至秋季则转为浊水态,浮游植物占主导,伴随大规模蓝藻(微囊藻属,*Microcystis sp.*)水华暴发。微囊藻生长所需的氮素来源于农业与园艺活动产生的面源污染,经地下水及泉水补给溪流输入湖体;当菹草群落衰亡时,沉积物会释放磷营养盐。上述营养盐会促进微囊藻属物种增殖,直至水体水温降至15℃以下。微囊藻属物种可将水体pH提升至10以上,进而诱导沉积物再次释放磷素,维持自身种群生长。高pH环境会将沉积物释放的无毒氨氮(ammonium-N)转化为有毒非离子氨(unionised NH₃),这可能引发夏秋季鱼类大规模死亡。受文化因素限制,当地治理方案无法采用磷钝化剂(P-inactivation agents);且通过喷洒药剂清除大型水生植物床群,会导致霍罗温湖永久转为浊水态。当前正试点采用水草收割机治理大型水生植物床群,以期借助沉积物种子库中的本土物种逐步替代菹草(*P. crispus*)。
提供机构:
Taylor & Francis
创建时间:
2022-08-12
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