首页> 外文期刊>Ecological Modelling >Modelling the relative importance of internal and external nutrient loads on water column nutrient concentrations and phytoplankton biomass in a shallow polymictic lake
【24h】

Modelling the relative importance of internal and external nutrient loads on water column nutrient concentrations and phytoplankton biomass in a shallow polymictic lake

机译:模拟内外养分负荷对浅水多湖湖泊水柱养分浓度和浮游植物生物量的相对重要性

获取原文
获取原文并翻译 | 示例
           

摘要

Lake Rotorua is a large (area 79 km(2)), shallow (mean depth 10.8m), polymictic lake in central North Island, New Zealand. The lake is eutrophic, with a mean external aerial load of 18.5 mg m(-2) d(-1) for total nitrogen and 1.2 mg m(-2) d(-1) for total phosphorus. Blooms of cyanobacteria and occasional anoxia of bottom waters occur during summer (December-March). We used a vertically resolved water quality model, DYRESM - CAEDYM, to examine the relative importance of internal and external nutrient inputs on water column nutrient concentrations and phytoplankton biomass, with particular emphasis on cyanobacteria. External nutrient loads associated with nine major inflows to the lake and three additional inflows representing smaller geothermal and coldwater flows and residual flows, were represented as inputs to the model. Other forcing inputs to the model included local meteorological data, discharge from the only outflow, the Ohau Channel, and measured rates of sediment nutrient release obtained from benthic chamber deployments which were used to prescribe ranges of sediment nutrient release that were simulated dynamically within the model. Profiles of water column nutrient concentrations, surface chlorophyll a concentrations and continuous temperature and dissolved oxygen measurements were used to validate the model. Simulated water column temperature and soluble reactive phosphorus (SRP) and ammonium (NH4) concentrations closely matched field measurements, and captured the timing and duration of stratification events as well as subsequent changes in bottom water nutrient concentrations. Surface water concentrations of chlorophyll a were also similar between simulated and observed data. Model simulations indicate that reductions in sediment nutrient fluxes would be more effective in reducing cyanobacterial biomass than similar proportional reductions in catchment fluxes, due to the coincidence of large sediment nutrient release events with high cyanobacterial biomass. This finding indicates that only a significant and prolonged reduction in external loads, which in turn reduces internal loads, will ultimately reduce cyanobacterial biomass in Lake Rotorua. (c) 2007 Elsevier B.V.. All rights reserved.
机译:罗托鲁瓦湖是一个大型的(面积79 km(2)),浅的(平均深度为10.8m)多色湖,位于新西兰北岛中部。湖泊富营养化,总氮的平均外部空气负荷为18.5 mg m(-2)d(-1),总磷的平均外部空气负荷为1.2 mg m(-2)d(-1)。夏季(12月至3月)会发生蓝藻开花和底部水偶尔缺氧的情况。我们使用垂直解析的水质模型DYRESM-CAEDYM来检查内部和外部养分输入对水柱养分浓度和浮游植物生物量的相对重要性,尤其是蓝藻。该模型的输入表示了与九个主要流入湖泊和三个附加流入(代表较小的地热和冷水流量以及剩余流量)相关的外部养分负荷。该模型的其他强迫输入包括本地气象数据,唯一流出量,奥豪河道的流量以及从底栖腔室部署获得的测得的沉积物养分释放速率,这些速率用于规定模型中动态模拟的沉积物养分释放范围。使用水柱养分浓度,表面叶绿素a浓度以及连续温度和溶解氧的测量值来验证模型。模拟的水柱温度以及可溶性反应性磷(SRP)和铵(NH4)的浓度与现场测量值非常匹配,并捕获了分层事件的时间和持续时间以及底部水营养物浓度的后续变化。在模拟数据和观测数据之间,叶绿素a的地表水浓度也相似。模型模拟表明,由于大的沉积物养分释放事件与高水平的蓝细菌生物量的同时发生,减少沉积物养分通量比减少流域通量的比例减少要更有效地减少蓝藻生物量。这一发现表明,只有外部负荷的显着和长期减少,进而减少内部负荷,才能最终减少罗托鲁瓦湖的蓝藻生物量。 (c)2007 Elsevier B.V.。保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号