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Sediment phosphorus release during stratification in polymictic Lake Rotorua, New Zealand

机译:新西兰罗托鲁瓦多层次湖分层过程中沉积物磷的释放

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摘要

Nutrients released across the sediment-water interface during stratification and deoxygenation events may contribute a significant fraction of the total nutrient requirements for primary production in shallow lakes. In eutrophic lakes, internal nutrient cycling may sustain high nutrient concentrations regardless of external nutrient load reductions (Marsden 1989, Anderson & Ring 1999). For example, in eutrophic Lake Rotorua, New Zealand, little change in nutrient concentrations and trophic status has occurred over the last two decades despite sewage diversion in 1991 (Burns 1997). Previous predictions of water quality in this lake indicate that internal nutrient loads are likely to be a significant component of the total nutrient budget (Rutherford et al. 1996). Our objective was to quantify sediment phosphorus release in polymictic Lake Rotorua during a stratification event.
机译:在分层和脱氧过程中,通过沉积物-水界面释放的营养物可能占浅湖初级生产总养分需求的很大一部分。在富营养化的湖泊中,内部营养循环可能维持较高的营养浓度,而不考虑外部营养负荷的减少(Marsden 1989,Anderson&Ring 1999)。例如,尽管1991年污水被分流,但在过去的二十年里,在新西兰富营养化的罗托鲁瓦湖,养分浓度和营养状况几乎没有发生变化(Burns 1997)。先前对该湖水质的预测表明,内部养分负荷可能是养分总预算的重要组成部分(Rutherford等,1996)。我们的目标是量化分层事件期间多旋态罗托鲁瓦湖中沉积物磷的释放。

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