首页> 外文期刊>International journal of design & nature and ecodynamics >ECODYNAMIC ASSESSMENT OF THE SUBMERGED AQUATIC VEGETATION IN LAKE OKEECHOBEE, FLORIDA UNDER NATURAL AND ANTHROPOGENIC STRESS
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ECODYNAMIC ASSESSMENT OF THE SUBMERGED AQUATIC VEGETATION IN LAKE OKEECHOBEE, FLORIDA UNDER NATURAL AND ANTHROPOGENIC STRESS

机译:自然和人为胁迫下佛罗里达州奥基乔比湖淹没水生植物的经济评估

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摘要

Lake Okeechobee, a large, shallow lake in southern Florida, is the liquid heart of the Everglades. The lake's hydrodynamic patterns and water depths have been impacted by four major hurricanes in the past decade, including Irene (1999), Frances and Jeanne (2004), and Wilma (2005), and intermittent water level variations due to droughts in 2000-2001 and 2007-2008. In the past few decades, conditions in Lake Okeechobee have changed significantly, largely as a result of nutrient inputs to the ecosystem from agriculture and other human activities in the watershed. The excessive phosphorus loads from the lake's watershed have led to an increase in eutrophication and contributed to the accumulation of phosphorus-rich mud sediments on the lake bottom. The cumulative effect of these continuous natural hazards and anthropogenic impacts in Lake Okeechobee resulted in resuspending a large quantity of sediment, lowering light transparency, and releasing a large amount of nutrients into the water column, followed by long-standing shallow water depths. Such collective impacts led to a drastic change of sediment bed and ecosystem stability, especially the submerged aquatic vegetation (SAV). This study quantifies the ecodynamics of SAV to elucidate the coupled impact of natural and anthropogenic stress by a numerical model, the Lake Okeechobee Environment Model (LOEM) that links the spatial and temporal distributions of SAV as a whole.
机译:奥基乔比湖是佛罗里达州南部的一个大而浅的湖,是大沼泽地的液态中心。在过去十年中,该湖的水动力模式和水深受到了四个主要飓风的影响,其中包括艾琳(1999),弗朗西斯和珍妮(2004)和威尔玛(2005),以及2000-2001年干旱造成的间歇水位变化和2007-2008年。在过去的几十年中,奥基乔比湖的条件发生了重大变化,这主要是由于流域内农业和其他人类活动向生态系统输入的养分所致。湖泊流域中过多的磷负荷导致了富营养化的增加,并促进了富含磷的泥沙在湖底的沉积。这些持续的自然灾害和人为影响在奥基乔比湖中的累积影响导致大量的沉积物重新悬浮,降低了光的透明度,并向水柱中释放了大量的养分,随后是长期浅水深度。这种集体影响导致沉积物床和生态系统稳定性的急剧变化,特别是淹没的水生植物(SAV)。这项研究通过数值模型量化了SAV的生态动力学,以阐明自然压力和人为压力的耦合影响,该模型将整个SAV的时空分布联系在一起的奥基乔比湖环境模型(LOEM)。

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