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Wind-induced increases in trophic state characteristics of a large (27 km~2), shallow (1.5 m mean depth) florida lake

机译:大面积(27 km〜2)浅(平均深度1.5 m)佛罗里达湖的风致营养状态特征增加

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摘要

Nutrient and chlorophyll concentrations in Lake Newnan (27 km~2, mean depth 1.5 m), Florida showed dramatic increases from 1991 to 1998. Historical data showed Lake Newnan never had sufficient aquatic macrophyte abund-ance for a shift in alternate stable states to account for increases in trophic state characteristics. External phosphorus and nitrogen loads from incoming streams were monitored from August 1997 to July 1998 to determine if external supplies of nutrients were responsible for increases in lake nutrient and chlorophyll concentrations. During the study period, external nutrient loading rates were not correlated to lake nutrient concentrations. Phosphorus and nitrogen models based on the external loading estimates predicted the lake total phosphorus and total nitrogen concentrations to be 370% and 680% less, respectively, than the observed lake total phosphorus and total nitrogen mean concentrations. Consequently, phosphorus and nitrogen exports were 280% and 540% greater, respectively, than stream input loading. Data during the study period revealed strong inverse relations between lake stage and total phosphorus (r=-0.78), total nitrogen (r=-0.71), and chlorophyll (r=-0.90) concentrations. Long-term data (1965-1998) also revealed inverse correlations (r=-0.48 to -0.52) between lake stage and total phosphorus, total nitrogen, and chlorophyll concentrtions. Applying fundamental wave theory and using a bathymetric map, it is probable that as much as 70% of the lake bottom sediment could be subjected to resuspension 50% of the time when the lake stage falls below 19.9 m mean sea levle (msl). Above a lake stage of 19.90 m msl, less than 20% of the lake bottom sediment can potentially be resuspended 50% of the time. A percent frequency distribution from 1991 to 1998 showed that over 30% of the lake stages fell below 19.9 m msl. However, from 1967 to 1990, only 8% of the lake stage values fell below 19.9 m msl. Increases in total phosphorus, total nitrogen and chlorophyll concentrations in Lake Newnan were likely caused by an increased probability of internal loading due to decreased lake levels, and not to external loading of phosphorus and nitrogen.
机译:1991年至1998年,佛罗里达州纽南湖(27 km〜2,平均深度1.5 m)中的营养盐和叶绿素浓度急剧增加。历史数据表明,纽南湖的水生植物丰度从来没有足够的变化来说明其他稳定状态的变化。用于增加营养状态特性。从1997年8月至1998年7月,监测了流入河流的外部磷和氮负荷,以确定外部养分供应是否导致湖泊养分和叶绿素浓度的增加。在研究期间,外部养分负荷率与湖泊养分浓度无关。基于外部负荷估算的磷和氮模型预测的湖泊总磷和总氮浓度分别比观察到的湖泊总磷和总氮平均浓度低370%和680%。因此,磷和氮的出口量分别比料流输入负荷大280%和540%。研究期间的数据显示,湖泊阶段与总磷(r = -0.78),总氮(r = -0.71)和叶绿素(r = -0.90)浓度之间存在强烈的反比关系。长期数据(1965-1998年)也揭示了湖泊阶段与总磷,总氮和叶绿素浓度之间的反相关关系(r = -0.48至-0.52)。应用基波理论并使用测深图,当湖泊水位降到平均海平面以下(19.9 m)以下时,多达70%的湖底沉积物可能会在50%的时间内重新悬浮。在19.90 m msl的湖泊水位以上,不到50%的时间可能会将不到20%的湖底沉积物重新悬浮。 1991年至1998年的频率分布百分比显示,超过30%的湖泊水位降到了19.9 m msl以下。但是,从1967年到1990年,只有8%的湖泊水位值降至19.9 m msl以下。纽南湖中总磷,总氮和叶绿素浓度的增加很可能是由于湖水位降低而不是磷和氮的外部负荷而增加了内部负荷的可能性。

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