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Hydrologic Controls of Coastal Groundwater Discharge in Southern Taylor Slough, Everglades National Park, Florida

机译:佛罗里达大沼泽地国家公园南泰勒斯劳沿海地下水排放的水文控制

摘要

This project empirically determined the controls of groundwater discharge potential and surface water chemistry in southern Taylor Slough, Everglades National Park, Florida. Potential for groundwater discharge was calculated as the difference in equivalent freshwater stage between groundwater and surface water on a daily basis for two sites (upland and coastal) along southern Taylor Slough. Upstream water stages were shown to vary most similarly to the timing of groundwater discharge potential in coastal Taylor Slough. Surface water major ion chemistry did not apparently change as a result of groundwater discharge potential. Surface water major ion chemistry at the coastal site was controlled by surface water flow direction, while at the more inland site surface water major ion chemistry was controlled by upstream water levels and evapotranspiration. Surface water phosphorus concentrations at the coastal site were controlled by groundwater discharge and flows of local surface water.
机译:该项目根据经验确定了佛罗里达大沼泽国家公园南部泰勒斯劳南部的地下水排放潜力和地表水化学的控制方法。地下水排放潜力的计算方法是:沿着泰勒斯劳河南部的两个地点(陆地和沿海地区)每天在地下水和地表水之间的当量淡水阶段之差。研究表明,上游沿海地区的水位变化与沿海泰勒斯劳(Taylor Slough)地下水排放潜力的时间变化最为相似。由于地下水的排放潜力,地表水主要离子的化学性质没有明显改变。沿海地区的地表水主要离子化学受地表水的流动方向控制,而内陆地区的地表水主要离子化学受上游水位和蒸散量控制。沿海地区的地表水磷浓度受地下水排放和当地地表水流量控制。

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    Linden Edward;

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  • 年度 2015
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