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评估美国东南部沿海河流的水文和营养参数的长期趋势。

Evaluation of long-term trends in hydrographic and nutrient parameters in a southeast US coastal river.

机构信息

Department of Biological Sciences, University of North Florida, Jacksonville, FL, 32224, USA,

出版信息

Environ Monit Assess. 2013 Dec;185(12):10495-509. doi: 10.1007/s10661-013-3347-4. Epub 2013 Aug 18.

DOI:10.1007/s10661-013-3347-4
PMID:23955496
Abstract

The Nassau River estuary is located in northeast Florida adjacent to the eutrophic St. Johns River. Historically, development has been sparse in the Nassau River's catchment; thus, the system may provide a relatively undisturbed aquatic environment. To monitor the condition of the Nassau River estuary and to discern spatial and temporal trends in water quality, nutrients and hydrographic variables were assessed throughout the estuary from 1997 to 2011. Hydrographic (temperature, salinity, total suspended solids, and turbidity) and nutrient parameters (total phosphorus, ortho-PO₄(3-), total nitrogen, NH₄(+), total Kjeldahl nitrogen, and NO₃(-)) were monitored bimonthly at 12 sites in the mesohaline and polyhaline zones of the river. Nonparametric Kendall's Tau was implemented to analyze long-term water quality patterns. Salinity was found to increase with time, particularly in the mesohaline sampling sites. Dissolved oxygen decreased over time in the estuary and hypoxic conditions became increasingly frequent in the final years of the study. Nutrients increased in the estuary, ranging from 149 to 401%. Rainfall data collected in adjacent conservation areas did not correlate well with nutrients as compared with stream discharge data collected in the basin headwaters, outside of the conservation lands, attributed here to expanding urbanization. During the study period, the Nassau basin underwent rapid human population growth and land development resulting in commensurate impacts to water quality. Nutrient and physical data collected during this study indicate that the Nassau River estuary is becoming more eutrophic with time.

摘要

拿骚河河口位于佛罗里达州东北部,毗邻富营养化的圣约翰河。历史上,拿骚河流域的发展相对较少;因此,该系统可能提供了相对未受干扰的水生环境。为了监测拿骚河河口的状况,并了解水质、营养物和水文学变量的时空趋势,1997 年至 2011 年期间对整个河口进行了评估。水文学(温度、盐度、总悬浮固体和浊度)和营养物参数(总磷、正磷酸盐(PO₄(3-))、总氮、NH₄(+)、总凯氏氮和 NO₃(-))在河流的中盐区和多盐区的 12 个地点每两个月监测一次。非参数 Kendall's Tau 用于分析长期水质模式。发现盐度随时间增加,特别是在中盐采样点。溶解氧随时间在河口减少,在研究的最后几年,缺氧条件变得越来越频繁。河口的营养物增加,范围从 149 到 401%。与收集于流域源头的溪流流量数据相比,收集于相邻自然保护区的降雨数据与营养物相关性不大,归因于城市不断扩张。在研究期间,拿骚流域经历了快速的人口增长和土地开发,对水质产生了相应的影响。本研究中收集的营养物和物理数据表明,拿骚河河口随着时间的推移变得越来越富营养化。

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