Caccia Valentina G, Boyer Joseph N
Southeast Environmental Research Center, OE-148, Florida International University, Miami, FL 33199, USA.
Mar Pollut Bull. 2007 Jul;54(7):994-1008. doi: 10.1016/j.marpolbul.2007.02.009. Epub 2007 Apr 5.
The water quality in Biscayne Bay has been significantly affected by past and continuing coastal and watershed development. The nutrient concentrations in the Bay have been dramatically changed by the conversion of natural creeks and sheet flow freshwater inputs to rapid and episodic canal inputs from the large and rapidly expanding Miami metropolitan area. This study is an evaluation of nutrient loadings to Biscayne Bay for 1994-2002 from canal, atmospheric, and groundwater sources. Dissolved inorganic nitrogen (DIN, as nitrate, nitrite, and ammonium) and total phosphorus (TP) loadings by the canals were influenced by their geographic locations relative to discharge amount, watershed land use, stormwater runoff, and proximity to landfills. Annual budgets showed that canals contributed the bulk of N loading to the bay as 1687.2 metric ton N yr(-1) (88% total load). Direct atmospheric DIN load for Biscayne Bay was only 231.7 ton N yr(-1), based on surface area. Of the canal DIN load, nitrate+nitrite (NO(x)(-)) loading (1294.5 ton N yr(-1)) made up a much greater proportion than that of ammonium (NH(4)(+), 392.6 ton N yr(-1)). In the urbanized north and central Bay, canal DIN load was evenly split between NO(x)(-) and NH(4)(+). However, in the south, 95% of the DIN load was in the form of NO(x)(-), reflecting the more agricultural land use. Contrary to N, canals contributed the only 66% of P load to the bay (27.5 ton P yr(-1)). Atmospheric TP load was 14 ton Pyr(-1). In the north, canal P load dominated the budget while in the south, atmospheric load was almost double canal load. Groundwater inputs, estimated only for the south Bay, represented an important source of N and P in this zone. Groundwater input of N (141 ton N yr(-1)) was about equal to atmospheric load, while P load (5.9 ton P yr(-1)) was about equal to canal load.
比斯坎湾的水质受到过去及持续的沿海和流域开发的显著影响。天然小溪和片状淡水输入转变为来自迅速扩张的迈阿密大都市区的快速且间歇性的运河输入,导致该湾的营养物浓度发生了巨大变化。本研究评估了1994年至2002年期间来自运河、大气和地下水的营养物负荷进入比斯坎湾的情况。运河的溶解无机氮(DIN,以硝酸盐、亚硝酸盐和铵计)和总磷(TP)负荷受到其相对于排水量的地理位置、流域土地利用、雨水径流以及与垃圾填埋场的距离的影响。年度预算显示,运河贡献了该湾大部分的氮负荷,为1687.2公吨氮/年(占总负荷的88%)。基于表面积计算,比斯坎湾的直接大气DIN负荷仅为231.7吨氮/年。在运河的DIN负荷中,硝酸盐+亚硝酸盐(NO(x)(-))负荷(1294.5吨氮/年)所占比例远高于铵(NH(4)(+),392.6吨氮/年)。在城市化的湾北部和中部,运河DIN负荷在NO(x)(-)和NH(4)(+)之间平均分配。然而,在南部,95%的DIN负荷以NO(x)(-)的形式存在,这反映了更多的农业土地利用情况。与氮不同,运河仅贡献了该湾66%的磷负荷(27.5吨磷/年)。大气TP负荷为14吨磷/年。在北部,运河磷负荷在预算中占主导地位,而在南部,大气负荷几乎是运河负荷的两倍。仅针对湾南部估算的地下水输入,是该区域氮和磷的重要来源。地下水的氮输入(141吨氮/年)约等于大气负荷,而磷负荷(5.9吨磷/年)约等于运河负荷。