首页> 外文期刊>Journal of the American Water Resources Association >Long-Term Trends of Nutrients and Sediment from the Nontidal Chesapeake Watershed: An Assessment of Progress by River and Season
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Long-Term Trends of Nutrients and Sediment from the Nontidal Chesapeake Watershed: An Assessment of Progress by River and Season

机译:非潮汐切萨皮克河流域的养分和沉积物长期趋势:按河流和季节的进展评估

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摘要

To assess historical loads of nitrogen (N), phosphorus (P), and suspended sediment (SS) from the nontidal Chesapeake Bay watershed (NTCBW), we analyzed decadal seasonal trends of flow-normalized loads at the fall-line of nine major rivers that account for >90% of NTCBW flow. Evaluations of loads by season revealed N, P, and SS load magnitudes have been highest in January-March and lowest in July-September, but the temporal trends have followed similar decadal-scale patterns in all seasons, with notable exceptions. Generally, total N (TN) load has dropped since the late 1980s, but particulate nutrients and SS have risen since the mid-1990s. The majority of these rises were from Susquehanna River and relate to diminished net trapping at the Conowingo Reservoir. Substantial rises in SS were also observed, however, in other rivers. Moreover, the summed rise in particulate P load from other rivers is of similar magnitude as from Susquehanna. Dissolved nutrient loads have dropped in the upland (Piedmont and above) rivers, but risen in two small rivers in the Coastal Plain affected by lagged groundwater input. In addition, analysis of fractional contributions revealed consistent N trends across the upland watersheds. Finally, total N:total P ratios have declined in most rivers, suggesting the potential for changes in nutrient limitation. Overall, this integrated study of historical data highlights the value of maintaining long-term monitoring at multiple watershed locations.
机译:为了评估非潮汐切萨皮克湾流域(NTCBW)的历史氮,磷,悬浮物的历史负荷,我们分析了9条主要河流的下降线流量归一化负荷的年代际趋势。占NTCBW流量的90%以上。按季节进行的负荷评估显示,N,P和SS负荷幅度在1月至3月最高,而在7月至9月最低,但是在整个季节,时间趋势都遵循类似的年代际尺度模式,但有明显的例外。总的来说,自1980年代后期以来,总氮(TN)含量下降了,但自1990年代中期以来,颗粒养分和SS却增加了。这些上升的大部分来自萨斯奎哈纳河,与科诺温戈水库的净捕集减少有关。然而,在其他河流中,也观察到SS的大幅上升。此外,其他河流的颗粒物磷负荷的总增加幅度与萨斯奎哈那州的相似。在高地(皮埃蒙特及以上)河流中,溶解的养分含量有所下降,但在沿海平原的两条小河中,受地下水输入滞后的影响,其溶解的养分含量有所增加。此外,对小部分贡献的分析表明,整个山地流域的氮素趋势一致。最后,在大多数河流中,总氮与总磷之比下降了,这表明有可能改变养分限制。总的来说,这项对历史数据的综合研究突出了在多个流域位置进行长期监测的价值。

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