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首页> 外文期刊>Estuarine Coastal and Shelf Science >Tidal fluxes of dissolved oxygen at the North Inlet-Winyah Bay National Estuarine Research Reserve
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Tidal fluxes of dissolved oxygen at the North Inlet-Winyah Bay National Estuarine Research Reserve

机译:北入口-威亚湾国家河口研究保护区的溶解氧潮汐通量

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摘要

Advective, dispersive and total dissolved oxygen (DO) fluxes from 1297 complete tidal cycles were analyzed to test the "outwelling" hypothesis as it pertains to DO. A 910 day time series of meteorological and water quality data (approximately 35,000 half-hourly observations) was used to assess DO fluxes and dynamics at Crab Haul Creek, a small (1.1 km~2) tidal salt marsh basin at North Inlet, South Carolina, within the North Inlet-Winyah Bay National Estuarine Research Reserve. A basin storage curve, derived from water velocity measurements made across a permanent transect in the tidal creek every half hour for eight semidiurnal tidal cycles, enabled water discharges to be estimated from tide height readings in the 910 day time series. The discharges along with DO concentration measurements were used to calculate DO fluxes for each tidal cycle in the series. The long-term mean dispersive and advective DO fluxes were —0.281 g O_2 s~(-1) and —0.375 g O_2 s~(-1), respectively. Based on "t" tests both means are significantly less than zero (p < 0.02), indicating exports. Furthermore a significant correlation was found between the dispersive DO export and the tidal mean solar radiation, indicating that photosynthesis is the principal process driving the dispersive export of DO. On the other hand no significant correlations were found between the advective export of DO and solar radiation or between the dispersive fluxes of DO and salt. The absence of such correlations indicates that the advective export of DO is simply an artifact of a slight ebb sampling bias in our computation of the tidal mean discharge. On a unit area basis the average annual dispersive export of DO is 8.9 g m~(-2) yr~(-1) or 0.28 mol DO m~(-2) yr~(-1). This is a small fraction of the oxygen produced in the basin by phytoplankton (18 mol DO m~(-2) yr~(-1)) and its contribution to the DO resources of the receiving waters is far exceeded by the oxygen demand associated with the concurrent export of dissolved organic carbon (200—300g m~(-2)yr~(-1)).
机译:分析了来自1297个完整潮汐周期的正,分散和总溶解氧(DO)通量,以检验与DO有关的“外部”假设。使用910天的时间序列的气象和水质数据(大约半小时观测35,000次)来评估Crab Haul Creek的DO通量和动态,Crab Haul Creek是南卡罗来纳州北入口的一个小型(1.1 km〜2)潮汐盐沼盆地。位于北入口-威亚湾国家河口研究保护区内。根据八个半日潮汐周期每半小时对潮汐小溪的永久断面进行水速测量得出的流域储水曲线,可以根据910天时间序列中的潮汐高度读数估算出排水量。排放量与溶解氧浓度测量值一起用于计算系列中每个潮汐循环的溶解氧通量。长期平均分散DO流量为-0.281 g O_2 s〜(-1)和-0.375 g O_2 s〜(-1)。根据“ t”检验,两种均值均显着小于零(p <0.02),表明出口。此外,在分散的DO出口与潮汐平均太阳辐射之间发现了显着的相关性,表明光合作用是驱动DO的分散出口的主要过程。另一方面,在DO的平流输出与太阳辐射之间或DO与盐的分散通量之间未发现显着相关性。没有这样的相关性,表明在我们的潮汐平均流量计算中,DO的对流输出只是一个轻微的退潮采样偏差的假象。按单位面积计算,溶解氧的年平均出口量为8.9 g m〜(-2)yr〜(-1)或0.28 mol DO m〜(-2)yr〜(-1)。这只是浮游植物在盆地中产生的氧气的一小部分(18 mol DO m〜(-2)yr〜(-1)),其对接收水的DO资源的贡献远远超出了相关的氧气需求并同时输出溶解的有机碳(200-300g m〜(-2)yr〜(-1))。

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