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首页> 外文期刊>Deep-Sea Research >Net biological oxygen production in the ocean-II: Remote in situ measurements of O_2 and N_2 in subarctic pacific surface waters
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Net biological oxygen production in the ocean-II: Remote in situ measurements of O_2 and N_2 in subarctic pacific surface waters

机译:海洋中的生物净氧气产量-II:北极地下太平洋地表水中O_2和N_2的远程原位测量

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Net community biological production in the euphotic zone of the ocean fuels organic matter and oxygen export from the upper ocean, which has a large influence on the atmospheric pressure of carbon dioxide and is the driving force for metabolite distributions in the sea. We determine the net annual biological oxygen production in the mixed layer of the northeast subarctic Pacific Ocean from in situ O_2 and N_2 measurements. Temperature, salinity, total gas pressure and O_2 were measured every 3 h for 9 months in 2007 at about 3 m depth on a surface mooring at Station P (50°N, 145°W). The concentration of nitrogen gas, N_2, determined from separate total gas pressure and pO_2 measurements, was used as an inert tracer of the physical processes that induce gas departure from thermodynamic equilibrium with the atmosphere. We use a simple model of the ocean's mixed layer along with the nitrogen concentration to constrain the importance of bubbles, gas exchange and horizontal advection, which are then used in the oxygen mass balance to derive net biological oxygen production. The mixed-layer oxygen mass balance is dominated by exchange with the atmosphere, and we determine a mean summertime oxygen production of 24 mmol O_2 m~(-2) d~(-1). The annual pattern in the difference between the supersaturation of oxygen and nitrogen in the surface waters reveals very little net oxygen production during the winter at this location. The calculated annual net community production (NCP) of carbon from this new method, 2.5 mol m~(-2) yr~(-1) agrees to within its error of about x 40% with previous determinations at this location from oxygen mass balance, NOf draw down and ~(234)Th measurements. This value is either indistinguishable from or lower than annual NCP measurements in the subtropical North Pacific, indicating that there is no experimental evidence for differences in annual NCP between the subarctic and subtropical North Pacific Ocean.
机译:海洋富营养区的净群落生物生产为上层海洋的有机物和氧气出口提供了燃料,这对二氧化碳的大气压力有很大的影响,并且是海洋中代谢物分布的驱动力。我们根据原位O_2和N_2的测量值确定了东北亚北极太平洋混合层中的净年度生物氧气产量。在P站(50°N,145°W)的地面系泊装置上,于2007年在3 m深度处每3小时测量温度,盐度,总气压和O_2,持续9个月。由单独的总气体压力和pO_2测量确定的氮气浓度N_2被用作物理过程的惰性示踪剂,该物理过程导致气体偏离与大气的热力学平衡。我们使用海洋混合层和氮浓度的简单模型来约束气泡,气体交换和水平对流的重要性,然后将其用于氧气质量平衡以推导净生物氧气的产生。混合层的氧气质量平衡主要是通过与大气交换来实现的,我们确定夏季平均氧气产量为24 mmol O_2 m〜(-2)d〜(-1)。地表水中氧气和氮气过饱和之间的差异的年度模式表明,该位置冬季的净氧气产量很少。通过这种新方法计算出的碳的年净社区总产值(NCP)2.5 mol m〜(-2)yr〜(-1)与以前根据氧气质量平衡确定的该位置的误差在x 40%左右。 ,NOf下降和〜(234)Th个测量值。该值与亚热带北太平洋的NCP年度测量值相差无几,或低于该值,这表明没有实验证据证明北极和亚热带北太平洋的年度NCP值存在差异。

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