首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >A nitrogen fixation estimate for the Baltic Sea based on continuous pCO(2) measurements on a cargo ship and total nitrogen data
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A nitrogen fixation estimate for the Baltic Sea based on continuous pCO(2) measurements on a cargo ship and total nitrogen data

机译:基于对货船的连续pCO(2)测量和总氮数据,对波罗的海的固氮估计

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Organic matter production and nitrogen fixation in the central Baltic Sea were studied on the basis of high-resolution CO2 partial pressure data that were obtained from an automated measurement system deployed on a cargo ship. The net organic carbon (OC) production was calculated from a surface water CO2 mass balance and used to estimate the nitrogen uptake by organic matter during the period March to August 2005. It was shown that the net OC production continued despite the exhaustion of dissolved inorganic nitrogen (DIN) after the spring bloom in April. The nitrogen demand for this production was calculated on the basis of the C/N ratio of organic matter. It was of the same order of magnitude than the winter DIN concentration that fuelled the spring bloom. Since the atmospheric DIN deposition was negligible and no indications of alternative DIN sources were found, it was assumed that N-2 fixation had taken place despite the low temperatures (4-8 degrees C) in April/May. This "cold fixation" amounted to 74 mmol m(-2) whereas a value of 99 mmol m(-2) was obtained for the summer N-2 fixation during June/July. Due to the contribution of the April/May N-2 fixation, a total annual rate (173 +/- 35 mmol m(-2)) was obtained for 2005 which is considerably higher than presently accepted estimates. These findings were confirmed by a nitrogen budget based on long-term data (1993-2006) for total nitrogen and total phosphorus concentrations. Furthermore, these data revealed a 30% increase in N2 fixation during the years 1994-2006.
机译:在高分辨率的二氧化碳分压数据的基础上,对波罗的海中部的有机物生产和固氮进行了研究,这些数据是从部署在货船上的自动测量系统获得的。根据地表水CO2的质量平衡计算净有机碳(OC)产量,并将其用于估算2005年3月至8月期间有机物质对氮的吸收。尽管溶解的无机物已耗尽,但净OC产量仍在继续4月春天开花后的氮(DIN)。根据有机物的碳氮比计算出该产品的氮需求量。它与冬季DIN浓度的数量级相同,助长了春季开花。由于大气DIN的沉积微不足道,并且没有找到替代DIN来源的迹象,因此可以认为尽管4月/ 5月温度较低(4-8摄氏度),N-2固着还是发生了。此“冷固色”总计为74 mmol m(-2),而在六月/七月的夏季N-2固色中获得的值为99 mmol m(-2)。由于4月/ 5月N-2固定的贡献,2005年的总年率(173 +/- 35 mmol m(-2))大大高于目前接受的估计值。这些发现得到了基于长期数据(1993-2006年)的总氮和总磷浓度的氮预算的证实。此外,这些数据显示在1994-2006年间,N2固定率增加了30%。

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