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首页> 外文期刊>Biogeosciences >How are oxygen budgets influenced by dissolved iron and growth of oxygenic phototrophs in an iron-rich spring system? Initial results from the Espan Spring in Fürth, Germany
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How are oxygen budgets influenced by dissolved iron and growth of oxygenic phototrophs in an iron-rich spring system? Initial results from the Espan Spring in Fürth, Germany

机译:如何在铁富型弹簧系统中受溶解的熨斗和含氧光学术的生长影响的氧预算? 来自德国Fürth的Espan Spring的初始结果

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At present most knowledge on the impact of iron on 18 O? / ? 16 O ratios (i.e. δ 18 O) of dissolved oxygen (DO) under circum-neutral conditions stems from experiments carried out under controlled laboratory conditions. These showed that iron oxidation leads to an increase in δ 18 O DO values. Here we present the first study on effects of elevated Fe(II) concentrations on the δ 18 O DO in a natural, iron-rich, circum-neutral watercourse. Our results show that iron oxidation was the major factor for rising dissolved oxygen isotope compositions in the first 85?m of the system in the cold season (February) and for the first 15?m during the warm season (May). Further along the course of the stream, the δ 18 O DO decreased towards values known for atmospheric equilibration around + 24.6?‰ during both seasons. Possible drivers for these changes may be reduced iron oxidation, increased atmospheric exchange and DO production by oxygenic phototrophic algae mats. In the cold season, the δ 18 O DO values stabilized around atmospheric equilibrium, whereas in the warm season stronger influences by oxygenic photosynthesis caused values down to + 21.8?‰. In the warm season from 145?m downstream of the spring, the δ 18 O DO increased again until it reached atmospheric equilibrium. This trend can be explained by respiratory consumption of DO combined with a relative decrease in photosynthetic activity and increasing atmospheric influences. Our study shows that dissolved Fe(II) can exert strong effects on the δ 18 O DO of a natural circum-neutral spring system even under constant supply of atmospheric O 2 . However, in the presence of active photosynthesis, with supply of O 2 to the system, direct effects of Fe oxidation on the δ 18 O DO value become masked. Nonetheless, critical Fe(II) concentrations may indirectly control DO budgets by enhancing photosynthesis, particularly if cyanobacteria are involved.
机译:目前大多数关于铁对18 o的影响的知识? /?在环中性条件下溶解氧(DO)的16℃(即δ18O)源于受控实验室条件下进行的实验。这些显示铁氧化导致δ180的增加。在这里,我们提出了第一研究对天然,铁富含,富含环中性水道δ180的升高的Fe(II)浓度的影响。我们的研究结果表明,铁氧化是寒季(二月)中的第一个85〜M系统中溶解的氧同位素组合物上升的主要因素,并在温暖的季节(5月)期间为前15μm。进一步沿着流的过程,Δ180确实朝向大气平衡所知的值下降+ 24.6在两个季节期间。这些变化的可能驾驶员可能会降低铁氧化,增加大气交换,并通过含氧光养藻类垫进行生产。在寒冷的季节中,δ180围绕大气平衡稳定的值,而在温暖的季节中的含氧光合作用的更强的影响导致+ 21.8 + 21.8。在温暖的季节从弹簧的下游145℃,δ180再次增加,直到它达到大气平衡。这种趋势可以通过呼吸消耗来解释与光合活性相对降低以及增加大气影响。我们的研究表明,即使在恒定的大气O 2的恒定供应下,溶解的Fe(II)也可以对自然环中性春季系统的δ180作用产生强烈影响。然而,在活性光合作用的存在下,随着系统的供应,Fe氧化在δ180上的直接影响成为掩蔽。尽管如此,临危Fe(ii)浓度可以通过增强光合作用来间接控制预算,特别是如果涉及蓝藻。

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