Institute of Marine Science, University of Alaska-Fairbanks, Fairbanks, Alaska 99775-1080.
Appl Environ Microbiol. 1988 Jun;54(6):1440-5. doi: 10.1128/aem.54.6.1440-1445.1988.
Rates of oxidation of Mn(II) were measured by an in situ incubation technique in the water column of Toolik Lake, Alaska. Measured rates were lower than those observed in other aquatic systems but were sufficient to oxidize all Mn(II) in the lake within a 3-month period. Measured rates compared favorably with rates estimated from a previous study of the geochemical cycling of Mn in Toolik Lake. The Mn(II) oxidation was largely microbially mediated, as indicated by inhibition of oxidation rates by sodium azide. Azide had been previously demonstrated to be a suitable microbial poison for studying Mn(II) oxidation in seawater. This study demonstrates that azide is also a suitable poison for freshwaters and that it inhibits microbial but not abiotic oxidation of Mn(II). Manganese(II) oxidation rates were similar during cold, under-ice conditions in early spring and during warmer summer conditions. This observation suggests that Mn(II) concentration, rather than temperature or oxygen concentration, is the most important factor regulating Mn(II) oxidation rates in Toolik Lake.
采用原位培养技术在阿拉斯加图利克湖的水柱中测量了 Mn(II)的氧化速率。测量的速率低于在其他水生系统中观察到的速率,但足以在 3 个月内氧化湖中的所有 Mn(II)。测量的速率与图利克湖之前研究锰地球化学循环的速率估计值相当吻合。Mn(II)的氧化主要是微生物介导的,这表明氧化速率被叠氮化钠抑制。先前已经证明,叠氮化钠是研究海水中 Mn(II)氧化的合适微生物毒物。本研究表明,叠氮化钠也适用于淡水,并且它抑制微生物但不抑制非生物氧化 Mn(II)。在早春冰下寒冷和温暖的夏季条件下,Mn(II)氧化速率相似。这一观察结果表明,Mn(II)浓度而不是温度或氧浓度是调节图利克湖 Mn(II)氧化速率的最重要因素。