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首页> 外文期刊>Indian Journal of Marine Sciences >Effects of biogeochemical processes on spatial distribution of iron, manganese, reactive phosphates and nitrates in the Black Sea
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Effects of biogeochemical processes on spatial distribution of iron, manganese, reactive phosphates and nitrates in the Black Sea

机译:生物地球化学工艺对黑海铁,锰,活性磷酸盐和硝酸盐的空间分布的影响

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The aim of this study was to identify differences in the distribution of Mn (Manganese), Fe (Iron), NO3- (Nitrates) and reactive phosphates (RP) in the water columns of the eastern and western basin of the Black Sea region. Accordingly, the selected sampling area covered offshore waters from west to east including Istanbul (station KD01), Eregli (KD2A, 2B, and 2C), Inebolu (KD03), Sinop (KD04), Ordu (KD5A, 5B, 5C) and Trabzon (KD06). The B and C codes for stations 2 and 5 indicate that the stations are towards the basin centers of the Black Sea. At all the stations of the study area, the Mn values were below the limit of detection (5 mu g/L) up to 100 m depth. The Mn concentration reached maximum at 200 m depth of stations KD2B, KD5B, KD5C and KD06. This situation could be due to mobilization of Mn from the continental slope sediments (Mn pump). Also, it was observed that relatively high values of nitrates were associated with low RP concentration in the deep waters of the eastern basin. If nitrate is present in the suboxic zone, bacteria prefers nitrate and reduce it as N-2 (g). Then, the FeOOH=RP (ferric oxyhydroxides equivalent to reactive phosphate) particulates sink into deeper layers without reduction by bacteria and cause the upper layers to become poor in phosphates. In case of low values of nitrate in suboxic zone, FeOOH equivalent to RP particulates are reduced to dissolved Fe+2 by the bacteria. Significantly higher levels of nitrate concentrations were observed at station KD06. In conclusion, the eastern basin center is characterized by relatively higher nitrate concentrations in water columns compared to those in the western basin center. Therefore, the eastern basin contains lower RP concentrations and this limits the phytoplankton growth. It is concluded that where nitrate concentrations are higher than 2 mu M, the bacteria preferred to reduce the nitrates. On the other hand, particulate Fe can be reduced chemically with H2S in the deeper layers, where there is lower nitrate concentration.
机译:该研究的目的是鉴定黑海地区东部和西部盆地水柱中Mn(锰),Fe(铁),No3-(硝酸盐)和反应性磷酸盐(RP)的差异。因此,所选择的采样面积从西部到东部覆盖了海上水域,包括伊斯坦布尔(电台KD01),Eregli(KD2A,2B和2C),Inebolu(KD03),SINOP(KD04),ORDU(KD5A,5B,5C)和Trabzon (kd06)。车站2和5的B和C代码表明该站朝向黑海的盆中中心。在研究区域的所有站点,MN值低于检测限直至100米深度的检测极限(5μg/ l)。 Mn浓度达到200米的电站KD2B,KD5B,KD5C和KD06的最大值。这种情况可能是由于从大陆坡沉积物(Mn泵)的Mn动员。而且,观察到,在东部盆地的深水中,硝酸盐的相对高值与低RP浓度相关。如果在中草区中存在硝酸盐,则细菌更喜欢硝酸盐并将其降低为N-2(G)。然后,FeOOH = RP(当量与反应性磷酸的二羟基氧化物)颗粒颗粒沉入深深的层而不会被细菌减少,使上层在磷酸盐中变差。在中毒区中硝酸盐的低值的情况下,通过细菌将FeOOH与RP颗粒相当于溶解的Fe + 2。在驻地KD06观察到显着较高水平的硝酸盐浓度。总之,与西部流域中心相比,东部盆地中心的特征在于水柱中的硝酸盐浓度相对较高。因此,东部盆地含有较低的RP浓度,这限制了浮游植物的生长。结论是,硝酸盐浓度高于2μm的情况下,细菌优选减少硝酸盐。另一方面,颗粒Fe可以在更深层中用H 2 S化学减少,其中硝酸浓度降低。

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