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首页> 外文期刊>American Journal of Plant Sciences >Phosphorus Release from Sediments in a Riparian Phragmites australis Community at the Estuary of the Chikugogawa River, Western Japan
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Phosphorus Release from Sediments in a Riparian Phragmites australis Community at the Estuary of the Chikugogawa River, Western Japan

机译:日本西部筑后川河口河岸芦苇群落中沉积物中的磷释放

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In order to determine the contribution of aquatic macrophyte communities on nutrition to sustain the high primary productivity of an estuary aquatic community, we analyzed the process of phosphorus release from sediments in aquatic macrophyte community in the estuary of the Chikugogawa River, South-Western Japan. Vertical profile of PD3-4 concentration and redox potential (Eh) of pore water in sediments were investigated within and outside the Phragmites australis community. Sediment horizon lower than 23 cm layer from the surface showed anaerobic (Eh australis community, whereas sediment was constantly oxic (Eh > 0 mV) up to 50 cm depth outside the P. australis community without organic matter accumulation. Non-vegetated sediment with organic matter accumulation showed anoxic profile as vegetated site. PD3-4 concentration in anaerobic parts of sediment showed higher than oxic parts, and higher PD3-4 concentration in sediment pore water corresponded to sulfur deposition in sediment. Sulfate ion supplied from the sea water is reduced under the anoxic condition and S2- reacts with water-insoluble phosphorus salts e.g. Fe3(PO4)2 or AlPO4 and Fe2S3 or Al2S3 precipitates. Thus PD3-4 was mobilized and released under anoxic sediments. P. australis supply organic litter to sediment and the sediment within the P. australis community showed anoxic after aerobic decomposition of organic substances in sediment. Incubation of sediments under N2 atmosphere accumulated PD3-4 in the medium corresponding to low Eh (3-4 was released under anaerobic condition. Estuary P. australis community has function for supplying PD3-4 to river water.
机译:为了确定水生植物群落对营养的贡献,以维持河口水生植物的高初级生产力,我们分析了日本西南部筑后川河口水生植物群落中沉积物中磷的释放过程。研究了芦苇群落内部和外部的沉积物中PD3-4浓度和孔隙水氧化还原电势(Eh)的垂直分布。距表层低于23 cm的沉积物水平显示为厌氧的(Eh australis群落),而沉积物在P. australis群落外直至50 cm的深度一直是有氧的(Eh> 0 mV),没有有机质积累。物质积累表现为缺氧分布,沉积物中厌氧部分的PD3-4浓度高于有氧部分,沉积物孔隙水中的PD3-4浓度较高,对应于沉积物中的硫沉积,海水中硫酸根离子的减少在缺氧条件下,S2-与水不溶性磷盐(例如Fe3(PO4)2或AlPO4)和Fe2S3或Al2S3沉淀物发生反应,从而使PD3-4在缺氧沉积物下动员并释放出来。 P. australis群落内的沉积物在对沉积物中的有机物进行好氧分解后显示出缺氧性。对应于低Eh的培养基中的D3-4(在厌氧条件下释放3-4)。河口P. australis社区具有向河水供应PD3-4的功能。

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