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Utilization of steelmaking slag at marine environment for coastal revegetation

机译:利用海洋环境中的炼钢渣进行沿海植被恢复

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Due to lack of nutrient elements supply such as iron for the multiplication of photoplankton and seaweeds, recently barren grounds without seaweed in coastal areas present serious environmental problems not only in Japan but also around the world. Because of various oxide constituents such as FeO, SiO2, CaO and P2O5, low cost and abundant quantity, steelmaking slag is regarded as one of the best suitable candidate materials for providing nutrient elements for restoring seaweed beds. Ferrous ion is the obligatory nutrient element for growth of seaweed. However it is easy to be oxidized to form ferric hydroxide colloid in the presence of dissolved oxygen in seawater. It is well known that the dredged soil contains various kinds of organic acid such as fulvic acid and humic acid, and these organic acids can chelate iron ion to stabilize it and improve its solubility. For effective utilization of steelmaking slag at marine environment for coastal revegetation, in the present study, the shaking experiment of synthesized steelmaking slag and dredged soil mixture was conducted to investigate the dissolution of Ca, Si, Al, Fe and P. The dissolution of Ca from slag-soil mixture results in increasing the pH of the shaking solution. Mg provides a buffering action when pH reaches a certain extent. Simultaneously soil also provides a buffering action on the whole pH increasing process. The dissolved iron is estimated to equilibrate with Fe2O3 phase, since the oxidation - reduction potential (ORP) value of solution is in the condition of the Fe2O3 stable area in the potential-pH diagram.
机译:由于缺乏营养元素供应,例如用于浮游植物和海藻繁殖的铁,最近在沿海地区没有海藻的贫瘠土地不仅在日本而且在世界范围内都带来严重的环境问题。由于FeO,SiO2,CaO和P2O5等各种氧化物成分,成本低廉且数量丰富,炼钢炉渣被认为是提供营养元素以恢复海藻床的最合适的候选材料之一。亚铁离子是海藻生长的必需营养元素。但是,在海水中存在溶解氧的情况下,很容易被氧化形成氢氧化铁胶体。众所周知,在疏soil的土壤中含有各种有机酸,例如富里酸和腐殖酸,这些有机酸可以螯合铁离子以使其稳定并提高其溶解度。为了有效利用海洋环境中的炼钢渣进行沿海植被恢复,本研究进行了合成炼钢渣与疏soil土混合物的振动实验,研究了Ca,Si,Al,Fe和P的溶出度。渣-土壤混合物中的残留物会增加振荡溶液的pH值。当pH达到一定程度时,Mg提供缓冲作用。同时,土壤在整个pH值增加过程中也起到缓冲作用。由于溶液的氧化还原电位(ORP)值处于电位-pH图中的Fe2O3稳定区域的条件下,因此估计溶解的铁与Fe2O3相平衡。

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