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Ca^(2+) and OH^- release of ceramsites containing anorthite and gehlenite prepared from waste lime mud 被引量:5

Ca^(2+) and OH^- release of ceramsites containing anorthite and gehlenite prepared from waste lime mud
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摘要 Lime mud is a kind of solid waste in the papermaking industry,which has been a source of serious environmental pollution.Ceramsites containing anorthite and gehlenite were prepared from lime mud and fly ash through the solid state reaction method at 1050°C.The objective of this study was to explore the efficiency of Ca^2+ and OH-release and assess the phosphorus and copper ion removal performance of the ceramsites via batch experiments,X-ray diffraction(XRD) and scanning electron microscopy(SEM).The results show that Ca^2+ and OH-were released from the ceramsites due to the dissolution of anorthite,gehlenite and available lime.It is also concluded that gehlenite had stronger capacity for Ca^2+ and OH-release compared with anorthite.The Ca^2+ release could be fit well by the Avrami kinetic model.Increases of porosity,dosage and temperature were associated with increases in the concentrations of Ca^2+ and OH-released.Under different conditions,the ceramsites could maintain aqueous solutions in alkaline conditions(p H = 9.3–10.9) and the release of Ca^2+ was not affected.The removal rates of phosphorus and copper ions were as high as 96.88% and 96.81%,respectively.The final p H values of both phosphorus and copper ions solutions changed slightly.The reuse of lime mud in the form of ceramsites is an effective strategy. Lime mud is a kind of solid waste in the papermaking industry,which has been a source of serious environmental pollution.Ceramsites containing anorthite and gehlenite were prepared from lime mud and fly ash through the solid state reaction method at 1050°C.The objective of this study was to explore the efficiency of Ca^2+ and OH-release and assess the phosphorus and copper ion removal performance of the ceramsites via batch experiments,X-ray diffraction(XRD) and scanning electron microscopy(SEM).The results show that Ca^2+ and OH-were released from the ceramsites due to the dissolution of anorthite,gehlenite and available lime.It is also concluded that gehlenite had stronger capacity for Ca^2+ and OH-release compared with anorthite.The Ca^2+ release could be fit well by the Avrami kinetic model.Increases of porosity,dosage and temperature were associated with increases in the concentrations of Ca^2+ and OH-released.Under different conditions,the ceramsites could maintain aqueous solutions in alkaline conditions(p H = 9.3–10.9) and the release of Ca^2+ was not affected.The removal rates of phosphorus and copper ions were as high as 96.88% and 96.81%,respectively.The final p H values of both phosphorus and copper ions solutions changed slightly.The reuse of lime mud in the form of ceramsites is an effective strategy.
出处 《Journal of Environmental Sciences》 SCIE EI CAS CSCD 2016年第9期91-99,共9页 环境科学学报(英文版)
基金 financially supported by the National Natural Science Foundation of China (Nos.51578289 and 51468053) the Technology Major Projects of China (No.2012ZX04010-032) the Research and innovation program of graduate students in Jiangsu Province (No.KYLX_0347) the Innovation Fund for National Small and Medium Technology Based Firms of China (No.11C26213201410)
关键词 Lime mud Ceramsite Gehlenite Calcium ion PH value Lime mud Ceramsite Gehlenite Calcium ion PH value
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