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绿泥石对U(VI)的吸附特征研究 总被引:1,自引:0,他引:1
以绿泥石为研究对象,利用静态吸附的方法,探究了吸附时间、U(VI)初始浓度、固液比、pH值、离子类型等对U(VI)吸附效果的影响.并讨论了U(VI)在绿泥石上的吸附动力学行为.结果表明:准二级动力学模型可以用来描述U(VI)在绿泥石上的吸附;绿泥石对U(VI)的吸附20 h即趋于稳定;最佳吸附固液附比为1∶150;最佳吸附初始浓度为20μg·mL~(-1);当pH为7时,吸附效果最好.过酸或过碱都会影响绿泥石对U(VI)的吸附;溶液中Ca~(2+)、HCO_3~-、CO_3~(2-)、SO_4~(2-)、Mg~(2+)对U(VI)的吸附有较强的抑制作用. 相似文献
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内蒙大井矿床的绿泥石研究 总被引:3,自引:0,他引:3
绿泥石是热液型多金属矿床中广泛分布的近矿晕矿物,在大井矿床见于近矿的电气石绢云母-石英交代岩,石英-绿泥石-永绢云母交代炭和碳酸盐岩矿物交代岩中,绿泥石成分复杂,通过对大井矿床绿泥石成分测定,并与国内外同类型矿床中的绿泥石成分进行对比研究,发现绿泥石成分的含铁度(Fe/(Fe+Mg+Mn+Ca)可用来标志矿床的不同金属组合。大井矿床为Ag,Cu,Sn,Pb,Zn组合,绿泥石为含铁度高的种属,俄罗斯 相似文献
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Yan Tang Longkang Sang Rong Liu Yanming Yuan Yunlong Yang Xianmao Qi Jing Tan 《科学通报(英文版)》2014,59(1):82-99
Using XRD measurements of illite crystallinity,b0values of K-rich white micas and chemical compositions of chlorites combined with homogenization temperatures of fluid inclusions in calcite,the metamorphic P–T conditions of very low-grade metapelites from different depths in the 7 km Hongcan Well 1 in the Zoige?Depression,Sichuan,China,have been obtained in this paper.Knowledge of the tectonic evolution of the studied basin allows us to derive geothermal curves for Middle and Late Triassic time(the geothermal peak)and the present day(from thermal logging of the borehole).The retrograde P–T tracks from clockwise P–T–t loops have been revealed by the plotting of individual samples on each geotherm,which can be interpreted by the lithospheric thickening due to sedimentation and folding followed by continuous uplift and erosion.A stratigraphic log indicates that the Well penetrates the steep limb of a fold which perturbed the peak geotherm and caused some P–T paths to cross. 相似文献
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