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作 者:曾祥峰[1,2] 王祖伟[1] 于晓曼[1] 王小霞[1] 李婷[1] 纪占华[1] 侯迎迎[1] 张辉[1] 徐喆[1]
机构地区:[1]天津市水环境与水资源重点实验室天津师范大学,天津300387 [2]中科院天津工业生物技术研究所,天津300308
出 处:《中国地质》2011年第1期212-217,共6页Geology in China
基 金:国家自然科学基金项目(40973078,40830746);天津市自然科学基金项目(08JCYBJC10400)联合资助
摘 要:实验研究了不同的pH值、初始离子浓度、矿物用量、温度以及时间等因素对针铁矿和软锰矿吸附镉的影响。结果表明:在pH值从酸性到近中性的范围内,两种氧化矿物对镉的吸附量增加较快,然后在碱性条件下吸附量保持着最大值;反应前后两种氧化矿物溶液的pH值均有不同程度的变化,其中针铁矿和软锰矿的临界pH值分别为8和6.5;两种矿物对镉的吸附在6 h左右达到了吸附平衡,吸附等温线都较好地符合Freundlich等温方程式;随着两种氧化物用量的增加,其吸附量也有增加;室温下,针铁矿和软锰矿对镉的吸附效果较好。The adsorption of cadmium by goethite and manganite was experimentally studied.The adsorption quantity of cadmium by goethite and manganite increased with the increase of pH from acid to neutral and reached the maximum under the alkaline condition.After the adsorption of cadmium by goethite and manganite happened,the pH values of the solutions were changed,and the critical pH values were 8 for goethite and 6.5 for manganite.The adsorption balance time of goethite and manganite for cadmium was 6 hours.The adsorption isotherms were consistent with Freundlich isothermal equation.The adsorption effect of goethite and manganite for cadmium was ideal at the room temperature.
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