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Isotherm and kinetic studies on the adsorption of humic acid molecular size fractions onto clay minerals
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作者 Mohamed E.A.El-Sayed Moustafa M.R.Khalaf James A.Rice 《Acta Geochimica》 EI CAS CSCD 2019年第6期863-871,共9页
Humic acid(HA)can adsorb onto mineral surfaces,modifying the physicochemical properties of the mineral.Therefore,understanding the sorption behavior of HA onto mineral surfaces is of particular interest,since the fate... Humic acid(HA)can adsorb onto mineral surfaces,modifying the physicochemical properties of the mineral.Therefore,understanding the sorption behavior of HA onto mineral surfaces is of particular interest,since the fate and transport of many organic and inorganic contaminants are highly correlated to HA adsorbed onto clay surfaces.Due to the extreme heterogeneity of HA,the extracted IHSS Leonardite humic acid(LHA)used in this work was fractionated using an ultrafiltration technique(UF)into different molecular size fractions(Fr1,>0.2μm;Fr2,0.2 pm-300,000 daltons;Fr3,300,000-50,000 daltons;Fr4,50,000-10,000 daltons;Fr5,10,000-1000 daltons).Equilibrium and the kinetics of LHA and fraction adsorption onto kaolinite and montmorillonite were investigated.The results demonstrated that the maximum adsorption capacity of LHA,Frl,Fr2,Fr3,Fr4,and Fr5 was 5.99,13.69,10.29,7.02,5.9&and 5.09 on kaolinite while it was 8.29,22.62,13.17,8.91,8.62,and 5.69 on montmorillonite,respectively.The adsorption equilibrium data showed that the adsorption behavior of LHA and its fractions could be described more practically by the Langmuir model than the Freundlich model.The rate of humic acid fraction adsorption onto clays increased with decreasing molecular size fraction and increasing carboxylic group content.Pseudo-first-and second-order models were used to assess the kinetic data and the rate constants.The results explained that LHA and its fractions adsorption on clay minerals conformed more to pseudosecondo rder. 展开更多
关键词 KAOLINITE montmorillonite Leonardite humic acid humic acid fractions Kinetics EQUILIBRIUM
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不同施肥处理土壤胡敏酸及其级分与蒙脱石的吸附特征 Ⅱ. 蒙脱石对胡敏酸不同级分的吸附 被引量:3
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作者 王旭东 张一平 胡田田 《土壤学报》 CAS CSCD 北大核心 2001年第1期60-66,共7页
采用酒精沉淀法,把不同施肥处理土壤胡敏酸分为7个级分,研究了胡敏酸不同级分与钙饱和蒙脱石的吸附特征。结果表明,蒙脱石对胡敏酸各级分的吸附可用单表面Langmuir、双表面Langmuir和Freundlich方程来描述。各级分的吸附量和吸附强... 采用酒精沉淀法,把不同施肥处理土壤胡敏酸分为7个级分,研究了胡敏酸不同级分与钙饱和蒙脱石的吸附特征。结果表明,蒙脱石对胡敏酸各级分的吸附可用单表面Langmuir、双表面Langmuir和Freundlich方程来描述。各级分的吸附量和吸附强度不是随级分数变化单一递增或递减,在7个级分中,级分4、3的吸附量和吸附强度较大,是吸附最佳级分。说明级分4、3具有与蒙脱石胶体最佳的成键吸附状态,是吸附最佳分子状态。有机肥处理,吸附最佳级分的吸附性状(吸附量和吸附强度)优于化肥、无肥处理。 展开更多
关键词 蒙脱石 胡敏酸级分 吸附 施肥
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