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土壤腐殖酸的质子解离平衡研究
Study on the Protonic Dissociation Equilibrium of Soil Humic Acid
【摘要】 本文用电位滴定法对提纯了的土壤胡敏酸HA、富啡酸FA 的质子解离平衡进行了研究,并根据离散模型和连续亲和谱模型对实验数据进行了分析,得知HA 和FA 均含有三类酸性基团,在离子强度为0.1 m ol/L、温度25℃的条件下,pKa1 在pH< 3 时已经解离,pKa2 为4.5~5.5 和4.5~5.0,pKa3 为7.5~9.0 和7.0~9.0。它们的解离度均随pH 值的升高而增加,这种变化正反映了腐殖酸酸性功能基的非均质性。用两种模型处理滴定数据所得的结果,在误差允许范围内是一致的。
【Abstract】 The paper discusses the protonic dissociation equilibrium of pure soil humic acid and fulvic acid by the method of potentiometric titration.Discrete model and affinity spectrum model were employed to treat the experimental data. It was found that HA and FA contain three acidic groups,their apparent dissociation p K a were in the range of 2.0~3.0, 4.5~5.5, 7.5~9.0 and 2.0~3.0, 4.5~5.0, 8.0~9.0 respectively, in respect to 0.1 mol/L ionic strengths and temperature 25℃. Their dissociation degrees increased with pH and revealed the heterogeneous property of acidic function groups. The method is suitable to treat the data.
【Key words】 Humic acid Fulvic acid Dissociation constant Potentiometric titration;
- 【文献出处】 辐射防护通讯 ,RADIATION PROTECTION BULLETIN , 编辑部邮箱 ,1999年04期
- 【分类号】S152
- 【被引频次】2
- 【下载频次】111