镉在土水系统中的迁移特征
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TRANSPORT CHARACTERISTICS OF CADMIUM IN SOIL-WATER SYSTEM
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    摘要:

    本文研究了4种红壤和水体系中镉的迁移特征。结果表明:镉扩散系数D变化在5.6×10-8-9.3×10-7cm2/sec;通过比较单、双表面Langmuir方程的参数,发现四个土壤的高能位吸附常数远远大于低能位吸附常数,高能位的最大吸附量b1明显小于低能位的最大吸附量b2,即镉被土壤吸附是以低能位为主,导致镉在土水体系中高度迁移性;四种土壤对镉的吸附量随土水系统中pH的变化,可分为三个区域,即pH6.0的强吸附和沉淀区,在稳定吸附区镉吸附量与pH呈正相关。pH6以下被吸附的镉中生物有效态镉量随pH的升高而增加,pH6以上被吸附的镉中生物有效态镉量随pH升高而降低。

    Abstract:

    Transport characteristics of cadmium in 4 soil-water systems were studied. The results showed that the diffusion coefficients of cadmium ranged from 5.6×10-8 to 9.3×10-7cm2/sec. Comparison between the parameters from the single and two-surface Langmuir equations demonstrated that the maximum adsorption capacity (b2)of low-energy sites was much greater than the maximum adsorption capacity (b1)of high-energy sites, resulting in high transportability of cadmium in the soil-water system. The variation of adsorption capacity of cadmium with pH had three distinct stages, i. e., low adsorption stage at pH6.0. The adsorption capacity of cadmium was positively correlated with pH at the stable adsorption stage. The bioavailability of adsorbed cadmium increased with increasing pH when pH<6 but decreased with increasing pH when pH<6.

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廖敏,谢正苗,黄昌勇.镉在土水系统中的迁移特征[J].土壤学报,1998,35(2):179-185. DOI:10.11766/trxb199611160205 Liao Min, Xie Zheng-miao, Huang Chang-yong. TRANSPORT CHARACTERISTICS OF CADMIUM IN SOIL-WATER SYSTEM[J]. Acta Pedologica Sinica,1998,35(2):179-185.

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  • 收稿日期:1996-11-16
  • 最后修改日期:1997-10-08
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  • 在线发布日期: 2013-02-25
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