锌在石灰性土壤中的吸附
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ZINC ADSORPTION IN CALCAREOUS SOILS
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    摘要:

    本文用平衡法研究石灰性土壤对锌的吸附.供试土壤为徐州丰县的黄潮土表层(0-15厘米).结果表明:吸附要用两个Laagmuir方程来描述,可以假想成两个L型表面,采用平移坐标法求出最大吸附量与实验结果基本相符.pH对锌的吸附影响很大,高pH(7.5)时,CaCO3组分对锌的吸附的贡献约占70%,低pH时,对吸附的贡献较小.

    Abstract:

    The effects of pH,temperature and soil components on Zn adsorption in calcareous soils were studied.The soil samples were collected from the surface layer (0-15 cm) of yellow fluvo-aquic soil in Fongxian,Jiangsu.The experimental results showed that fitting of the adsorption data to the Langmuir equation,the Langmuir plots should be split into two linear portions.This may be considered that two Langmuir type surfaces existed.The adsorption maxirtia determined by a method based on the moving of the origin of coordinates approximately agreed with the experimental results.The effect of pH on Zn adsorption was very significant.At high pH range (7.5),the contribution of CaCO3 to Zn adsorption was approximately 70% of the total amount adsorbed.At low pH the contribution bzcame less significant.The zdsorption capacity increased with increasing the temperature.

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林玉锁,薛家骅.锌在石灰性土壤中的吸附[J].土壤学报,1987,24(2):135-141. Lin Yusuo, Xue Jiahua. ZINC ADSORPTION IN CALCAREOUS SOILS[J]. Acta Pedologica Sinica,1987,24(2):135-141.

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  • 在线发布日期: 2013-02-25
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