紫色土K+吸附解吸动力学研究
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STUDY ON K+ ADSORPTION-DESORPTION KINETICS OF PURPLE SOIL
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    摘要:

    从国家紫色土肥力与肥料效益监测基地定位试验上,在第10年水稻收获后从0~30cm土层采取土壤样品,研究土壤K+吸附、解吸动力学过程。结果表明,不同施肥处理土壤K+吸附、解吸反应分别在24~32min和46~64min达到平衡,吸附、解吸平衡量分别为141~192cmol kg-1和116~175cmol kg-1。相关分析说明,土壤阳离子交换量(CEC)及粘粒含量是影响吸附平衡时间、吸附平衡量的重要因素;CEC、交换钾量是影响解吸平衡时间、解吸平衡量的重要因素。由此可见,长期不同施肥对土壤CEC、粘粒及交换钾量产生影响,从而影响了紫色土K+吸附、解吸平衡时间及吸附、解吸平衡量。平衡前钾离子的吸附、解吸速度及吸附、解吸率与反应时间lnt间存在良好的线性关系。其中反应速度直线和解吸率直线的斜率、初始反应速度及初始吸附率均与CEC、粘粒含量密切相关。Elovich方程和一级扩散方程分别为描述紫色土K+吸附、解吸反应的最优与最差模型,指数方程和抛物线扩散方程拟合性介于Elovich方程和一级扩散方程之间。由此可见,紫色土K+吸附、解吸过程不是一个单纯的过程,而是一个包括土体膨胀、吸附位活化、表面扩散等诸多因素的复杂过程。

    Abstract:

    Soil samples were taken from 0~30 cm layer from selected plots with various fertilization treatments from a 10 years fixed site field trial in the National Purple Soil Fertility and Fertilizer Efficiency Monitored Base.Kinetics of K adsorption and native K desorption of the soil samples were studied.Results showed that K+ adsorption and desorption equilibrated in 24~32 min and 46~64 min, respectively, and the capacity of K+ equilibrium adsorption and desorption were 14.1~19.2 cmol kg-1 and 11.6~17.5 cmol kg-1, respectively.Correlation analysis indicated that soil cation exchange capacity (CEC) and clay content were important factors that affected the time and the capacity of K+ equilibrium adsorption; soil CEC and exchangeable K content were important factors that affected the time and capacity of K+ equilibrium desorption.As mentioned above the effects of long-term different fertilizer application on soil CEC, clay content and exchangeable K content affected the time and capacity of K+ equilibrium adsorption and desorption in purple soil.

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熊明彪,田应兵,宋光煜,石孝均,毛炳衡.紫色土K+吸附解吸动力学研究[J].土壤学报,2004,41(3):354-361. DOI:10.11766/trxb200304240305 Xiong Mingbiao, Tian Yingbing, Song Guangyu, Shi Xiaojun, Mao Bingheng. STUDY ON K+ ADSORPTION-DESORPTION KINETICS OF PURPLE SOIL[J]. Acta Pedologica Sinica,2004,41(3):354-361.

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  • 收稿日期:2003-04-24
  • 最后修改日期:2003-08-29
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  • 在线发布日期: 2013-02-25
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