摘要
4种土壤对三价锑的吸附及动力学的研究结果表明,吸锑量的大小顺序为河潮土>红壤>紫色土.吸锑规律河潮土和紫色土呈直线型,红土红壤服从Langmuir等温式,砂岩红壤服从Temkin等温式.4种土壤的吸锑速度都很快.河潮土、砂岩红壤和紫色土的吸附动力学规律用Elovich和双常数速率方程式能很好地描述,呈极显著正相关.由于红土红壤吸附速度太快,1~2min内就几乎达到吸附平衡,不能用Elovich和双常数速率方程式描述,相关性不显著.
Adsorption and kinetics of antimony(Ⅲ)on 4 soil samples
has been studied.The results show that the order of amount of antimony(Ⅲ)adsorbed is river
tidal soil>redloam >purple soil. The isotherms of antimony(Ⅲ)adsorption on river tidal soil and
purplesoil are linear.Antimony(Ⅲ)adsorption of red loam soil is fit for the isothermal equation
ofLangmuir,and antimony(Ⅲ)adsorption sandstone red loam is fit for the isothermal equationof
Temkin. Adsorption kinetics of antimony(Ⅲ)on 4 soil samples is very rapid. The adsorp-tion
kinetics of river tidal soil. Sandstone red loam and purple soil can be described excellent-ly by
both Elovich and two-constant rate equations. The correlations are extremely signifi-cant. The
adsorption kinetics of red loam soil is also extremely rapid,and the sorbed equilibri-um
completed almost within the first 1~2min,Therefore the adsorption kinetic can not bedescribed
by both Elovich and two-constant rate equations. The correlation is not significant.
基金
湖南农业大学青年科研基金
关键词
土壤
锑离子
吸附
动力学
soils
antimony ions
adsorption
dynamics