pH对砷在贵州红壤中的吸附的影响
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

国家自然科学基金重点项目(498330002),攀登-95-预-39和贵州省科学技术基金项目资助。


EFFECT OF PH ON ADSORPTION AND TRANSFORMATION OF ARSENIC IN RED SOIL IN GUIZHOU
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    本文研究了贵州遵义红壤中pH对砷(As)的吸附和形态的影响。结果表明,当溶液中As的浓度增大时,土壤对As的吸附量增大,吸附率逐渐降低,As从红壤的低能位点位逐渐进入到高能位吸附点位,吸附反应速率减慢。Langmuir方程拟合等温吸附效果较好,可决系数达到0.969(P<0.001)。体系pH是影响红壤对As吸附、解吸的重要因素,As的吸附量随着体系pH的升高而降低,吸附态As的解吸量随着体系pH的升高而增大。酸性环境(pH=4~6.5)有利于As的吸附,碱性环境(pH=7~8.5)有利于As的解吸。

    Abstract:

    Characteristics of Arsenic adsorption in red soil,in Zunyi,Guizhou,affected by pH were studied in this research work.Results show that with increase in Arsenic concentration in the soil solution,Arsenic adsorption of the soil increased,while its adsorption rate declined,high-energy adsorption sites began to gradually replace low-energy adsorption sites in absorbing As,and the absorbing reaction rate reduced.The isotherm adsorption could be well fitted by the Langmuir equation.Soil pH was an important factor that affected adsorption and desorption of Arsenic.Acid environment (pH=4~6.5) facilitated adsorption of Arsenic while alkaline environment (pH=7~8.5) did desorption of Arsenic.

    参考文献
    相似文献
    引证文献
引用本文

陈静,王学军,朱立军. pH对砷在贵州红壤中的吸附的影响[J].土壤,2004,36(2):211-214. CHEN Jing, WANG Xue-jun, ZHU Li-jun. EFFECT OF PH ON ADSORPTION AND TRANSFORMATION OF ARSENIC IN RED SOIL IN GUIZHOU[J]. Soils,2004,36(2):211-214

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:
  • 最后修改日期:
  • 录用日期:
  • 在线发布日期: 2017-05-19
  • 出版日期: