氧化还原条件下红壤磷吸附与解吸特性及需磷量探讨
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

江西省自然科学基金项目(0630103)和江西省教育厅项目(赣教技字[2007]346号)资助


Study on adsorption and desorption characteristics of soils and phosphorus requirement under oxidized and reduced conditions
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:

    研究了5个酸性红壤由氧化条件转为还原条件的P吸附和解吸特性,以及确定供试红壤作为水田或旱地相应的施P量。结果表明:5个土样P吸附量随P液浓度的增加而增加,土壤对P的吸附曲线均可用Langmuir方程拟合,氧化条件下P最大吸附量变化范围为794.22 ~ 956.75 mg/kg,还原条件下P最大吸附量变化范围为867.31 ~ 1 195.62 mg/kg。P解吸量随P吸附量的增加而增加,P解吸率的结果表明,淹水不同程度地降低土壤 P解吸量。以Langmuir方程计算土壤溶液中P浓度在0.2 mg/kg时的土壤需P量作为施P量的依据,淹水后土壤标准需P量增加。

    Abstract:

    Phosphate requirement of paddy or upland were investigated by adsorption/desorption experiment under oxidized and reduced conditions in five red soils. Results showed that P adsorption capacity increased with the increase of added P concentration. Phosphate adsorption curves of soils fitted well with Langmuir equation. The range of the maximum capacities of P adsorption (Qm) ranged from 794.22 to 956.75 mg/kg under oxidized condition and from 867.31 to 1 195.62 mg/kg under reduced condition. The capacity of desorption P increased with the increase of the capacity of P adsorption, P desorption rate of soils was lower under reduced condition than that under oxidized condition. Phosphorus requirement was calculated from the Langumir equation on the basis of P concentration in soil solution at 0.2 mg/kg. Phosphorus requirement of soils increased after water logging.

    参考文献
    相似文献
    引证文献
引用本文

邵兴华,张建忠,毛 勇,王中敏.氧化还原条件下红壤磷吸附与解吸特性及需磷量探讨[J].土壤,2010,42(2):207-212. SHAO Xing-hua, ZHANG Jian-zhong, MAO Yong, WANG Zhong-min. Study on adsorption and desorption characteristics of soils and phosphorus requirement under oxidized and reduced conditions[J]. Soils,2010,42(2):207-212

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:
  • 出版日期: