盐渍土中盐结晶的显微研究——Ⅰ.芒硝无水芒硝的转换因素和蓬松盐土蓬松层的形成
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:


MICROSCOPICAL RESEARCH ON THE CRYSTALLIZATION OF SALTS IN SALINE SOILS
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:

    应用偏光显微镜技术与扫描电子显微镜技术,对三种不同类型盐土的盐结晶进行观察研究。从土壤溶液的蒸发过程中,我们观察到石膏(CaSO4·2H2O)、芒硝(Na2SO4·10H2O)、泻利盐(MgSO4·7H2O)、石盐(NaCl)结晶的析出过程,析出顺序受温度的影响。用这种方法可以快速确定土壤溶液中主要盐分类型。扫描电子显微镜的照片,展示出某些盐类结晶的自然特征,它们是:与土粒胶结紧密的石盐(NaCl)、由芒硝(Na2SO4·10H2O)脱水转变成的无水芒硝(Na2SO4)、或由硫酸钠、硫酸钙形成的复盐——钙芒硝Na2Ca(SO4)2。各种盐类在土壤中结晶出来形态清晰。以硫酸钠的溶解特性为例,扼要地讨论了土壤中芒硝—无水芒硝的转化条件及其对土壤结构产生的影响。

    Abstract:

    The crystallization of salts in three kinds of saline soil was studied,with polarizing microscope and of scanning electron microscope (SEM).It was found that the crystallization order depended on temperature,and under different temperature the main salts in soil solution were determined rapidly.The morphology of several salts in soil were studied by SEM Technique.It was found that halite (NaCl) Pras closely cemented with soil particles,thenardite (Na2SO4) was transformed from mirabilite (Na2SO4·10H2O) by dehydration,and the glaubcrite [Na2Ca(SO4)2] was formed by calcium sulfate and sodium sulfate.These salt crystals separated were clear,without any mixture.They would be formed in complex salt under certain conditions.As an example,the condition which affected the transformation of mirabilite-thenardite and its effect on the development of soil structure are discussed.

    参考文献
    相似文献
    引证文献
引用本文

张粹雯,王遵亲.盐渍土中盐结晶的显微研究——Ⅰ.芒硝无水芒硝的转换因素和蓬松盐土蓬松层的形成[J].土壤学报,1987,24(3):281-285. Zhang Cuiwen, Wang Zunqin. MICROSCOPICAL RESEARCH ON THE CRYSTALLIZATION OF SALTS IN SALINE SOILS[J]. Acta Pedologica Sinica,1987,24(3):281-285.

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: 2013-02-25
  • 出版日期: