华北农学报 ›› 2005, Vol. 20 ›› Issue (S1): 69-72. doi: 10.7668/hbnxb.2005.S1.019

所属专题: 土壤肥料

• 论文 • 上一篇    下一篇

青藏高原东缘山地土壤现代冰卷泥发生及其历史演变

张伟华1, 芦永兴1, 吕粉桃2, 史长青2, 周心澄2   

  1. 1. 内蒙古农业大学生态环境学院, 内蒙古呼和浩特 010019;
    2. 北京林业大学水土保持学院, 北京 100083
  • 收稿日期:2005-10-10 出版日期:2005-12-31
  • 作者简介:张伟华(1962- ),男,呼和浩特人,副教授。博士,主要研究方向为土壤改良与土壤侵蚀。
  • 基金资助:
    “十五”国家科技攻关项目(2001BA510B01)

Formation of Modern Times Involutions of Hilly Country Soil and their Historical Evolution in Altiplano of Qingzang

ZHANG Wei-hua1, LU Yong-xing1, LV Feng-tao2, SHI Chang-qing2, ZHOU Xin-cheng2   

  1. 1. Inner Mongolia Agricultural University the Academy of Ecologica Enironmet, Hu hhot 010019, China;
    2. College of Soil and Water Conservation BFU Key Laboratory of Soil and Water Conservation and Desertification Combating of the Ministry of Education, Beijing 100083, China
  • Received:2005-10-10 Published:2005-12-31

摘要: 文章研究了青藏高原东缘山地土壤黑钙土冰卷泥的形成过程、形态变化及发育特征。结果表明:(1)晚全新世以来,黑钙土冰卷泥层位逐渐下移,且存在加速之势,这与全球气候变化密切相关。(2)黑钙土发生分化,存在向栗钙土演化趋势,CaCO3层由粉末沉积转变为粒状沉积,且层位提升,CaCO3二次沉积普遍,溶质表聚现象加剧,与冰卷泥层位下移可互为佐证。

关键词: 黑钙土, 冰卷泥, CaCO3沉积, 演变

Abstract: In this article,the formation process,morphology variation and development features of involutions of chernozem soil were researched in eastern mountain area of Qingzhang plateau.The results were as follows:(1)The solum of involutions went down and there had a trend of speedup since late Holocene.The appears were correlated to global environmental variation.(2)The chernozem soil had evolved to kanstanozems since late Holocene.

Key words: Chernozem soi, Involutions, CaCO3 deposition, Evolution

中图分类号: 

引用本文

张伟华, 芦永兴, 吕粉桃, 史长青, 周心澄. 青藏高原东缘山地土壤现代冰卷泥发生及其历史演变[J]. 华北农学报, 2005, 20(S1): 69-72. doi: 10.7668/hbnxb.2005.S1.019.

ZHANG Wei-hua, LU Yong-xing, LV Feng-tao, SHI Chang-qing, ZHOU Xin-cheng. Formation of Modern Times Involutions of Hilly Country Soil and their Historical Evolution in Altiplano of Qingzang[J]. ACTA AGRICULTURAE BOREALI-SINICA, 2005, 20(S1): 69-72. doi: 10.7668/hbnxb.2005.S1.019.

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