青藏高原正常有机土与草毡寒冻雏形土地温观测的比较研究
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

*中国科学院土壤系统分类特别支持项目(49131020);中国科学院青藏高原研究项目(KZ951-A1-204,KZ951-A1-301,KZ957-06.KZ957-04),国家重点基础研究项目(61998040800)及中国科学院生态网络研究项目基金资助


COMPARISION OF THE EARTH TEMPERATURE BETWEEN FIBORTHIC HISTOSOLS AND MAT-CRYIC CAMBISOLS IN TIBET PLATEAU
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:

    在海拔高度相同、距离相近的纤维正常有机土与草毡寒冻雏形土地区,虽然区域气候一致,但二者地温具有显着的分布差异.从不同类型土壤40~80cm层次地温分布特征来看,草毡寒冻雏形土区域地温年平均3.0℃,变化剧烈,年较差大,0℃等值线可延伸至很深处.纤维正常有机土地温年平均1.4℃,变化较为平稳,0℃等值线只延至80~90cm左右.二类型地区地温随深度变化也有很大的不一致性.

    Abstract:

    Earth temperature was studied respectively, in Fb-Orthic Histosols area and Mat-Cryic Cambisols soil area at the same elevation and near in distance. The result showed that the two types of soils were under the identical climate, yet the earth temperature distribution differed significantly. According to the character of the earth temperature distribution in 40-80cm soil layer of the two soils, the soil temperature in Mat Cryic Cambisols varied dramatically averaging annually 3.4℃,with its zero temperature isoline extending fairly deep, whereas it was quite steady in Rb-0rthic Histosols, averaging annually 1.4℃ with its zero temperature isoline only reaching at 80-90cm or so. With increasing soil depth, the difference in variation of earth temperature in two types of soils became greater.

    参考文献
    相似文献
    引证文献
引用本文

李英年,鲍新奎,曹广民.青藏高原正常有机土与草毡寒冻雏形土地温观测的比较研究[J].土壤学报,2001,38(2):145-152. DOI:10.11766/trxb199908310201 Li Ying-nian, Bao Xin-kui, Cao Guang-min. COMPARISION OF THE EARTH TEMPERATURE BETWEEN FIBORTHIC HISTOSOLS AND MAT-CRYIC CAMBISOLS IN TIBET PLATEAU[J]. Acta Pedologica Sinica,2001,38(2):145-152.

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:1999-08-31
  • 最后修改日期:1999-12-25
  • 录用日期:
  • 在线发布日期: 2013-02-25
  • 出版日期: