桂西北主要退耕还林模式土壤水文—物理性质研究
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

广西壮族自治区退耕还林工作领导小组文件,桂退发[2003]10号


Soil Hydrological and Physical Properties for Main Patterns of Converting Farmland into Forestland in Northwest Guangxi Province
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:

    退耕还林是退化生态系统重建的重要途径。对桂西北地区12种退耕还林模式3a植被恢复期林地土壤水文—物理性质进行了定位监测研究。结果表明,(1)不同土壤深度(0—20 cm,20—40 cm,40—100 cm)的平均土壤容重为0.824~1.256 g/cm3,分别比农作物地增大2.4%~4.4%,其中0—20 cm土层的差异达到显著水平。(2)土壤非毛管孔隙度、总孔隙度和通气度的平均值依次为1.1%~21.3%,52.4%~59.8%和28.3%~35.7%,分别比农作物地下降4.1%~20.7%,其中非毛管孔隙度0—20 cm土层的差异达到显著水平;毛管孔隙度的平均值为38.5%~41.3%,比未退耕地增大5.2%~7.6%。(3)1m土层内的最大持水量、毛管持水量、最小持水量依次为43.0%~58.3%,37.0%~48.4%和30.5%~38.2%,分别比农作物地降低1.3%~10.5%,但差异不显著。(4)1m土层退耕还林地土壤有效贮水量为1 652.6~2 294.3 t/hm2,比农作物地提高1.9%~5.9%,但两者的差异不显著。

    Abstract:

    Converting cultivated land into forestland is an important way for the reconstruction of degraded ecosystem.Soil hydrological and physical properties on 12 converted lands in Northwest Guangxi Province after 3 year reconstruction were observed.Results showed that the averaged soil densities in different soil layers(0-20,20-40,and 40-100 cm)were 0.824~ 1.256 g/cm3,which increased by 2.4%~ 4.4%compared with cropland.Soil density within 20 cm of the surface soil reached a significant level.The averaged soil non-capillary porosity,total porosity,and ventilation were 1.1%~ 21.3%,52.4%~ 59.8%,and28.3%~ 35.7%,respectively.Soil non-capillary porosity within 20 cm of the surface soil reached a significant level.The averaged capillary porosities were 38.5%~ 41.3%,which increased by 5.2%~ 7.6%compared with original farmland.The maximum water holding capacity,the capillary water holding capacity,and the minimum water-holding capacity in the 1m layer were 43.0%~ 58.3%,37.0%~ 48.4%,and 30.5%~ 38.2%,respectively,which had no significant differences.The effective storage capacities in the 1m soil layer on converted farmland were 1652.6%~2294.3t/hm2,which increased by 1.9%~ 5.9%compared with cropland,but the differences were not significant.

    参考文献
    相似文献
    引证文献
引用本文

黄承标,李保平,赖家业,庄嘉.桂西北主要退耕还林模式土壤水文—物理性质研究[J].水土保持通报,2009,(3):108-112,169

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:2008-09-14
  • 最后修改日期:2008-11-26
  • 录用日期:
  • 在线发布日期: 2014-11-26
  • 出版日期: