Soil Quality Evolution on Converted Farmland in High-mountain of Datong County in Qinghai Province
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Soil Quality Evolution on Converted Farmland in High-mountain of Datong County in Qinghai Province
Bulletin of Soiland Water ConservationVol. 26, Issue 1, Pages: 6-10(2007)
作者机构:
1. 深圳市水利规划设计院,广东,深圳,518036
2. 北京林业大学水土保持学院,北京,100083
3. 西北农林科技大学, 陕西 杨凌,712100
4. 青海省大通县林业局, 青海 大通,810100
作者简介:
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Published:2007
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ZHENG Jia-li, GAO Guo-xiong, LU Fen-tao, et al. Soil Quality Evolution on Converted Farmland in High-mountain of Datong County in Qinghai Province[J]. Bulletin of Soiland Water Conservation, 2007, 26(1): 6-10.
DOI:
ZHENG Jia-li, GAO Guo-xiong, LU Fen-tao, et al. Soil Quality Evolution on Converted Farmland in High-mountain of Datong County in Qinghai Province[J]. Bulletin of Soiland Water Conservation, 2007, 26(1): 6-10.DOI:
Soil Quality Evolution on Converted Farmland in High-mountain of Datong County in Qinghai Province
The research was conducted in high-mountain of Datong County in Qinghai Province
where is a demonstration site for Land Conversion Program(LCP).For the specific converted lands
the typical soil type-Chernozem was selected as the main research object.Using the idea of substituting space for time
statistic analysis method and Principal Component Analysis(PCA)
the paper appraises and compares soil quality index quantitatively so as to further study soil quality evolution in the time series.Results indicate that soil quality index in the 30 year conversion fluctuates with time
showing a rising trend.The history of the conversion can be basically divided into three stages of the initial
middle and later periods.The initial period is the first 5 years after the conversion initiation
which is characterized by the sapling stage and a relative increase in soil quality index.The middle period ranges from 5 to 20 years after land conversion initiation.Conifer and broad-leaf forests grow rapidly in the period
and soil quality index increases greatly and reaches its peak.The later period is from 20 years after conversion initiation to current time.The period is the stable period characterized by the forest with dense canopy and a modest decline in soil quality index.After conversion for more than 25 years
forests will self-sparse
and soil quality index will rise to some extent and tend to be stable.
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