Distribution Characteristics of Fine Roots of Plantations and Soil Properties in Semi-arid Loess Hilly Area
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Distribution Characteristics of Fine Roots of Plantations and Soil Properties in Semi-arid Loess Hilly Area
Bulletin of Soiland Water ConservationVol. 29, Issue 4, Pages: 27-31(2010)
作者机构:
1. 西北农林科技大学资源环境学院, 陕西杨凌,712100
2. 中国科学院水利部水土保持研究所, 陕西杨凌,712100
3. 浙江中冶勘测设计有限公司,浙江,杭州,310009
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Published:2010
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WANG Linlin, CHEN Yunming, ZHANG Fei, et al. Distribution Characteristics of Fine Roots of Plantations and Soil Properties in Semi-arid Loess Hilly Area[J]. Bulletin of Soiland Water Conservation, 2010, 29(4): 27-31.
DOI:
WANG Linlin, CHEN Yunming, ZHANG Fei, et al. Distribution Characteristics of Fine Roots of Plantations and Soil Properties in Semi-arid Loess Hilly Area[J]. Bulletin of Soiland Water Conservation, 2010, 29(4): 27-31.DOI:
Distribution Characteristics of Fine Roots of Plantations and Soil Properties in Semi-arid Loess Hilly Area
an investigation in the semi-arid loess hilly area was made on the vertical distribution of fine root characteristics and soil properties in the recovery of typical plantations. Results showed that fine root biomass
root length density(RLD)
root surface area
and specific root length(SRL) decreased significantly as soil depth increased. In the 0—60 cm soil layer
the averages of the fine root biomass
RLD
and root surface area for 14 a Hippophae rhamnoides(HR) were the highest; for 30 a Robinia pseudoacacia(RP)
less; and for 10 a RP
the lowest. The SRL of 10 a RP was the highest and the SRLs of 14 a HR and 30 a RP were the lowest. Dry layers obviously existed below soil depth of 150 cm in different plantations and the difference between arbor and shrub forests did not influence them significantly. Soil dry degree increased with the increasing of growth age. The improvement of tree forest to soil bulk density
which was greater than that of the two shrub forests
increased with the increasing of growth age. The vertical distribution of soil organic carbon was similar to roots. In the 0—60 cm soil layer
organic carbon contents of 24 a HR and 50 a RP were the highest and organic carbon content of 10 a RP was the lowest.