Physical and Chemical Properties of Soil Crust in Salix Gordejevii Sand Barrier with Different Distances of Row Spacing
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Physical and Chemical Properties of Soil Crust in Salix Gordejevii Sand Barrier with Different Distances of Row Spacing
Bulletin of Soiland Water ConservationVol. 27, Issue 5, Pages: 86-90(2008)
作者机构:
1. 内蒙古农业大学 生态环境学院,内蒙古,呼和浩特,010019
2. 内蒙古林业科学研究院,内蒙古,呼和浩特,010010
3. 锡林郭勒盟水土保持工作站, 内蒙古 锡林浩特,026000
4. 内蒙古水文总局,内蒙古,呼和浩特,010010
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Published:2008
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SHI Xiao-dong, HU Xiao-long, GAO Yong, et al. Physical and Chemical Properties of Soil Crust in Salix Gordejevii Sand Barrier with Different Distances of Row Spacing[J]. Bulletin of Soiland Water Conservation, 2008, 27(5): 86-90.
DOI:
SHI Xiao-dong, HU Xiao-long, GAO Yong, et al. Physical and Chemical Properties of Soil Crust in Salix Gordejevii Sand Barrier with Different Distances of Row Spacing[J]. Bulletin of Soiland Water Conservation, 2008, 27(5): 86-90.DOI:
Physical and Chemical Properties of Soil Crust in Salix Gordejevii Sand Barrier with Different Distances of Row Spacing
Based on field experiment and comparative analysis
physical and chemical properties of soil crust at the base of the Salix gordejevii sand barrier with row spacing of 5 m and 8 m and at 2 m away from the base(for contrast) are investigated.Results show that soil is alkaline at the base of the two row Salix gordejevii sand barrier
while soil at 2 m away from the base is acidic.The soils in the 5 m and 8 m row spacing sand barriers do not have significant difference in pH value.The content of organic matter
total N
and total P at the base of the sand barrier are greater than the contrast.Compared with the base and the location 2 m away from the base
available nutrients in both 5 m row spacing and 8 m row spacing are higher and available N are lower than the contrast.Both available N and available P in 8 m row spacing sand barrier are greater than those in 5 m row spacing sand barrier.The formation of soil crust in the Salix gordejevii sand barrier is a physical process which takes sand grains as skeleton and fill soil pore space with the fine kernel(d0.02 mm).
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