Vegetation Restoration and Soil Nutrient Changes in Edge of Tengger Desert
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Vegetation Restoration and Soil Nutrient Changes in Edge of Tengger Desert
Bulletin of Soiland Water ConservationVol. 32, Issue 6, Pages: 107-111(2013)
作者机构:
宁夏大学农学院,宁夏,银川,750021
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Published:2013
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SHI Ming, WANG Rui, SUN Quan, et al. Vegetation Restoration and Soil Nutrient Changes in Edge of Tengger Desert[J]. Bulletin of Soiland Water Conservation, 2013, 32(6): 107-111.
DOI:
SHI Ming, WANG Rui, SUN Quan, et al. Vegetation Restoration and Soil Nutrient Changes in Edge of Tengger Desert[J]. Bulletin of Soiland Water Conservation, 2013, 32(6): 107-111.DOI:
Vegetation Restoration and Soil Nutrient Changes in Edge of Tengger Desert
In order to study the soil nutrients and pH value at different revegetation stages in the edge of Tengger Desert
we selected six kinds of vegetation recovery phase soil from east to west
and tested pH value
organic matter total and available nutrients.The results showed that:in the process of sand dune fixation
soil organic matter and total nitrogen exhibited an increasing trend
respectively from 1.32 and 0.025g/kg ro 1.89 and 0.061 g/kg which reached a significant level.Available nitrogen and available potassium in the semi-fixed sand dunes were significantly increased.Due to the large number of plants growth soil available nitrogen and potassium contents in the fixed sand dunes were lower than that in the semi-fixed sand dunes.Desert grassland had a higher content in soil organic matter
total nitrogen and available nitrogen
and degraded desert grassland had slightly higher available phosphorus than that of the desert grassland.With the restoration process of degraded desert grassland
available phosphorus in the artificial Haloxylon forest declined and available potassium increased.Artificial Haloxylon Haloxylon forest had a low pH value.In vegetation recovery process
the presence of sand vegetation played a decisive role of nitrogen and organic matter enrichment.With the fixing of sand dunes and restoration of vegetation
soil organic matter
nitrogen and phosphorus contents increased
and the soil organic matter content had a strong positive correlation with soil total nitrogen