Characteristics of Soil Water Stable Aggregates and Relationship with Soil Properties During Vegetation Rehabilitation in Ningxia Loess Hilly Region
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Characteristics of Soil Water Stable Aggregates and Relationship with Soil Properties During Vegetation Rehabilitation in Ningxia Loess Hilly Region
Vol. 20, Issue 1, Pages: 72-75(2006)
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CLC:S152.3S153
Published:2006
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YANG Jian-guo, AN Shao-shan, ZHANG Fen-li. Characteristics of Soil Water Stable Aggregates and Relationship with Soil Properties During Vegetation Rehabilitation in Ningxia Loess Hilly Region[J]. 2006, 20(1): 72-75.
DOI:
YANG Jian-guo, AN Shao-shan, ZHANG Fen-li. Characteristics of Soil Water Stable Aggregates and Relationship with Soil Properties During Vegetation Rehabilitation in Ningxia Loess Hilly Region[J]. 2006, 20(1): 72-75.DOI:
Characteristics of Soil Water Stable Aggregates and Relationship with Soil Properties During Vegetation Rehabilitation in Ningxia Loess Hilly Region
Based on the field investigation and indoor analysis
we study on the characteristics of soil water-stable aggregates and soil properties during vegetation rehabilitation in typical grassland of hilly-gullied loess area
and analysis the relationship between them by canonical correlation analysis.The results show that: In terms of vegetation succession stages
the contents of big gravel soil water-stable aggregates increased
the >5 mm aggregate is priority in different layers
about 50%~80%.The 5~2 mm aggregate is second main component.The mean value of >5 mm aggregate in 2 m layers show that Stipa gradiss Community >Stipa bungana Trin Community>Artemisia sacrorum Ledeb community>Thymus mongolicus Ronn community>Hierochloe ordorata community.Physical clay
organic matter and total nitrogen are the key factors that influenced the total water-stable aggregates.Total nitrogen and organic matter are the comprehensive factor that influenced the water stable macroaggregates which are >5 mm and 1~0.5 mm.The ferralic oxide
ferralic aluminum and physical clay are the comprehensive factor which influence the water stable microaggregates which are 2~1 mm and 0.5~0.25 mm.The main factors can be divided into comprehensive physical factor(physical clay and clay)
comprehensive chemical factor(total nitrogen
organic matter) and comprehensive mineral factor(ferralic oxide and ferralic aluminum).