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Effects of Land Use Types on Phosphorus Forms and Their Contents in Soil Aggregates in Watershed of Hongfeng Lake
  
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KeyWord:Hongfeng Lake watershed; land use; aggregate; phosphorus content; phosphorus form
Author NameAffiliation
YANG Hua Guizhou Key Laboratory of Mountain Environment, Guizhou Normal University, Guiyang 550001 
LONG Jian Guizhou Key Laboratory of Mountain Environment, Guizhou Normal University, Guiyang 550001 
LI Zhao-jun Institute of Agricultural Resources and Regional Planning, China Academy of Agricultural Sciences, Beijing 100081 
LIAO Hong-kai Guizhou Key Laboratory of Mountain Environment, Guizhou Normal University, Guiyang 550001 
LIU Ling-fei Guizhou Key Laboratory of Mountain Environment, Guizhou Normal University, Guiyang 550001 
LI Juan Department of Geography and Environment Science, Guizhou Normal University, Guiyang 550001 
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Abstract:
      Excessive phosphorus(P) in soils may increase the potential to pollute water through runoff and/or leaching. Different land use types may change phosphorus mobility. A study was performed to examine the chemical forms and their contents of P in bulk soil and soil aggregates at 0~15 cm and 15~30 cm under four land use types:cornfields, vegetable fields, forest land and abandoned land in the watershed of Hongfeng Lake in Anshun, Guizhou Province. Total P contents in bulk soils and soil aggregates were in order of cornfields>vegetable fields>abandoned land>forest land under different land use types. Residual P, NaOH-P, and NaHCO3-P were the major forms in soil aggregates at each depth. The residual P was the highest among all P forms in soils under four land use types, and ranged 28.3%~45.4%, 61.1%~72.7%, 45.9%~53.0% and 52.1%~72.4% in cornfield, forest land, vegetable field and abandoned land, respectively. The organic P contents were as about 2 times as inorganic P contents in cornfield and vegetable field. Soil P was mainly present in soil aggregates of 5~2 mm and 2~0.5 mm, accounting for more than 77% of soil total P. Phosphorus in aggregates of 5~2 mm and 2~0.5 mm in cultivated soils including cornfield and vegetable field were the main contributors to lake P and could be the key factor of the lake eutrophication.