Soil phosphorus and relationship to phosphorus balance under long-term fertilization

被引:10
作者
Sun, Benhua [1 ,2 ]
Cui, Quanhong [1 ,2 ]
Guo, Yun [1 ,2 ]
Yang, Xueyun [1 ,2 ]
Zhang, Shulan [1 ,2 ]
Gao, Mingxia [3 ]
Hopkins, David W. [4 ,5 ]
机构
[1] Northwest A&F Univ, Coll Nat Resources & Environm, Yangling, Shaanxi, Peoples R China
[2] Northwest A&F Univ, Key Lab Plant Nutr & Agrienvironm Northwest China, Minist Agr, Yangling, Shaanxi, Peoples R China
[3] Northwest A&F Univ, Coll Water Resources & Architectural Engn, Yangling, Shaanxi, Peoples R China
[4] Royal Agr Univ, Cirencester, Glos, England
[5] Scotlands Rural Coll, Peter Wilson Bldg, Edinburgh, Midlothian, Scotland
关键词
loess soil; phosphorus activation coefficient; wheat-maize rotation; ACCUMULATION; MANAGEMENT; SYSTEMS; CROP;
D O I
10.17221/709/2017-PSE
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Temporal changes in the concentrations of plant-available phosphorus (P) in soil (Olsen-P), total soil-P and P activation coefficient (the ratio of Olsen-P to residual-P (i.e. an approximation to total-P)) were measured in plots that received consistent inorganic nitrogen, phosphorus and potassium plus organic fertilizers annually. Maize and winter wheat crops were grown in rotation for 24 years. Olsen-P and P activation coefficient declined significantly in the earlier years (< 12 years) for treatments that did not include any P fertilizer, and increased over the same period for the P-fertilized treatments. The rates of change in the Olsen-P and P activation coefficient values were positively related to P balance. In the later years, the Olsen-P and P activation coefficient plateau values were positively related to the P balance.
引用
收藏
页码:214 / 220
页数:7
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