Site-specific phosphorus application based on the kriging fertilizer-phosphorus availability index of soils

被引:17
|
作者
Juang, KW
Liou, DC
Lee, DY [1 ]
机构
[1] Ming Dao Univ, Dept Post Modern Agr, Changhua, Taiwan
[2] Natl Taiwan Univ, Grad Inst Agr Chem, Taipei 10764, Taiwan
关键词
D O I
10.2134/jeq2002.1248
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Site-specific phosphorus management is done to optimize crop production and minimize P loss from soils. The spatial variability of the available P prior to fertilizer application and the P-fixation tendency of soil both need to be taken into account for variable-rate P application. The objectives of this research were to document the spatial variability of the fertilizer-P availability index, which shows the P-fixation tendency, and to develop a strategy that takes the spatial distribution of this index into account for site-specific phosphorus application. In this study, the spatial patterns of the fertilizer-P availability index were characterized by using geostatistics. The ordinary kriging was used for spatial interpolation of the fertilizer-P availability index. Because the fertilizer-P availability index of soil is related to oxalate-extractable Fe and Al and because measuring oxalate-extractable Fe and Al is much easier than directly determining the fertilizer-P availability index, the spatial distribution of the fertilizer-P availability index can be obtained using the oxalate-extractable Fe and A] data. The spatial distribution of Olsen-extractable P, which was used to measure the available-P status prior to fertilizer-P application, was also estimated by using ordinary kriging. The required fertilizer-P amounts were then determined using the kriging estimates of the fertilizer-P availability index and Olsen-extractable P. A fertilizer-P recommendation map for the 430-ha study site in Changhua county, Taiwan was generated by using this approach for illustration. The proposed method for generating fertilizer-P recommendation maps can be used for variable-rate application to maintain an adequate P status for crop production and to potentially reduce the P loss from soils.
引用
收藏
页码:1248 / 1255
页数:8
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