RESIDUAL PHOSPHATE FERTILIZER COMPOUNDS IN SOILS .2. THEIR INFLUENCE ON SOIL TESTS FOR AVAILABLE PHOSPHATE

被引:11
|
作者
KUMAR, V
GILKES, RJ
BOLLAND, MDA
机构
[1] Soil Science and Plant Nutrition, School of Agriculture, The University of Western Australia, Nedlands, 6009, W.A.
[2] Western Australian Department of Agriculture, Baron-Hay Court, South Perth, 6151, W.A.
来源
FERTILIZER RESEARCH | 1991年 / 30卷 / 01期
关键词
RESIDUAL PHOSPHATE FERTILIZER COMPOUNDS IN SOIL; SOIL TESTING FOR PHOSPHATE;
D O I
10.1007/BF01048824
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Six phosphate (P) compounds, including soil minerals and fertilizer residues, were extracted with eight standard soil P-test reagents. In the absence of soil, the solubility of P differed greatly depending upon P compound type and extractant. For example an aluminium phosphate was almost completely soluble in Bray-1 reagent yet it was insoluble in Morgan reagent. P sorbed by calcium carbonate was insoluble in acid Bray-1 reagent but soluble in the alkaline Colwell soil test. In the presence of soil, the amounts of P extracted from the compounds were commonly reduced by sorption of dissolved P by the soil. For example, most dissolved P was sorbed by the soil from an ammonium sulphate solution whereas relatively little P was sorbed by soil from the Bray-1 reagent. The strong influence of the type of P compound on the solubility of P in soil test reagents might be partly responsible for the need for different calibration curves of P soil test versus plant yield for soils that have received different types of P fertilizer.
引用
收藏
页码:31 / 38
页数:8
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