PHOSPHORUS EXTRACTED BY ION EXCHANGE RESINS AND MEHLICH-1 FROM OXISOLS (LATOSOLS) TREATED WITH DIFFERENT PHOSPHORUS RATES AND SOURCES FOR VARIED SOIL-SOURCE CONTACT PERIODS

被引:29
|
作者
de Freitas, Irio Fernando [1 ]
Novais, Roberto Ferreira [2 ]
de Albuquerque Villani, Ecila Merces [3 ]
Novais, Sarah Vieira [2 ]
机构
[1] Fed Univ Vicosa UFV, Soil Dept, BR-36570000 Vicosa, MG, Brazil
[2] Univ Fed Vicosa, Soil Dept, Vicosa, MG, Brazil
[3] UFV FAPEMIG Scholarsphip, Soil Dept, Vicosa, MG, Brazil
来源
REVISTA BRASILEIRA DE CIENCIA DO SOLO | 2013年 / 37卷 / 03期
关键词
phosphorus fertilizers; rock phosphates; phosphorus extractants; PHOSPHATE; AVAILABILITY; DISSOLUTION; CALCIUM; SIZE;
D O I
10.1590/S0100-06832013000300013
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Despite the large number of studies addressing the quantification of phosphorus (P) availability by different extraction methods, many questions remain unanswered. The aim of this paper was to compare the effectiveness of the extractors Mehlich-1, Anionic Resin (AR) and Mixed Resin (MR), to determine the availability of P under different experimental conditions. The laboratory study was arranged in randomized blocks in a [(3 x 3 x 2) + 3] x 4 factorial design, with four replications, testing the response of three soils with different texture: a very clayey Red Latosol (LV), a sandy clay loam Red Yellow Latosol (LVA), and a sandy loam Yellow Latosol (LA), to three sources (triple superphosphate, reactive phosphate rock from Gafsa-Tunisia; and natural phosphate from Araxa-Minas Gerais) at two P rates (75 and 150 mg dm(-3)), plus three control treatments (each soil without P application) after four contact periods (15, 30, 60, and 120 days) of the P sources with soil. The soil acidity of LV and LVA was adjusted by raising base saturation to 60 % with the application of CaCO3 and MgCO3 at a 4: 1 molar ratio (LA required no correction). These samples were maintained at field moisture capacity for 30 days. After the contact periods, the samples were collected to quantify the available P concentrations by the three extractants. In general, all three indicated that the available P-content in soils was reduced after longer contact periods with the P sources. Of the three sources, this reduction was most pronounced for triple superphosphate, intermediate for reactive phosphate, while Araxa phosphate was least sensitive to the effect of time. It was observed that AR extracted lower P levels from all three soils when the sources were phosphate rocks, while MR extracted values close to Mehlich-1 in LV (clay) and LVA (medium texture) for reactive phosphate. For Araxa phosphate, much higher P values were determined by Mehlich-1 than by the resins, because of the acidity of the extractor. For triple superphosphate, both resins extracted higher P levels than Mehlich-1, due to the consumption of this extractor, particularly when used for LV and LVA.
引用
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页码:667 / 677
页数:11
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