Variabilidade do fósforo extraído causada pela variação analítica nos métodos Mehlich - 1 e 3

• Ano de defesa: 2013
• Autor(a) principal: Santos, Lenio da Silva
• Tipo de documento: Dissertação
• Tipo de acesso: Acesso aberto
• dARK ID: ark:/26339/001300000d2db
• Idioma: por
• Instituição de defesa: Universidade Federal de Santa Maria; BR; Agronomia; UFSM; Programa de Pós-Graduação em Ciência do Solo
• Palavras-chave em Português: Fontes de variabilidade; Fósforo; Mehlich -1 e 3; Sources of variability; Phosphorus; Mehlich -1 and 3; CNPQ::CIENCIAS AGRARIAS::AGRONOMIA::CIENCIA DO SOLO
• Link de acesso: http://repositorio.ufsm.br/handle/1/5572

Performing a soil analysis requires a series of operations so a specific element may be conveniently extracted to be then detected or measured. Protocol methods have been adjusted to facilitate the execution, however here may be variability in analytical results by different laboratories even if they follow the same general principles of the method. This study aimed to identify sources of variability that affect analytical precision and accuracy of phosphorus extracted by Mehlich-1 and Mehlich-3 under variations in protocol procedures. Eleven soil samples in the surface layer (0 - 20 cm) were selected and collected in the geomorphologic Plateau and Central Depression of Rio Grande do Sul state, Brazil, which have wide variation of physical, chemical and mineralogical composition, including different clay contents and phosphorus availability. In the laboratory, seven experiments were conducted to determine the effect of different factors: sample particle size (<0.30, <0.60, <0.85, <1.70 and <2.00 mm), extraction container type (Erlenmeyer and snap-cap ), the void volume of the container (6.0, 17.0, 22.5, 33.5 and 39.0 ml), the shaking frequency (80, 100, 120, 140 and 160 oscillations per minute - opm), time to rest solution after shaking (8, 12, 16, 20 and 24 h), reaction time of the phosphomolybidic complex used as a reducing agent (15, 30, 45, 60 and 120 minutes) and environmental temperature (15, 20, 25, 30 and 35 °C). The results indicate that the particle size of the soil samples did not significantly affect the amount of phosphate extracted by the Mehlich-1 solution. However, for Mehlich-3 solution, particle size of the samples had an effect being more pronounced in soil phosphorus with medium and high availability. The use of snap-cap type containers optimized the quantities of phosphorus extracted by Mehlich-1 solution when compared with Erlenmeyer container. For the Mehlich-3, there is a combined effect of the type of container with the soil mineralogy and phosphorus content in the sample. The amount of phosphorus extracted significantly increased by increasing the void volume of the container for Mehlich-1. For Mehlich-3 solution, the amounts of phosphorus were affected by the void volume of the flask, but did not have the same behavior as Mehlich-1. Shaking frequency above 120 opm caused an increased amount of extracted phosphorus by Mehlich-1 and Mehlich-3. Resting time up to 16 h increased the amount of phosphorus extracted by Mehlich-1 conversely for Mehlich-3 this resting time caused a reduction in the amount of phosphorus extracted. The phosphomolybdic complex tends to stabilize within a range of 30 to 60 minutes for both Mehlich-1 and Mehlich-3. The temperature had no predominant effect on the extraction capacity of Mehlich-1 and Mehlich-3.