Dissertação
Balanço e evolução temporal de teores de fósforo e potássio no solo em áreas manejadas com agricultura de precisão
Fecha
2011-08-31Registro en:
MONTIEL, Luis Ramiro Samaniego. Soil phosphorus and potassium levels budget and temporal evolution farming management areas. 2011. 135 f. Dissertação (Mestrado em Agronomia) - Universidade Federal de Santa Maria, Santa Maria, 2011.
Autor
Montiel, Luis Ramiro Samaniego
Institución
Resumen
The need for improving nutrient use efficiency and increase savings demand a better
knowledge of soils and production systems. The objective of this study was to
evaluate the soil P and K budget and its relationships with their temporal evolution on
site-specific management areas. The experiments were carried out in four cropland
areas from the Medium Plateau region of the Rio Grande do Sul state, located at the
cities of Almirante Tamandaré do Sul, Tio Hugo, Não-Me-Toque and Vitor Graeff.
Soil tests were used to verify the spatial variability, budget and temporal evolution of
soil P and K levels by the comparison of the years of 2005 and 2009. Regression
analysis was performed by the software JMP IN v.3.2.1 to evaluate the relationship
between P and K budget and the temporal evolution of soil P and K levels. Cropland
areas showed high spatial variability for P and K soil test levels at the beginning of
the study, which was decreased by applying precision farming techniques.
Relationships between P and K budget and the temporal evolution of soil P and K
test levels were positive with the exception of the Vitor Graeff area which showed
negative P and K budget. P and K fertilization were 30 and 25% higher in relation to
their exportation, respectively. On average, soybean extracted 44 kg P2O5 ha-1 and
63 kg K2O ha-1, while the maize exported 78,5 kg P2O5 ha-1 and 59 kg K2O ha-1.
Temporal evolution of soil P and K test levels was high when P and K budget was
low and there was a low temporal evolution when the P and K budget was high. On
the average of the four cropland areas there were necessary the input of 12,0 kg
P2O5 ha-1 to increase 1 mg dm-3 of soil P test levels and the input of 4,1 kg K2O ha-1
to increase 1 mg dm-3 of soil K test levels.