Calibration and management of porous cap soil solution samplers and pressure transducers for monitoring fertigation ions / Calibração e manejo de extratores providos de cápsulas porosas e transdutores de pressão para monitoramento de íons na fertirrigação

AUTOR(ES)
DATA DE PUBLICAÇÃO

2010

RESUMO

The fertigation management with ion concentration control in the soil solution its an alternative technique and feasible economic, however its necessary to calibrate it to be effectively recommended. This work had the aim to determine calibrated equations to monitor the electrical conductivity (EC) and the solution ion concentration in soils of two different textures, with primary focus on different vacuum intensity, vacuum application time after the irrigation event and time after the vacuum application for collection of soil solution. The study consisted of two experiments under greenhouse condition. The statistic delineation utilized was the entirely randomized and the soil types were the same for both experiments; the first in the factorial scheme was 2 x 4 x 4, 32 treatments in the all, with three repetition. The treatments were composed of: two soil type ( loamsandy - S1 and loam-clayish- S2), four vacuum intensity applied to extractors (V1 - 50, V2 - 60, V3 - 70, and V4 - 80 kPa) and four levels of water content on weight base ( 100, 72, 61 e 43% in the soil S1 and 100, 79, 66 and 60% in the soil S2 ); the second in the factorial scheme was 2 x 4 x 3, 24 treatments in all, with three repetition. The treatments had four types of solution with concentration of the 0, 30, 60 e 90% in the utilized standard solution and three vacuum intensity (V1 - 60, V2 - 70, V3 80 kPa). The results showed that its possible, to monitor the volume and ionic concentration of extracted solution with high precision and also the tension variation in real time with the help of extractors and pressure to transductors. The minimum time for ionic equilibrium was the 30 hours after the fertigation event to apply the vacuum in both soils. The necessary time between vacuum applications until the moment of collection of solution, increased with the reduction of water content in soil, and also due to increment in the applied vacuum. The smaller time range observed was from the 0.37 to 0.67 hours under the combination of the maximum water content in both soils with the bigger and smaller vacuum intensity, respectively. The water content reduction resulted an increase in the ionic concentration and electrical conductivity. The vacuum increment did not affect ionic concentration in both soils, except for K+, Ca2+, Mg2+ and SO4 2-, which were reduced in the soil S1 and the collected volume increased. The increasing level of the applied concentration provided an increase in the ionic concentration and in the EC of the obtained solution, except for pH, that which reduced in the soil S2; the applied vacuum increment did not affect significantly evaluated parameters in both soils in the second experiment.

ASSUNTO(S)

Íon vacuum. soil moisture vácuo. Íons soils properties physic-chemical umidade do solo solos - propriedades físico-químicas fertigation fertirrigação

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