Spatio-temporal variability of biophysical parameters of irrigated maize using orbital remote sensing

This study proposes to estimate the actual crop evapotranspiration, using the SAFER model, as well as calculate the crop coefficient (Kc) as a function of the normalized difference vegetation index (NDVI) and determine the biomass of an irrigated maize crop using images from the Operational Land Ima...

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Veröffentlicht in:Semina. Ciências agrárias : revista cultural e científica da Universidade Estadual de Londrina 2021-07, Vol.42 (4), p.2181-2201
Hauptverfasser: Costa, Taiara Souza, dos Santos, Robson Argolo, Santos, Rosangela Leal, Filgueiras, Roberto, da Cunha, Fernando Franca, Pereira, Anderson de Jesus, de Salles, Rodrigo Amaro
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Sprache:eng
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Zusammenfassung:This study proposes to estimate the actual crop evapotranspiration, using the SAFER model, as well as calculate the crop coefficient (Kc) as a function of the normalized difference vegetation index (NDVI) and determine the biomass of an irrigated maize crop using images from the Operational Land Imager (OLI) and Thermal Infrared (TIRS) sensors of the Landsat-8 satellite. Pivots 21 to 26 of a commercial farm located in the municipalities of Bom Jesus da Lapa and Serra do Ramalho, west of Bahia State, Brazil, were selected. Sowing dates for each pivot were arranged as North and South or East and West, with cultivation starting firstly in one of the orientations and subsequently in the other. The relationship between NDVI and the Kc values obtained in the FAO-56 report (Kc(FAO)) revealed a high coefficient of determination (R-2 = 0.7921), showing that the variance of Kc(FAO) can be explained by NDVI in the maize crop. Considering the center pivots with different planting dates, the crop evapotranspiration (ETc) pixel values ranged from 0.0 to 6.0 mm d(-1) during the phenological cycle. The highest values were found at 199 days of the year (DOY), corresponding to around 100 days after sowing (DAS). The lowest BIO values occur at 135 DOY, at around 20 DAS. There is a relationship between ETc and BIO, where the DOY with the highest BIO are equivalent to the days with the highest ETc values. In addition to this relationship, BIO is strongly influenced by soil water availability.
ISSN:1676-546X
1679-0359
1679-0359
DOI:10.5433/1679-0359.2021v42n4p2181