Expansion of palm oil (Elaeis guineensis Jacq.) in the state of Maranhão and soil water deficit limitations in the Brazilian Amazon

Abstract

Oil palm is considered the crop with the highest oil production per planted area unit. This condition has driven the Brazilian government to create the Sustainable Oil Palm Production Program. Since 2009, the agroenergy production chain has used oil palm as a viable and profitable crop to recover deforested areas in the Amazon. The aim of this study was to assess hydric conditions able to indicate the potential to expand oil palm crops in the state of Maranhão, even in the Legal Amazon. The climate database used (average and extreme temperature in degrees Celsius; rainfall values; relative humidity, and vapour-pressure deficit). Water deficit values were was obtained by comparing the potential evapotranspiration of oil palm (ETc) to actual rainfall (ER). Water balance was calculated based on available water capacity of 125 mm.month -1 . Evapotranspiration was obtained using the methodology according to the climate database available to calculate the evapotranspiration rate in an area planted with oil palm in this study. The water deficit values show no restriction in the soil water replacement between January and June. However, from July to December, the water deficit varies between 200 and 300 mm. The levels showed that, in the areas evaluated, oil palm crops will require irrigation. In this period, yield was estimated at 17 tons ha -1 when the water deficit was considered at 210 mm and 14 tons ha -1 for a deficit of 380 mm. This result reinforces that oil palm production may drop by more than 50% due to water deficits and the crop will greatly impact the economy and the environment if the irrigation strategy is adopted in the areas of Maranhão.

Water requirement of oil palm in two different edaphoclimatic conditions in Brazil

“…According to Köppen's climate classification, the climate in the area is Tropical rainforest (Af) characterized by rains well distributed throughout the year. Precipitation ranges 2500−3000 mm yr -1 with the driest period occurring between July and December, which has rainfall above 60 mm (SUDAM, 1984;Martorano et al, 2017). Mean temperature is 26 °C ± 3 °C (Benami et al, 2018) and relative air humidity is between 80-85% yearly, associated to the rainfall regime (Martorano et al, 1993).…”