Iron Availability as Affected by Soil Moisture in Intercropped Peanut and Maize

Abstract

Pot and rhizobox experiments were carried out to investigate the iron availability in intercropped peanut and maize as affected by soil moisture. Results from pot experiment showed that the root growth of peanuts were significantly inhibited at 25% soil water content compared to those at 15% soil water content. The chlorophyll content in the new leaves of intercropped peanut decreased and leaves became chlorotic at 25% soil water content. There were no significant differences in the active iron concentration in new leaves of peanut between 15% and 25% soil water content. The soil pH were higher in peanut rhizosphere than in bulk soil at the early, middle, and harvest stages for both 15% and 25% soil water content. The soil bicarbonate content was also higher in peanut rhizosphere than in bulk soil for both 15% and 25% soil water content. There was significant difference in soil bicarbonate of peanut rhizosphere between 15% and 25% soil water content at the harvest stage. The available iron content in both rhizosphere soil and bulk soil were lower than 3.5 mg kg−1 in all growth stages at both 15% and 25% soil water content. Results from rhizobox experiment showed that citric acid, maleic acid, and fumaric acid in exudates of peanuts significantly increased at 25% soil water content compared to that at 15% soil water content. The apoplastic iron content of peanut roots decreased by 0.216 and 0.409 µmol g−1 fresh weight−1 (FW) from the 28th growth day to 42nd growth day at 25% and 15% soil water content, respectively. The mobilizing ability of apoplastic iron in intercropped peanuts at 15% soil water content was 20.1% higher compared to that at 25% soil water content. It is concluded that improvement of iron nutrition of peanuts with intercropping with maize could be affected by soil moisture condition.