G. Ramirezoliveras et al., HYDROGEN-ION EFFLUX DIFFERENCES IN SOYBEAN ROOTS ASSOCIATED WITH YIELDS, The Journal of agriculture of the University of Puerto Rico, 81(3-4), 1997, pp. 159-180
Significant differences in hydrogen ion (H+) efflux from soybean roots
among soybean cultivars were found ranging from 0.5 to 2.4 pH units i
n 24 h. The hydrogen ion efflux was positively correlated with the cul
tivar's seed yield in three different soil series. On highly leached,
low cation exchange capacity (CEC) Oxisol (less than 10 cmol/kg), the
cultivars with high H+ efflux capacity yielded highest and accumulated
the highest amount of nutrients at flowering. All macronutrients, exc
ept for Ca and Mg, decreased at the beginning of the seed stage. Hydro
gen ion efflux was positively correlated to leaf K and the K/(Ca + Mg)
ratio.The K/(Ca + Mg) ratio was positively correlated to biomass and
yields, thus suggesting nutrient accumulation up to seed production. R
esults from the medium CEC Ultisol (10 to 20 cmol/kg) were similar to
those from the low CEC soil. On the high CEC Vertisol (above 35 cmol/k
g), the cultivars with high H+ efflux depleted the rhizosphere soil zo
ne for K faster than those with low H+ efflux, giving positive correla
tions for seed and biomass yields but negative correlations with leaf
K and the K/(Ca+Mg) ratio.