RE-SORPTION OF ORGANIC-COMPOUNDS BY ROOTS OF ZEA-MAYS L AND ITS CONSEQUENCES IN THE RHIZOSPHERE .2. EXPERIMENTAL AND MODEL EVIDENCE FOR SIMULTANEOUS EXUDATION AND RE-SORPTION OF SOLUBLE C COMPOUNDS
Dl. Jones et Pr. Darrah, RE-SORPTION OF ORGANIC-COMPOUNDS BY ROOTS OF ZEA-MAYS L AND ITS CONSEQUENCES IN THE RHIZOSPHERE .2. EXPERIMENTAL AND MODEL EVIDENCE FOR SIMULTANEOUS EXUDATION AND RE-SORPTION OF SOLUBLE C COMPOUNDS, Plant and soil, 153(1), 1993, pp. 47-59
The exudation of soluble carbon compounds from Zea mays roots was inve
stigated over a 10 day growth period under sterile and non-sterile sol
ution culture conditions. The results showed that plants grown in ster
ile static solution culture, where C was allowed to accumulate, releas
ed 8 times less C than plants grown under culture conditions in which
the solutions were replaced daily. The increased C loss from plant cul
tures in which exudates were removed daily was attributable to, (a) th
e reduced potential for root re-sorption of previously lost C, and (b)
, increasing diffusion gradients between the root and the surrounding
bathing solution increasing passive leakage of exudates from the roots
. In treatments where C was removed daily from the root-bathing soluti
on, 86% of the total C lost was of a soluble low molecular weight natu
re, whereas, in sterile and non-sterile static cultures, allowing the
accumulation of C over 10 days, this was reduced to 67.5 and 48% respe
ctively. The main C fluxes operating in a solution culture system (eff
lux and influx of C by both roots and microorganisms) were examined us
ing a computer simulation model to describe movement of soluble sugar-
C in both sterile and non-sterile conditions. In sterile static cultur
es where C was allowed to accumulate in solution over a 10 day growth
period, 98% of the C exuded was re-absorbed by the plant. Where C was
removed daily from the root-bathing solution this was reduced to 86%.
The predicted patterns of C accumulation were similar to those found i
n the experiments. Simulations showed that the pattern of accumulation
and final equilibrium concentrations were dependent on the rate of ex
udation, the spatial characteristics of exudation, solution volume, ro
ot growth rate and the presence of a microbial population. Simulations
under non-sterile conditions showed that roots can compete with micro
organisms for exudates in solution indicating the possible importance
of re-sorption in a soil environment. The results clearly indicate tha
t roots are capable of regulating the net amount of C released into a
solution culture with the amount of C collected being highly dependent
on the experimental conditions employed. The possible implications of
soluble C influx on processes operating within the rhizosphere and in
experimental systems is discussed.