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

Citation
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
Citations number
40
Categorie Soggetti
Agriculture Soil Science","Plant Sciences",Agriculture
Journal title
ISSN journal
0032079X
Volume
153
Issue
1
Year of publication
1993
Pages
47 - 59
Database
ISI
SICI code
0032-079X(1993)153:1<47:ROOBRO>2.0.ZU;2-F
Abstract
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.