2015
DOI: 10.1007/s11104-015-2784-y
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Poor regulation of phosphorus uptake and rhizosphere carboxylates in three phosphorus-hyperaccumulating species of Ptilotus

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Cited by 9 publications
(3 citation statements)
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“…The exudation rate for C. arietinum (C) would allow accumulation of the carboxylate amounts present in the rhizosheath in <1 h. This rapid exudation could perhaps be a response to fast microbial degradation, as found for citrate and malonate (Martin et al 2016), or losses through soil sorption (Suriyagoda et al 2016). However, these factors would have had relatively little impact in the river sand used in our experiment, as soil sorption and microbial degradation are minimal (Ryan et al 2012).…”
Section: Exudation Ratesmentioning
confidence: 97%
“…The exudation rate for C. arietinum (C) would allow accumulation of the carboxylate amounts present in the rhizosheath in <1 h. This rapid exudation could perhaps be a response to fast microbial degradation, as found for citrate and malonate (Martin et al 2016), or losses through soil sorption (Suriyagoda et al 2016). However, these factors would have had relatively little impact in the river sand used in our experiment, as soil sorption and microbial degradation are minimal (Ryan et al 2012).…”
Section: Exudation Ratesmentioning
confidence: 97%
“…Oburger [ 99 ] found that the adsorption and desorption isotherms of organic acids could be described by the Freundlich equation and the dynamic sorption model. This model succeeds in both predicting the solid solution partitioning of citrate in soils and demonstrating the plateau and steady state concentrations of citrate in solution, highlighting the key effects of organic acid dynamics on the P i adsorption-desorption reactions and the functional roles of PSM in soil [ 98 , 100 ].…”
Section: Psm-derived P Desorption From Clay Mineralsmentioning
confidence: 99%
“…3a, b), suggesting that the loss of each OA by microbial degradation or mineral adsorption in the rhizosphere was in proportion to what were produced by plants and hence the treatment effects were similar for those two measures. However, for M. stipoides acetic acid was observed in OA rhizo but not in OA exuded : this likely reflected acetic acid being derived from rhizosphere microbes (Suriyagoda et al 2016). On the other hand, fumaric acid from M. stipoides and E. tereticornis was less abundant in OA rhizo than OA exuded , suggesting it was rapidly degraded by microbes or adsorbed onto soil particles.…”
Section: Discussionmentioning
confidence: 83%