2003
DOI: 10.1023/a:1022371130939
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Origins of root-mediated pH changes in the rhizosphere and their responses to environmental constraints: A review

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Cited by 1,204 publications
(570 citation statements)
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References 121 publications
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“…Organic acids in the soil, produced from root exudates, may compete for the same binding sites as P, depressing the P sorption strength of the soil (Ylivainio et al, 2008). The exudation of organic anions by the roots has been found to occur in the rhizosphere, associated with NO3 − -N nutrition in preference to NH 4 + -N (Marschner, 1995;Hinsinger et al, 2003); also, localized release of H + by some portions of the roots has been reported to occur as a response to P deficiency, favoring P solubility in the soil (Hinsinger et al, 2003). Jones (1998) reported two mechanisms of P release in the soil rhizosphere: direct ligand exchange, whereby citrate directly replaces P on ligand exchange surfaces, and complexation with metal ions in the solid phase, which constitutes the exchange matrix holding P (such as Ca 2+ in rock phosphate).…”
Section: Nutrient Uptake and Accumulation By L Multiflorummentioning
confidence: 99%
“…Organic acids in the soil, produced from root exudates, may compete for the same binding sites as P, depressing the P sorption strength of the soil (Ylivainio et al, 2008). The exudation of organic anions by the roots has been found to occur in the rhizosphere, associated with NO3 − -N nutrition in preference to NH 4 + -N (Marschner, 1995;Hinsinger et al, 2003); also, localized release of H + by some portions of the roots has been reported to occur as a response to P deficiency, favoring P solubility in the soil (Hinsinger et al, 2003). Jones (1998) reported two mechanisms of P release in the soil rhizosphere: direct ligand exchange, whereby citrate directly replaces P on ligand exchange surfaces, and complexation with metal ions in the solid phase, which constitutes the exchange matrix holding P (such as Ca 2+ in rock phosphate).…”
Section: Nutrient Uptake and Accumulation By L Multiflorummentioning
confidence: 99%
“…Interestingly, malonate has been labeled a potential inhibitor of microbial respiration due to its inhibition of succinate dehydrogenase, a key enzyme of the citric acid cycle (Ikuma and Bonner, 1967;Li and Copeland, 2000;Phillips et al, 2012). However, our results show that malonate greatly increases soil respiration.…”
Section: Citrate and Malonate Enhanced Microbial Activity In Uncontammentioning
confidence: 55%
“…The fact that soil pH was highest in the treatment with the greatest cumulative CO 2 evolution (citrate) is consistent with this scenario. However, the increase in soil pH may also be due to the reaction of carboxylate ions with free H + in the soil solution, ammonification of organic nitrogen or NO − 3 uptake by microorganisms (Hinsinger et al, 2003). Soil acidification poses a potential impediment to biodegradation as PHCs are optimally degraded within a near-neutral pH (Dibble and Bartha, 1979).…”
Section: Citrate and Malonate Enhanced Microbial Activity In Uncontammentioning
confidence: 99%
“…This seems to be the principal explanation for the lower As levels on plants cultivated in control soil (pH: mean 7.3; organic matter: 6.8%) than in experimental soil (pH: mean 7.8; organic matter 2.7%) values presented in Table 2. The main mechanisms responsible for the pH in the rhizosphere have been classified by Hinsinger et al [31]. Among these one of the most important is the release of large amounts of citrate by lupine roots [22] [32].…”
Section: Total As Concentration In Soil Seeds Leaves and Roots Of Lmentioning
confidence: 99%
“…The pK for citrate 2− /citrate 3− is 6.40 which is feasible for reacting with free H + in the soil solution at relative low pH. Hence in acidified soils (pH ≤ 5.5) the presence of citrate could contribute to an increase in the rhizosphere pH [31]. The decrease in the concentrations of soluble elements in the presence of plants could be due to either plant uptake or plant interaction with the soil components or both, being the pH the most important factor [19] [21].…”
Section: Total As Concentration In Soil Seeds Leaves and Roots Of Lmentioning
confidence: 99%