1995
DOI: 10.1111/j.1469-8137.1995.tb03062.x
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Root‐induced iron oxidation, pH changes and zinc solubilization in the rhizosphere of lowland rice

Abstract: S Ll M M . A R YRice plants {Oryza sativa L., cv, [R34) were grown with their roots sandwiched between cylinders of an anaerobic low-Zn Molhsol. After periods of root-soil contact of up to 12 d (total plant age c. 28 d) the profiles of different Zn fractions, reduced and oxidized Fe, and pH in the soil near the root 'plane' were determined. The concentration of easily plant-extractable Zn in the soil (measured by extraction in 1 M KCl) was negligible, and so it was necessary for the plants to induce changes i… Show more

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Cited by 156 publications
(116 citation statements)
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“…If this is also true for rice, then rhizosphere effects could play a major role in Zn uptake. These rhizosphere effects may involve acidification of the rhizosphere (Kirk and Bajita, 1995) and exudation of Zn chelators (Tolay et al, 2001). Alternatively, or in addition, mycorrhizas could play a role (Purakayastha and Chhonkar, 2001).…”
Section: Discussionmentioning
confidence: 99%
“…If this is also true for rice, then rhizosphere effects could play a major role in Zn uptake. These rhizosphere effects may involve acidification of the rhizosphere (Kirk and Bajita, 1995) and exudation of Zn chelators (Tolay et al, 2001). Alternatively, or in addition, mycorrhizas could play a role (Purakayastha and Chhonkar, 2001).…”
Section: Discussionmentioning
confidence: 99%
“…In a nutrient solution, the resultant pH change will be dispersed throughout the solution; but in a soil or sediment this change will be propagated away from the roots more slowly and the pH at the root surface can often be 1-2 units lower than that in the soil bulk following chemical reduction. This will greatly alter the mobility of nutrients and toxins, as shown for Zn (Kirk & Bajita, 1995), cations in general (Kirk & Solivas, 1994) and P (Saleque & Kirk, 1995). A fall in pH will tend to increase the concentrations of Cu and Ni in solution in most soils and sediments.…”
Section: Discussionmentioning
confidence: 99%
“…It is established that rice roots can release O # at rates sufficient to support nonspecific aerobic microbial processes (Armstrong et al, 1990 ;Bedford et al, 1991 ;Begg et al, 1994 ;Kirk & Du, 1997) and to oxidize substantial quantities of iron and sulphate at the rhizosphere (Kirk & Bajita, 1995 ;Wind & Conrad, 1995, 1997Arth et al, 1998). The oxidation of NH % + to NO $ − appears equally possible (Reddy & Patrick, 1986 ;Mosier et al, 1990 ;Buresh et al, 1991 ;Arth et al, 1998) and must be tested.…”
Section: mentioning
confidence: 99%