2017
DOI: 10.1016/j.rhisph.2017.10.002
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Buffering capacity affects phosphorous solubilization assays in rhizobacteria

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Cited by 15 publications
(7 citation statements)
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“…To date, phosphate solubilizing microorganisms are distributed in different bacteria, fungi and actinomycete, P solubilization mechanisms are also different. Many PSMs are mainly through secreting various low-molecular-weight organic acids, which can chelate P via hydroxyl or carboxyl groups and convert insoluble P into soluble forms (HPO4 2and H2PO4 -) (Ahmed & Shahab 2011;Lavania & Nautiyal 2013;Li et al 2015;Nobahar et al 2017). The gluconic and 2-ketogluconic acid were most common organic acids.…”
Section: Discussionmentioning
confidence: 99%
“…To date, phosphate solubilizing microorganisms are distributed in different bacteria, fungi and actinomycete, P solubilization mechanisms are also different. Many PSMs are mainly through secreting various low-molecular-weight organic acids, which can chelate P via hydroxyl or carboxyl groups and convert insoluble P into soluble forms (HPO4 2and H2PO4 -) (Ahmed & Shahab 2011;Lavania & Nautiyal 2013;Li et al 2015;Nobahar et al 2017). The gluconic and 2-ketogluconic acid were most common organic acids.…”
Section: Discussionmentioning
confidence: 99%
“…Phytases are widespread in bacteria and have been identified in, for example, Pseudomonas sp. (Irving and Cosgrove, ; Richardson and Hadobas, ; Cho et al ; Nobahar et al ), Klebsiella sp. (Greiner et al ), Enterobacter sp.…”
Section: Introductionmentioning
confidence: 99%
“…The capability of phosphate‐solubilizing bacteria to convert insoluble phosphate to the absorbable form, orthophosphate, is a property of utmost importance for plant growth‐promoting rhizobacteria (Nobahar et al ). Phytate ( myo ‐inositol(1,2,3,4,5,6)hexaphosphate) is considered the most widespread source of phosphate in soils (Rodriguez and Fraga ), and phytases ( myo ‐inositol (1,2,3,4,5,6)hexaphosphate dephosphorylases, E.C.…”
Section: Introductionmentioning
confidence: 99%
“…Furthermore, fertilization is the most common practice to overcome soil P fixation processes and maintain soil solution P at optimal levels to provide the P demand of agricultural crops and produce them sustainably (Menezes-Blackburn et al 2017;Wei et al 2017). Many complex chemical forms of P differ in mobility and bioavailability, and this affects the fate and transport of soil P (Nobahar et al 2017). Various factors such as the proportional distribution of P in different physicochemical forms, adsorption-desorption reactions, and precipitation-dissolution of P-containing minerals play an important role in converting insoluble P to available P. Knowledge about P fractions and P-containing minerals is necessary to understand the behavior of P in soil and its availability for agricultural crops (Adhami et al 2013;Jalali and Jalali 2016;Shen et al 2019).…”
Section: Introductionmentioning
confidence: 99%
“…Phosphate solubilizing bacteria (PSB) can convert insoluble P to soluble P forms in the rhizosphere. Via its microbial biochemical ability, the P-solubilizing activity has been found to produce and release metabolites such as organic acids (e.g., citrate, malate, oxalate, and gluconate), to acidify the microbial cells and their environment, and to produce phosphatases (Marschner et al 2011;Lagos et al 2016;Nobahar et al 2017;Boroumand et al 2019). The main mechanisms to convert insoluble P to available forms by PSB include (1) the release of complexing or chelating compounds, e.g., organic acids (Rodríguez and Fraga 1999;Barea et al 2005;Hayat et al 2010); (2) the reduction of pH (Gyaneshwar et al 2002;Hayat et al 2010); (3) the release of assimilated P (Sharma et al 2013); (4) the liberation of enzymes (Kaur and Reddy 2015); and (5) the effect on the expression of P transporter genes (Murgese et al 2020).…”
Section: Introductionmentioning
confidence: 99%