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was used as C source, microorganisms produced higher amounts of organic acids
which causes more insoluble P solubilization. The influence of C on the solubili-
zation of insoluble P was determined further by Song et al. ( 2008 ) who used
different sugars such as glucose, sucrose, or maltose in order to assess the P
solubilization activity of Burkholderia cepacia (DA23). Among all sugars, P
solubilization was found to be twofold lesser in a medium containing sucrose
relative to glucose which generally resulted in the most extensive solubilization
of calcium P (Panda et al. ( 2013 ). Mechanistically, the P-solubilizing efficiency of
microorganisms is associated with its ability to secrete organic acids (Maliha
et al. 2004 ; Khan et al. 2009 , 2010 ), the nature and quantity of which, however,
varies between different sugars and microbes (Rodriguez et al. 2004 ; Hu et al. 2006 ;
Perrig et al. 2007 ). For example, glucose, galactose, maltose, and sucrose used as
single C source were metabolized by Bacillus (strain T-34) and produced citric,
malic, acetic, and lactic acids in considerably higher concentrations compared to
those secreted by Azospirillum (WS-1) and Enterobacter T-41 strains (Tahir
et al. 2013 ). Similar results have also been reported by others (Chen et al. 2006 ;
Archana et al. 2012 ) where Azospirillum , Bacillus, and Enterobacter produced
variable amounts of citric, oxalic, gluconic, and 2-keto-gluconic acids. Also, the
concentrations of the preferred energy source plays a pivotal role in enhancing PS
activity of microbes, and generally the PS activity increases with increasing con-
centration of sugars added to the growth medium. Increasing the concentration of
glucose, for instance, from 1 to 3 % resulted in profound increase in RP solubili-
zation by PSM because higher concentration of glucose led to increased production
of acidity, an important factor in P solubilization (Song et al. 2008 ). In other reports,
a further increase in glucose concentrations from 1 to 5 % (w/v) enhanced the P
solubilization considerably, and the most obvious increment has been recorded up
to 3 % glucose which, however, decreases at 5 % glucose level (Son et al. 2006 ;
Stephen and Jisha 2011 ).
3.2.4 Nitrogen Source
Nitrogen (N), like many other nutrients, influences the growth and functionality of
soil-inhabiting PSM. Nitrogen is involved in various metabolisms such as it partici-
pates in synthesis of amino acids, proteins, and nucleotides. Microorganisms take
up N in ammonical, nitrite, nitrate, or amino form, depending upon the enzyme
present in their system and greatly influencing P solubilization activity (Bar-Yosef
et al. 1999 ; Habte and Osorio 2012 ). Recently, an in vitro experiment was carried
out to evaluate the effect of different nitrogen (N) forms (NH 4 + and/or NO 3 ) on the
dissolution of rock phosphates (RP) by the PSF Mortierella sp. (Habte and Osorio
2012 ). It has been reported that in the presence of NH 4 Cl or NH 4 NO 3 , the solution
of pH following Mortierella sp. application significantly decreases from an initial
value of 7.6 to 3.4 and 3.7, respectively, while KNO 3 reduces the pH to 6.7 only.
Due to greater decrease in pH, there was significantly more P solubilized in the
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