Biochemistry & Molecular Biology Journal Open Access

Keywords

Phosphate solubilization; Rhizosphere soil; Enrichment culture; Insoluble phosphate sources

Introduction

Phosphorus (P) is a one of the major plant growth-limiting nutrients although it is abundant in soils in both inorganic and organic forms. The nitrogen (N) fixing legume plants usually require more P than the plants depending upon mineral N fertilizer. Nodule establishment and functioning are important sinks for P and nodules have usually the highest P content in the plant. Therefore, P deficiency condition results in reduced biological nitrogen fixation (BNF) potential and P fertilization will usually result in enhanced nodule number and mass as well as greater BNF potential. Soil P transformation are primarily mediated by microbial activity, which in turn, is influenced by a combination of factors including plant species, soil type and environmental conditions. Soil microorganisms play a significant role in mobilizing P for plants by bringing about changes in pH in rhizosphere soil and also by producing chelating substances, which lead to solubilization of phosphates [1]. These microbes are known as phosphate solubilizers consisting predominately of fungal, bacterial and Actinomycetes species collectively called the phosphate solubilizing microorganisms (PSM) [2]. Soil microorganisms, specifically bacteria and fungi, growing in the root region of plants play an important role in the supply of P in rhizosphere region. There is a preferential stimulation of gram negative, non-sporulating rod shaped bacteria. Arthrobacter, Azotobacter, Azospirillum, Agrobacterium, Cellulomonas, Flavobacterium, Mycobacterium and Micrococcus are mostly present in the rhizosphere region. Microbial inoculants are produced on the basis of selection of beneficial soil microorganisms which have the highest efficiency to enhance plant growth by providing nutrients in a readily absorbable form. Application of microbial inoculants provided an abundant population of active and effective microorganisms to the root activity zone which increases plant ability to uptake more nutrients [3]. The objective of the present study is to isolate phosphate-solubilizing microorganisms from the soil samples of leguminous plants to screen and identify them for phosphate solubilizing efficacy.

Materials and Methods

Isolation of phosphate solubilizing microorganisms

Bacteria, fungi and phosphate solubilizing microorganisms were isolated from three different sites i.e., rhizoplane, rhizosphere and non-rhizosphere [4] of leguminous plants from in and around Gandhigram Rural Institute, Gandhigram, Dindigul. Serial dilutions of the root homogenate of rhizoplane, soil samples of rhizosphere and non-rhizosphere were individually plated on Nutrient Agar (NA), Rose Bengal Agar (RBA) and Pikovskaya Agar Medium (PVK) as described by Gaur [5]. Total bacterial, fungal and phosphate solubilizing microorganisms were enumerated and the RS ratio [6] between the rhizosphere and non-rhizosphere soil samples was calculated by using the formula

Enrichment culture technique

For isolation of insoluble phosphate solubilizing microorganisms, the rhizosphere and non-rhizosphere soil samples were enriched by the method adopted by Tardieux-roche and Barjac [7] and Bardiya and Gaur [8]. The colonies exhibiting zones of phosphate solubiliation were transferred to agar slants on the PVK medium containing 0.5 percent CaCO2 and allowed to grow at room temperature for 3 days. Total bacterial, fungal and phosphate solubilizing microorganisms were enumerated.

Screening of phosphate solubilizing microorganism in solid medium

The ability of the isolated microorganisms to solubilize insoluble phosphate was calculated by solubilization efficiency (E) [9]. Those strains showed solubilization zone were presumed to be phosphate solubilizers and they were further tested for solubilization of phosphates quantitatively.

Screening of phosphate solubilizing microorganism in liquid medium

100 ml aliquots of PVK broth was transferred into 250 ml conical flasks and sterilized by autoclaving before the addition of phosphate source. After 15 days of incubation period the filtrate was used to measure the pH and soluble P. The soluble P present in the supernatant was estimated using the Jasco Spectrophotometer V-530 by chlorostannous reduced molybdophosphoric acid blue method [10]. The pH of the supernatant was measured using an Elico L1 120 pH meter. The organic acids produced by selected PS bacterial cultures were detected by thin layer paper chromatography [5].

Results and Discussion

The isolation of microbes like bacteria, fungi and PSM from rhizoplane, rhizosphere and non-rhizosphere soil samples of various leguminous plants are given in Table 1. The total number of bacterial and fungal colonies varied in the three different regions; PSM were detected in all the regions, but their number gradually decreased from rhizosphere, rhizoplane and nonrhizosphere soil. When compared to fungal population, bacterial population was greater in number. Tephrosia purpurea recorded the highest total bacterial population of 50.51 × 10⁶ cfu/g in the rhizosphere region. The lowest total bacterial population of 2.11 × 10⁶ cfu/g was noticed in the non-rhizosphere region of Lablab purpureus. The capacity of bacterial isolates to solubilize phosphate depends upon the zone of their origin. The large number of phosphate solubilizing bacteria (PSB) observed in the rhizosphere region might be due to the favorable influence of root exudates, containing amino acids, organic acids, sugars, growth promoting substances [11], land use, physico chemical properties, organic matter, available Phosphorus and organic carbon content [12]. Soils poor in organic matter are known to be low in microbial activities except in the rhizosphere of growing plants [4]. Similar findings on occurrence of higher numbers of PSM in the rhizosphere region have been recorded by Swaby and Sperber [13] in legumes, Tomashevska and Manzon [14] and Majumdar [15] in sugarcane rhizosphere, Mehta and Bhide [16], Johri et al. [4], Wahid and Wahid and Mehana [17] and Hwangbo et al. [18] in grass rhizosphere and Rao and Charyalu [19] in foxtail millet. The R:S ratio is the comparison microbial population of rhizosphere and non-rhizosphere regions of a plant and to find out the degree or extent of plant roots exudates effect on soil microorganisms. The R:S ratio of bacterial population was higher in Cicer arietinum. The R/S ratio of microbes was calculated by dividing the microbial population in the rhizosphere area by microbial population in the non-rhizosphere area.

Table 1: Isolation of phosphate solubilizing microorganisms from rhizoplane, rhizosphere and non-rhizosphere soil of various leguminous plants in and around Gandhigram. Mean value of two replicates *RS Ratio between Rhizosphere and non-rhizosphere soil samples.

Enrichment in PVK liquid medium

Rhizosphere and non-rhizosphere soil samples of Clitoria ternatea and Vigna unguiculata were enriched with different phosphate sources in PVK liquid medium and their effects were given in Table 2. Highest phosphate solubilizing bacterial population was recorded in the rhizosphere soil of Clitoria ternatea (23 × 10³ cfu/g) in PVK medium containing tricalcium phosphate (TCP). Lowest population growth was observed in PVK medium containing FePO₄ (9.60 × 10³ cfu/g) in the rhizosphere soil of V. unguiculata. Highest phosphate solubilizing fungal population was observed in rhizosphere soil of V. unguiculata (25.33 × 10³ cfu/g) containing FePO₄. AlPO₄ inhibited the growth of phosphate solubilizing fungal colonies (Plate 1). This enrichment culture technique enhances the growth of phosphate solubilizing microorganisms.

Mean value of three replicates

Table 2: Enumeration of phosphate solubilizing microorganisms from rhizosphere and non-rhizosphere soil by enrichment culture technique. Mean value of three replicates.

Screening in solid medium

Phosphate solubilizing bacterial (11 Nos) and fungal (14 Nos) strains isolated from different soil samples having the ability to solubilize TCP in solid PVK medium are presented in Table 3.

Table 3: Screening of microorganisms for tricalcium phosphate solubilization and evaluation of their solubilization efficiency (E) by plate assay method.

Bacillus sp. 1 to 4 were able to solubilize TCP and produce solubilization zone range from 0.8 cm to 1.0 cm but isolates belonging to Fusarium sp., Mucor sp., Penicillium sp. (2), Aspergillus ochraceus, A. sydawi, A. terreus, A. versicolor and Trichoderma viride were able to produce only 0.2 cm to 0.4 cm of solubilization zone. Solubilization efficiency (E) varied from 13.04 percent to 85.71 percent on 7 days of incubation period only. The colony diameter found to vary from 0.7 cm to 2.9 cm. The growth of the fungal colonies, as in diameter was found to be more when compared to bacterial colonies. Solubilization of insoluble phosphate depends on the type of acids secreted by the organism into the medium. The inhibition zone size varied (cm) in the plate assay may be due to the diffusion rate of different organic acid secreted by the organisms [4].

Screening in liquid medium

After 15 days of incubation, isolates showed good zone of solubilization on solid PVK medium. Phosphate solubilization efficiency of the isolates was confirmed by quantitative analysis of available phosphorus in the PVK liquid medium (Table 4). All the isolated microorganisms solubilized TCP though they varied in their ability and the growth period for highest phosphate solubilization (PS) activity. Among the 25 isolates, 13 isolates viz., 7 Bacillus spp., 4 Aspergillus spp., 1 Pseudomonas sp. and 1 Penicillium sp. showed highest PS activity. The phosphate solubilization ability of the isolated microorganisms varied from 11.85 mg to 61.96 mg P₂O₅. The Proteus sp. showed comparatively lesser PS activity. During 15 days of incubation, the medium changed acidic and the pH of the organisms varied from the initial value of 6.7 to 3.2. Production of organic acid by the isolated organisms in the liquid medium coupled with the decrease of the pH value of the medium. The results obtained showed that the solubilization of insoluble phosphates depends on a decrease in pH and acid production, confirming the observations of Kucey et al. [20]. A correlation between final pH and soluble P level have been reported by Arora and Gaur [21], Venkateswarlu et al. [22], Thomas [23], Narsian et al. [24] and Dave and Patel [25].

Table 4: Screening of microorganisms for TCP solubilization in a broth assay after 15 days.

Organic acid secretion during phosphate solubilisation

Production of organic acid by the selected bacterial sp. in the PVK liquid medium after 10-15 days of incubation was coupled with the decrease of the pH value of the medium. The type of the microorganism and concentration of organic acid produced by them varied with respect to TCP.

Acid production during phosphate solubilization appears to be an event of common occurrence. Citric acid, fumaric acid, gluconic acid, glutaric acid, glyoxalic acid, ketobutyric acid, ketoglutaric acid, malic acid, malonic acid, succinic acid and tartaric acid are commonly produced by the selected phosphate solubilizing bacteria (Table 5).

Table 5: Identification of organic acids produced by the phosphate solubilizers in PVK medium containing TCP after 15 days of incubation.

Solubilization of insoluble phosphate by microorganisms is mainly by production of organic acids and chelating substances [1,26-31]. The synthesis of organic acids by PSB has been well documented [13,32-35]. The synergistic effect of the microorganisms would permit a better response because of greater diversity of the acids secreted. The concentration of organic acids secreted by the microorganisms varied with the phosphate source employed [36].

Conclusion

The soil is one of the most dynamic sites of biological interaction in nature and it is the site in which the nutrition of agricultural crops occurs. Rhizosphere is the region that surrounds plant roots, where materials released from the roots and the metabolic activities of the root change the characteristics of the soil. Phosphate solubilizing microorganisms (PSMs) were isolated from rhizoplane, rhizosphere and non-rhizosphere of different leguminous plants. Seed or soil inoculated phosphate solubilizing bacteria (PSB) is known to improve solubilization of fixed and applied phosphates in soil and it increase the crop yield. The PSM are effective as biofertilizers in enhancing crop yields in phosphate deficient soils. The supply of phosphate to the plants by this environmentally friendly way is a sustainable manner.

References

1. Halder AK, Mishra AK, Chakrabarty PK(1991) Solubilization of inorganic phosphates by Bradyrhizobium. Indian J ExpBiol29: 28-31.
2. Nautiyal CS, Bhadauria S, Kumar P, Lal H,Mondal R, et al. (2000) Stress induced phosphate solubilization in bacteria isolated from alkaline soils. FEMS MicrobiolLett82: 291-296.
3. Mehrvarz S, Chaichi MR (2008) Effect of Phosphate Solubilizing Microorganisms and Phosphorus Chemical Fertilizer on Forage and Grain Quality of Barely (Hordeumvulgare L.). American-Eurasian J Agric & Environ Sci 3: 855-860.
4. Johri JK, Surange S, Nautiyal CS (1999) Occurrence of salt, pH, and temperature-tolerant, phosphate-solubilizing bacteria in alkaline soils.  CurrMicrobiol39: 89-93.
5. Gaur AC (1990) Phosphate solubilizing microorganisms as biofertilizers. Omega scientific Publishers, New Delhi.
6. Oyeyiola GP(2010)Rhizosphere bacterial flora of Amaranthushybridus. Research Journal of Microbiology 5: 137-143.
7. Tardieux-roche A, Barjac HD(1959)Solubilization of natural phosphates by soil microorganisms. Ann Inst Pasteur96: 781-789.
8. Bardiya MC, Gaur AC(1974) Isolation and screening of microorganisms dissolving low-grade rock phosphate. Folia Microbiol19: 386-389.
9. Seshadri S,Muthukumarasamy R, Lakshminarasimhan C, Ignacimuthu S (2000) Solubilization of inorganic phosphates byAzospirillumhalopraeferans.CurrSci79: 565-567.
10. Jackson ML(1973)Soil Chemical Analysis. Prentice Hall of India Pvt. Ltd., New Delhi.
11. Kumar V, Narula N(1999)Solubilization of inorganic phosphates and growth emergence of wheat as affected by Azotobacterchroococcummutants. BiolFertil Soils 28: 301-305.
12. Pal SS(1999) Selection of acid tolerant strains of phosphate–solubilizing bacteria in soils of Uttar Pradesh Himalaya.  Indian J AgriSci69: 578-582.
13. Swaby RJ, Sperber JI(1958) Phosphate dissolving microorganisms in the rhizosphere of legumes in Nutrition of Legumes. Academic Press, New York.
14. Tomashevska OG, Manzon VD (1961) The effect of microorganisms on the solubility of phosphate fertilizer and the P uptake by the plants. Trudy InstMicrobiolAkadNauk11: 260-268.
15. Majumdar SB(1968) Studies on fungi in rhizophore of sugarcane with special reference to their biochemical activities and the influence of root exudates. PhD thesis, Poona University, Poona.
16. Mehta YR, Bhide VP(1970) Solubilization of tricalcium phosphate by some soil fungi. Indian J ExpBiol 8: 228-229.
17. Wahid OA, Mehana TA(2000) Impact of phosphate solubilizing fungi on the yield and phosphorus uptake by wheat and faba bean plants. Microbiol Res155: 221-227.
18. Hwangbo H, Park RD, Kim YM, Rim YS, Park KH, et al.(2003) 2-ketogluconic acid production and phosphate solubilization by Enterobacterintermedium. CurrMicrobiol 47: 87-92.
19. Rao KVB, Charyulu PBBN (2003) Population dynamics and nitrogen fixation by diazotropic bacteria in the rhizosphere of foxtail millet.  Indian J Microbiol43: 223-236.
20. Kucey RMN, Janzen HH, Leggett ME(1989)Microbially mediated increases in plant available PAdvAgron42: 199-221.
21. Arora D, Gaur AC (1978) Periodic microbial solubilization of 32P labelled hydroxyapatite. Indian J Microbiol18: 193-195.
22. Venkateswarlu B, Rao AV, Raina P (1984) Valuation of P solubilization by microorganisms isolated from aridsoils. J Indian Soc Soil Sci32: 273-277.
23. Thomas GV(1985) Occurrence and ability of phosphate solubilizing fungi from coconut plantation soils. Pl Soil87: 357-364.
24. Narsian V, ThakkarJ, Patel HH (1994) Isolation and screening of phosphate solubilizing fungi. Indian JMicrobiol34: 113-118.
25. Dave A, Patel HH (1999) Inorganic phosphate solubilizing soil Pseudomonas. Indian JMicrobiol39: 161-164.
26. Singh CP, Mishra MM, Yadav KS (1980)Solubilization of insoluble phosphates by thermophilic fungi. AnnMicrobiol131: 289-296.
27. Mishra MM, Phoget VK, GoyalS, Yadav KS (1983)Solubilization of phosphorus from Mussoorie rock phosphate by Aspergillusawamoriand humic substances. Trop Plant Sci Res1: 221-224.
28. Halvorson HO, KeyanA, Kornberg HL (1990) Utilization of calcium phosphates for microbial growth at alkaline pH.Soil BiolBiochem22: 887-890.
29. Luo AC, Sun X, Zhang YS (1993) Species of inorganic phosphate solubilizing bacteria in red soil and the mechanism of solubilization. Pedosphere3: 285-288.
30. Asea PEA, KuceyRMN, Stewart JWB (1988)Inorganic phosphate solubilization by two Penicilliumspecies in solution culture and soil. Soil BiolBiochem20: 459-464.
31. Sundaram VM, Kathiresan D, Eswaran S,Sankaralingam S, Balakan B, et al. (2016) Phosphate solubilization and phytohormones production by rhizosphere microorganisms. Advance in Agriculture and Biology5: 5-13.
32. Louw HA, Webley DM(1959) A study of soil bacteria dissolving certain mineral phosphate fertilizers and related compounds. JApplBact22: 227-233.
33. Ahmed N, Jha KK (1968)Solubilization of rock phosphate by microorganisms isolated from Bihar soils. J Gen ApplMicrobiol14: 89-95.
34. Taha SM, Mahmoud SAZ, El-Damaty AA, Abd El-Hafez AM(1969) Activity of phosphate dissolving bacteria in Egypitan Soil.Pl Soil31: 149-160.
35. Bajpai PD, Sundara WVB(1971) Phosphate solubilizing bacteria. II. Extracellular production of organic acids by selected bacteria solubilizing insoluble phosphate. Soil Sci Pl Nut17: 44-45.
36. Gadagi RS, Sa T (2002) New isolation method for microorganisms solubilizing iron and aluminium phosphates using dyes. Soil Sci Pl Nutr48: 615-618.