STRUVITE PRODUCTION BY PSEUDOMONAS SYRINGAE PV PHASEOLICOLA

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October – November 2018, vol. 8, no. 2
pages: 812-814
Article type: Microbiology of Microbiology
DOI: 10.15414/jmbfs.2018.8.2.812-814
Abstract: Struvite is a biogenic mineral of low solubility. For many years, it has been considered as a fertilizer, but due to the additional cost of manufacture, its use has been limited to only high-value crops. Struvite production by some bacterial strains have been previously reported. However, this is the first study that reports struvite production in Pseudomonas syringae pv phaseolicola strain. Crystal formation was observed within four days of incubation on solid media. Microscopy, X-ray diffraction, Scanning electron microscope and Energy dispersive x-ray spectroscopy analysis confirmed the crystal structure as Struvite. Moreover, this study suggests a possible biotechnological use of P. syringae pv phaseolicola for struvite production for agricultural applications.
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STRUVITE PRODUCTION BY PSEUDOMONAS SYRINGAE PV PHASEOLICOLA


AUTHORS

Ashutosh Sharma, Paola Isabel Angulo-Bejarano, Grisel Fierros-Romero, Rosario del Carmen Vallejo Flores, Karen Rubi Gomez-García, Gabriela Ruiz Collin

ABSTRACT

Struvite is a biogenic mineral of low solubility. For many years, it has been considered as a fertilizer, but due to the additional cost of manufacture, its use has been limited to only high-value crops. Struvite production by some bacterial strains have been previously reported. However, this is the first study that reports struvite production in Pseudomonas syringae pv phaseolicola strain. Crystal formation was observed within four days of incubation on solid media. Microscopy, X-ray diffraction, Scanning electron microscope and Energy dispersive x-ray spectroscopy analysis confirmed the crystal structure as Struvite. Moreover, this study suggests a possible biotechnological use of P. syringae pv phaseolicola for struvite production for agricultural applications.


KEYWORDS

Struvite, Pseudomonas syringae pv phaseolicola, Crystallization

INTRODUCTION

Crystal formation by bacteria is a widely studied phenomenon (Robinson, 1889; Han et al., 2015). Reports during the past decades include the formation of struvite in different bacterial genus such as Bacillus, Staphylococcus, and Myxococcus, among others (Beavon and Heatley, 1962; Nelson et al., 1991; Rivadeneyra et al., 1992). Some of these structures are formed even under impaired physiological conditions. For instance, the formation of struvite by Proteus mirabilis in urinary tract infections (Prywer et al., 2012).

Struvite [NH4MgPO46H2O] is a hydrous magnesium-ammonium phosphate, relatively abundant in soils and lakes; it is a biogenic material that presents a solubility of 0.2 g/L in water (Barak et al., 2006). This crystal structure is rare in nature; however, it has been reported in specific environments that involve organic matter decomposition (Sánchez-Roman et al., 2007). Struvite can be found frequently in wastewater treatment lines and under anaerobic conditions in parts of the water treatment process (Ariyanto et al., 2014). The struvite precipitation has lately been regarded as a plausible source for phosphate recovery, with interesting advantages over conventional methods (Kataki et al., 2016). The Pseudomonas genus comprises one of the most important ecological groups in nature, which includes species with diverse characteristics. Within this group, plant pathogens such as P. syringae, has been extensively studied for its role in plant diseases and quorum sensing (De Smet et al., 2017). P. syringae pv phaseolica is a specific strain that is related with the onset of halo blight and the production of the phytotoxin “phaseolotoxin” in Phaseolus vulgaris (Aguilera et al., 2017; De Ita et al., 1998). Also, its particular role in ice nucleation has also been described (Morris et al., 2013). Some bacterial strains within the Pseudomonas genus have been associated with struvite precipitation (Rivadeneyra et al., 1992; Da Silva et al., 2000); however, to the best of our knowledge, the report of P. syringae pv phaseolicola as a struvite producer has not yet been reported. The main objective of the present study was to confirm the crystal formation capacity of P. syringae pv phaseolicola.

MATERIAL AND METHODS

Bacterial culture development

A bacterial strain of Pseudomonas syringae pv phaseolicola (NPS3121-120905) kindly provided by Dr. Ariel Alvarez-Morales (CINVESTAV, Campus Guanajuato) was cultivated in BD-King solid media (Sigma-Aldrich, Darmstadt, Germany) according to Lelliott and Stead, (1987) and placed in an incubator (IKA KS4000i, Staufen, Germany) at 28 °C and monitored every 4 h until crystal formation was noticed. Bacterial culture growth was obtained by solid BD-King medium, and crystal formation was analyzed every 4 h under a bright field microscope (Olympus, CX31 Tokyo, Japan).

Solubility test

Solubility test was conducted using distilled water, HCl and glacial acetic acid. In addition, the effect of temperature (30, 60, 70, 80 °C) in the crystal solubility was evaluated. Finally, the crystals were properly washed in hot distilled water (70 °C) to allow dissolution of the medium, and placed on a filter paper in a laminar flow cabinet for further analysis.

X-ray diffraction (XRD) analysis

The crystals structure produced by P. syringae pv phaseolicola were ground to powder in an agate mortar and analyzed by X-ray diffraction (XRD) methods. Targeted particles were selected and submitted to X-ray analysis to determine their mineralogical composition, which was assessed using a Rigaku MiniFlex X-ray diffractometer equipment with a scintillator detector. Data were collected for a 0.4 s integration time in 0.02° 2 steps at 40 kV and 40 mA in a 2 interval between 5–80°.

Scanning Electron Microscopy (SEM) Analysis

Scanning Electron Microscopy (SEM) images were obtained using a Scanning Electro Microscope (JEOL JMS-6060 LV with an Oxford spectrometer Inca X-Sight and a silicon doped with lithium WAFER detector) and various magnifications were tested: 37 x, 50 x, 100 x, 500 x, 1,000 x, 2,500 x, 5,000 x, 10,000 x, using gold as coating material.

Energy Dispersive X-Ray Spectroscopy (EDS) Analysis

For the Energy Dispersive X-Ray Spectroscopy (EDS) the amplification was 2,000x with no coating material and an acquisition time of 50s. Both EDS and SEM were analyzed in different sample zones to give more accurate results. The combined analysis of SEM-EDS and XRD confirmed the crystal structures as struvite.

RESULTS AND DISCUSSION

Struvite formation depends on the bacterial strain and culture conditions (Rivadeneyra et al., 1992). Thus, we analyzed the effect of BD King culture media in struvite formation in by P. syringae pv phaseolicola. Crystal formation was observed 4 days after inoculation in solid growth media (Fig. 1a, and 1b). Crystal formation was observed in a bright field microscope (Fig. 1). They were a colorless, transparent vitreous luster and hexagonal structure with 3 or more symmetric perpendicular axes.

Figure 1 Effect of culture media on crystal formation in P. syringae pv phaseolicola, a) Bacterial growth before the crystal formation b) bacterial culture with crystal formation.

Figure 2 Microscopic observation of crystal formed by P. syringae pv phaseolicola.

Struvite precipitation can take place due to the adsorption of Mg2+ and PO43- ions, along with NH4+ liberation (Rivadeneyra et al., 1992). In our experiment, phosphate in the BD King solid medium (King et al., 1954) came in the form of K2HPO4, and the magnesium was obtained in the form of MgSO4•7H2O; thus, our bacterial strain could be using the mechanism for struvite precipitation reported by Rivadeneyra et al., (1992). In fact, the chemical requirement for these ions in our study resembles the ones reported in the B-41 medium that is proposed as the most suitable culture for struvite precipitation in few Pseudomonas spp strains (Rivadeneyra et al., 1992). Furthermore, the overall composition of BD King medium and B-41 medium are very similar regarding both KHPO4 and MgSO4 concentrations (0.15 % for BD King Medium and 0.2 % for B-41 medium). Solubility test results revealed no solubility of the crystal structure formed, under any of the conditions evaluated when water was used as a solvent. However, when HCl was used as a solvent, crystals disintegrated completely after 5 min of exposure. While with the use of glacial acetic acid, crystal samples turned into black and dark in color. Crystal formation depends on a set of physicochemical parameters, namely: pH, mixing, temperature, crystal size, supersaturation degree and presence of impurities. In these parameters, supersaturation and pH are considered the most important for struvite crystallization. Crystal precipitation can be controlled by adjusting the pH in culture conditions (Ariyanto et al., 2014).  Different authors have stated that pH controls the ion activity of the ionic forms of phosphorus and ammonium, especially in NH4+ and PO43- (Matynia et al., 2006; Ariyanto et al., 2014). In our study, both pH and temperature were constant during culture conditions; as for the solubility analysis, the crystal structures were dissolved completely in the presence of HCl, and struvite is reported to be soluble at low pH (Matynia et al., 2006).

Crystal structure identification was assessed using SEM and X-ray diffraction analysis. As a result, the crystal structures formed in BD King solid media were identified as struvite according to the reference pattern (Fig. 3). This struvite conformation is also reported by Rivadeneyra et al., (2014) when analyzing crystal production by different bacterial genus in biofilm formation.

Figure 3 X –Ray powder diffraction with an angular range of 5 to 80º (in 2-theta), with a velocity of 2º per minute and a sampling every 0.02 seconds for the crystals formed by Pseudomonas syringae pv phaseicola that indicated Struvite component.

According to the results obtained from the SEM analysis, the main components found in all the samples analyzed were: Carbon (32.2 %), Oxygen (52.4 %), Mg (7.47 %), P (6.9 %) (mean weight values expressed as a percentage). The main structure of the samples analyzed is shown in Figure 4. Different sites of analysis were chosen for the struvite samples which were analyzed at different magnifications (Figure 4 a to d), and the composition of analyzed crystals has been shown in Table 1.

Figure 4 Scanning Electron Microscope (SEM) results set at an acceleration voltage of 20kV with a spot size of 50 a) to d). Different sample sites were chosen for the SEM analysis. In the upper right box, the general composition diagram can be observed.

Pseudomonas syringae pv phaseolicola is related with plant pathology and also with ice formation (ice nucleation) in the water cycle, in fact, some proteins related with this process are already reported (Morris et al., 2013). Even though there are few reports on Pseudomonas genus and struvite production none of them demonstrate clear evidence for P. syringae pv phaseolicola and struvite precipitation; therefore, this constitutes the first report.

Struvite crystals contain 39 % phosphate, 10 % magnesium and 7 % ammonium (Gell et al., 2011). Hence, due to its high phosphate content, several reports highlight the feasibility of using the struvite precipitation process as a way of recapturing phosphate from different sources (Kataki et al., 2016). This is interesting since global demands for phosphate are increasing and phosphate deposits are diminishing worldwide (Kataki et al., 2016). Therefore, finding bacterial strains that are able of phosphate precipitation in the form of struvite crystals like the one we describe here, opens the possibility of biotechnological applications that could help in the recapturing of phosphate in the environment. Furthermore, several reports indicate the relationship between phosphate solubilization and the Pseudomonas genus (Oteino et al., 2015).

However, a clear mechanism for phosphate recovery or a possible re-introduction or fixation of phosphate in soils due to these microorganisms and their struvite production has not been fully elucidated to date. Therefore, we propose that this might also be a promising use for P. syringae pv phaseolicola; however, the exact mechanism by which this occurs remains to be fully investigated.

Table 1 SEM analysis results for struvite crystal structures
  Element App conc. Intensity corrn Weight % Weight sigma % Atomic %
1 C, K, 47.03 0.4987 33.33 1.58 42.75
O, K 96.39 0.6891 49.45 1.22 47.62
Mg, K 18.01 0.7542 8.44 0.25 5.35
P, K, 28.10 1.2454 7.98 0.24 3.97
K, K 2.29 1.0132 0.8 0.05 0.32
Totals 100
2 C, K, 47.30 0.4973 31.03 1.49 40.02
O, K 116.90 0.7331 52.04 1.17 50.39
Mg, K 19.25 0.7455 8.43 0.23 5.37
Al, K 0.71 0.7396 0.31 0.05 0.18
P, K, 28.86 1.2367 7.61 0.21 3.81
K, K 1.81 1.0134 0.58 0.05 0.23
Totals 100
3 C, K 35.52 0.4642 28.14 1.70 36.94
O, K 110.06 0.7628 53.09 1.30 52.30
Mg, K, 18.46 0.7458 9.11 0.27 5.90
Al, K 0.65 0.7328 0.32 0.06 0.19
P, K 28.61 1.2318 8.55 0.25 4.35
K, K 2.17 1.0108 0.79 0.05 0.32
Totals 100
4 C, K 63.86 0.7427 35.95 0.83 44.04
O, K 100.95 0.7395 57.10 0.79 52.51
Mg, K 5.52 0.7049 3.27 0.12 1.98
P, K 8.15 1.2476 2.73 0.10 1.30
Br, L 1.57 0.6941 0.95 0.12 0.17
Totals 100

Table1 Comparative results of Scanning Electron Microscope observations for all the samples taken. Each column shows the concentration, weight and atomic proportion of the components present in struvite crystals

CONCLUSION

Struvite formation has extensively been reported in different microorganisms. Here we report struvite precipitation induced by P. syringae pv phaseolica strain in laboratory conditions. The crystal structure was validated through SEM and XRD analysis, and that confirms that these crystals belong to struvite mineral. Struvite has been considered as an eco-friendly form for Phosphate recovery from different disposal sources in the environment, namely wastewaters. Furthermore, it is now commercially produced. Therefore, we propose that P. syringae pv phaseolicola can be used to produce struvite through biotechnological approaches.

REFERENCES

Aguilera, S., Álvarez-Morales, A., Murillo, J., Hernández-Flores, J. L., Bravo J., De la Torre-Zavala, S. 2017. Temperature-mediated biosynthesis of the phytotoxin phaseolotoxin by Pseudomonas syringae pv. phaseolicola depends on the autoregulated expression of the phtABC genes. PLoS ONE 12(6), e0178441. https://doi.org/10.1371/journal.pone.0178441

Ariyanto, E., Ang, H. M., Sen, T. K. 2014. Impact of various physico-chemical parameters on spontaneous nucleation of struvite (MgNH4PO4. 6H2O) formation in a wastewater treatment plant: kinetic and nucleation mechanism. Desalination Water Treat, 52 (34-36), 620-6631. https://doi.org/10.1080/19443994.2013.821042

Barak, P., Stafford, A. 2006. Struvite: a recovered and recycled phosphorus fertilizer. (Proceedings of the 2006 Wisconsin Fertilizer, Aglime & Pest Management Conference). University of Wisconsin-Extension US Department of Agriculture, Wisconsin. USA. p.17-19

Beavon, J., Heatley N.G. 1963. The occurrence of struvite magnesium ammonium phosphate hexahydrate in microbial cultures. Microbiology 31 (1), 167-169. https://doi.org/10.1099/00221287-31-1-167

Da Silva, S., Bernet, N., Delgenes J. P., Moletta, R. 2000. Effect of culture conditions on the formation of struvite by Myxococcus xanthus. Chemosphere 40 (12), 1289-1296. https://doi.org/10.1016/S0045-6535(99)00224-6

De Ita, M.E., Marsch-Moreno, R. Guzmán, P., Álvarez-Morales, A. 1998. Physical map of the chromosome of the phytopathogenic bacterium Pseudomonas syringae pv phaseolicola. Microbiology 144 (2), 493-501. https://doi.org/10.1099/00221287-144-2-493

De Smet, J., Hendrix, H., Blasdel, B. G., Danis-Wlodarczyk, K., Lavine, R. 2017. Pseudomonas predators: understanding and exploiting phage-host interactions. Nature Reviews Microbiology 15 (9), 517–530. https://doi.org/10.1038/nrmicro.2017.61

Gell, K., Ruijter, F. J., Kuntke, P., Graaff, M., Smit, A. L. 2011. Safety and effectiveness of struvite from black water and urine as a phosphorus fertilizer. Journal of Agricultural Science, 3(3), 67–80. http://dx.doi.org/10.5539/jas.v3n3p67

Han Z., Zhao, Y., Yan, H., Zhao, H., Han, M., Sun, B., Sun, X., Hou, F., Sun, H., Han, L, Sun, Y., Wang, J, Li, H, Wang, Y., Du, H. 2015. Struvite precipitation induced by a novel sulfate- reducing bacterium Acinetobacter calcoaceticus SRB4 isolated from river sediment. Geomicrobiology Journal, 32(10), 868–877. https://doi.org/10.1080/01490451.2015.1016247

Kataki, S., West, H., Clarke, M., Baruah, D. C. 2016. Phosphorus recovery as struvite from farm, municipal and industrial waste: Feedstock suitability, methods and pre-treatments. Waste Management 49, 437-454. https://doi.org/10.1016/j.wasman.2016.01.003

King, E. O., Ward, M. K., Raney, D. E. 1954. Two simple media for the demonstration of pyocyanin and fluorescin. Translational Research 44(2), 301-307

Lelliott, R. A., Stead, D. E. 1987. Methods for the diagnosis of bacterial diseases of plants. Blackwell Scientific Publications. Hoboken, New Jersey USA.

Matynia, A., Koralewska, J., Wierzbowska, B., Piotrowski, K. 2006. The influence of process parameters on struvite continuous crystallization kinetics. Chemical Engineering Communications 193 (2), 160–176. https://doi.org/10.1080/009864490949008

Morris C., Monteil, C., Berge, O. 2013. The life history of Pseudomonas syringae: linking agriculture to earth system processes. Annual Review of Phytopathology. 51, 85–104. https://doi.org/10.1146/annurev-phyto-082712-102402

Nelson, B., Struble J., McCarthy, G. 1991. In vitro production of struvite by Bacillus pumilus. Canadian Journal of Microbiology 37 (12), 978-983. https://doi.org/10.1139/m91-169

Oteino N., Lally R. D., Kiwanuka S., Lloyd A., Ryan D., Germain K. J., Dowling D. N. 2015. Plant growth promotion induced by phosphate solubilizing endophytic Pseudomonas isolates. Frontiers in Microbiology 6, 745. https://doi.org/10.3389/fmicb.2015.00745

Prywer J., A. Torzewska, Plocinski T. 2012. Unique surface and internal structure of struvite crystals formed by Proteus mirabilis. Urological Research 40 (6), 699–707. https://doi.org/10.1007/s00240-012-0501-3

Rivadeneyra M. A., Pérez-García I., Ramos-Cormenzana, A. 1992. Influence of ammonium ion on bacterial struvite production. Geomicrobiology Journal. 10 (2), 125–137. https://doi.org/10.1080/01490459209377912

Rivadeneyra A., González-Martínez, A. González-López J., Martin-Ramos D., Martínez-Toledo M. V. Rivadeneyra M. A. 2014. Precipitation of phosphate minerals by microorganisms isolated from a fixed-biofilm reactor used for the treatment of domestic wastewater. International journal of environmental research and public health 11 (4), 3689-3704. https://doi.org/10.3390/ijerph110403689

Robinson, H. 1889. On the formation of struvite by microorganisms. Proceedings of the  Cambridge Philosophical. Society. 6, 360-362.

Sánchez-Román, M., Rivadeneyra, M. A. Vasconcelos, C., McKenzie, J. A. 2007. Biomineralization of carbonate and phosphate by moderately halophilic bacteria. FEMS Microbiology Ecology 61 (2), 273–284. https://doi.org/10.1111/j.1574-6941.2007.00336.x