Identification and characterization of the rhizosphere phosphate-solubilizing bacterium <Emphasis Type="Italic">Pseudomonas frederiksbergensis</Emphasis> JW-SD2 and its plant growth-promoting effects on poplar seedlings

The rhizospheric bacterium JW-SD2 was identified as Pseudomonas frederiksbergensis based on phenotypic features, the Biolog Identification System and 16S rRNA sequence analysis. The phosphate-solubilizing activity, acidification in culture media, growth rate and organic acid secretion of JW-SD2 were investigated during 192 h of cultivation. The phosphate solubilized by JW-SD2 reached 7.75 mM. The decrease of pH and increase of titratable acidity were closely correlated (Pearson’s r?=??0.953 and 0.969, respectively) with the phosphate-solubilizing activity. High concentrations of gluconic, 2-ketogluconic, pyruvic, maleic and malic acids were detected before 96 h of culture, when the strain displayed a high level of phosphate-solubilizing activity, indicating that these organic acids were efficient components in phosphate solubilization. However, acetic acid did not affect phosphate solubilization as shown by a remarkable increase at 144 h of culture when the phosphate-solubilizing activity decreased. The phosphate-solubilizing ability of JW-SD2 was significantly (P?<?0.01) affected by environmental factors. Over a broad ranges of temperature (20?35 °C), pH (4?9), salinity (0?3.0 %), and volume of medium (1/5?3/5 of flask volume), the phosphate solubilized by JW-SD2 remained above 4.00 mM, demonstrating good potential in adapting to a changing environment. The inoculation experiments indicated that JW-SD2 could significantly (P?<?0.05) promote growth of poplar (Populus euramericana cv. NL-895) in both sterilized and non-sterilized soils. The effects of plant growth promotion were greater in non-sterilized than in sterilized soil. During the 150 days of the trial, the effects of plant growth promotion by JW-SD2 first increased then decreased over time, suggesting that, in field applications, the periodic supplementation of the strain into the rhizosphere should be considered.