[Effects of Soil Microbial Diversity on the Phosphate Fraction in the Rhizosphere of in the Yeyahu Wetland in Beijing, China].
Journal:
Huan jing ke xue= Huanjing kexue
Published Date:
Nov 8, 2017
Abstract
In this research, microorganisms in rhizosphere/non-rhizosphere soils of in the Yeyahu Wetland were studied. A sequential extraction procedure was used to analyze the phosphorus (P) forms in the rhizosphere/non-rhizosphere soil with a variety of plant growth conditions (April, July, October). The soil bacteria community structure and the diversity was measured using the high-throughput of 16S rRNA amplicons. Furthermore, the complete crystallographic analysis (CCA) method was used to analyze the relationship between phosphate solubilizing microorganisms and P transformation in the soil samples. The results showed that the rank order of inorganic P (IP) fractions in the soil was generally as follows:Ca-bound P (Ca-P) > Occluded P (Oc-P) > Fe-bound P (Fe-P) > Exchangeable P (Ex-P) > Al-bound P (Al-P). The IP content was most affected by the growth of . The minimum content of IP appeared in the vigorous growth period and the total IP content in the rhizosphere soil was generally lower than in the non-rhizosphere soil. The rank order of organic P (OP) fractions were highly resistant OP (HR-OP) > moderately resistant OP (MR-OP) > moderately labile OP (ML-OP) > labile OP (L-OP), and all the components of OP first decreased and then increased with the growth of plant. The major phylogenic groups in rhizosphere/non-rhizosphere soil of , included Proteobacteria, Acidobacteria, Chloroflexi, and Actinobacteria among which, Proteobacteria was the majority group in the community composition. Furthermore, the rhizosphere/non-rhizosphere microbial community structure was significantly affected by seasonal changes and existing differences between the rhizosphere and non-rhizosphere soils. In addition, the main functional groups of the modal transformation of P bacteria genera were , , , , , which can make use of most OP and IP, playing an important role in the transformation of P in wetland soils.