Microbial mechanisms responsible for the variation of soil Cd availability under different pe+pH environments
Microbial mechanisms responsible for the variation of soil Cd availability under different pe+pH environments
复制标题
不同pH环境下土壤Cd有效性变化的微生物机制
DOI:
10.1016/j.ecoenv.2020.111057
复制
发表时间:
2020
期刊:
影响因子:
--
通讯作者:
Wang Duo
中科院分区:
文献类型:
--
作者:
Wang Meng;Chen Shibao;Chen Li;Wang Duo
The objective of this study was to explore potential microbial mechanisms associated with how water management may alter soil Cd availability under changing pe + pH environments. Four water regimes, aerobic [70% MWHC] + dissolved oxygen, aerobic, continuous flooding, and continuous flooding + N2, were applied to Cd-contaminated soil. The results show that the anoxic treatments were effective in decreasing soil pe + pH and in turn decreased Cd availability and increased soil S and Fe availability relative to those of the aerobic treatments. The decreased pe + pH enriched some anaerobic microorganisms such as those in the familiesAnaerolineaceaeandGeobacteraceae. Conversely, other families, such asGemmatimonadaceaeandSphingomonadaceae, appeared to be sensitive biomarkers that responded to aerobic treatments. Bacterial community structure and network interactions were altered to strengthen bacterial responses to different pe + pH environments as indicated by phylogenetic molecular ecological network (pMEN) analysis. The majority of predicted functional categories, such as metabolism, cell motility, and membrane transport, were affected by different irrigation regimes as indicated by a functional gene profile analysis. The categories were related to important traits that facilitated acclimation of bacteria to their local environment with altered soil pe + pH. Structural equation models revealed that soil pe + pH contributed significantly to soil enzyme activities and differences in bacterial community and function, and consequently, was responsible for the variation of soil Cd availability and iron or sulfur reduction.