JOURNAL OF HAZARDOUS MATERIALS
·
2023
·
IF 13.6
Xiaoting Zhang,Lujian Lin,Hanyi Li,Shanle Liu,Shuai Tang,Bo Yuan,Hualong Hong,Manlin Su,Jingchun Liu,Chongling Yan,Haoliang Lu
Iron (Fe) plaques in coastal wetlands are widely recognized because of their strong adsorption affinity for natural particles, but their interaction behaviors and mechanisms with plastics remain unknown. Through laboratory incubation experiments, paired with multiple characterization methods and microbial analysis, this work focused on the characteristics of Fe plaques on low-density polyethylene plastic surfaces and their relationship with environmental factors in coastal wetlands (Mangrove and Spartina alterniflora soil). The results showed that iron plaques increased the adhesive force of the plastic surface from 65.25 to 300 nN and promoted the oxidation of the plastic surface. Fe plaque formation was stimulated by salinity , anaerobic conditions , natural organic matter, and a weak alkaline scenario (pH 8.0–8.3). The Fe content showed a stable positive correlation with heavy metals loading (i.e., As, Mn, Co, Cr, Pb, and Zn). Furthermore, we revealed that Fe plaque was positively regulated by Nitrospirae through 16S rRNA high-throughput sequencing analysis. Meanwhile, Verrucomicrobia and Kiritimatiellaeota . may act as depressants by consuming salt. This work illustrated that iron plaques could enhance the role of plastics in contaminant migration by altering their adsorption performance, providing new insights into plastic interface behavior and potential ecological effects in coastal wetlands.
研究领域:
环境科学
·
微生物学
✓ 已验证
产品关联
DOI
PubMed
高影响因子
SOIL BIOLOGY & BIOCHEMISTRY
·
2024
·
IF 9.8
Jinzhi Yao,Minghui Xie,Linpeng Yu,Ting Liu,Tim J. Clough,Nicole Wrage-Mönnig,Jiafa Luo,Chunsheng Hu,Tida Ge,Shungui Zhou,Shuping Qin
Iron (Fe) plaque is a concentrated form of microbially available Fe oxide that coats rice plant root surfaces, representing a high density of Fe oxide and which potentially mediates paddy soil CH 4 emissions. Using a combination of methods including Fe plaque induction, isotopic labeling , pure microbial strains, and Fe oxide addition experiments, we investigated the impact of Fe plaque on methane (CH 4 ) emissions from paddy soils and explored the associated mechanisms underlying the influence of Fe plaque on CH 4 emissions. A 13 C–CH 4 isotopic labeling experiment showed that Fe plaque did not significantly affect CH 4 oxidation and associated gene expression, whereas Fe plaque significantly enriched methanogenic archaea and their expression of genes associated with methanogenesis. Pure microbial strain and Fe oxide addition experiments showed that the enhancement of CH 4 production in the presence of Fe plaque was caused by the (semi) conductive minerals within the Fe plaque, specifically, hematite , which promoted the extracellular electron transfer between the methanogenic archaea and their syntrophic bacteria, resulting in enhancement of methanogenesis. Our results imply that the presence of Fe plaque will accelerate CH 4 emissions from paddy soils and suppressing Fe plaque has the potential to mitigate CH 4 emissions.
研究领域:
环境微生物学
·
土壤学
✓ 已验证
DOI
高影响因子
SOIL BIOLOGY & BIOCHEMISTRY
·
2022
·
IF 8.546
Jinzhi Yao,Shuping Qin,Ting Liu,Tim J. Clough,Nicole Wrage-Mönnig,Jiafa Luo,Chunsheng Hu,Tida Ge,Shungui Zhou
Poorly crystalline iron (Fe) oxides are commonly deposited on the surface of rice roots, forming an Fe plaque. This Fe plaque is an important area for Fe redox reactions because the poorly crystalline Fe is available for microbial transformations. However, it remains unclear what the mechanisms are that cause the root Fe plaque to affect CO 2 emissions from paddy soils . Thus, this study investigated the effects of Fe plaque on paddy soil CO 2 emissions and the associated mechanisms. Paddy soil with rice plant roots containing an Fe plaque-coating had 1.5-fold larger CO 2 emissions and higher expression levels of genes involved in soil carbon (C) degradation than Fe plaque-free roots, indicating that Fe plaque stimulated paddy soil derived CO 2 emissions. Fe plaque-coated rice roots, immersed in a 13 C-labeled glucose solution, emitted more CO 2 , with a higher abundance of 13 CO 2 , than the Fe plaque-free roots. These differences were not observed when the surfaces of the rice roots were sterilized. These results indicate that the Fe plaque-stimulated CO 2 emissions were due to soil microbial respiration , not autotrophic root respiration . Chelating the dissolved Fe on the root surface eliminated Fe plaque stimulation of CO 2 emissions, while Fe(III) supplementation correlated with enhanced CO 2 emissions. The stoichiometric mole ratio of the enhanced CO 2 emissions to the Fe(II) generated was comparable to the theoretical ratio of Fe(III) when used as an electron acceptor for organic C decomposition. These results showed that the Fe plaque enhancement of CO 2 emissions was coupled to Fe(III) reduction. Limiting the stimulating effects of Fe plaque on CO 2 emissions may be a potentially useful approach for mitigating organic C loss from paddy soils.
研究领域:
土壤学
·
微生物学
·
环境科学
✓ 已验证
DOI
高影响因子