98%
921
2 minutes
20
Understanding how plant functional traits respond to mining activities and impact metal(loid)s accumulation in dominant species is crucial for exploring the driving mechanisms behind plant community succession and predicting the ecological restoration potential of these plants. In this study, we investigated four dominant herbaceous species (, , , and ) growing on antimony (Sb) mining sites (MS) with high Sb and arsenic (As) levels, as well as non-mining sites (NMS). The aim was to analyze the variations in functional traits and their contribution to Sb and As concentrations in plants. Our results indicate that mining activities enhanced soil nitrogen (N) limitation and phosphorus (P) enrichment, while significantly reducing the plant height of three species, except for . The four species absorbed more calcium (Ca) to ensure higher tolerance to Sb and As levels, which is related to the activation of Ca signaling pathways and defense mechanisms. Furthermore, plant Sb and As concentrations were dependent on soil metal(loid) levels and plant element stoichiometry. Overall, these findings highlight the regulatory role of plant element traits in metal(loid) concentrations, warranting widespread attention and further study in the future.
Download full-text PDF |
Source |
---|---|
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC11343610 | PMC |
http://dx.doi.org/10.1002/ece3.70212 | DOI Listing |
PLoS One
September 2025
School of Geography and Resources, Guizhou Education University, Guiyang, China.
Antimony (Sb) is extensively utilized in industrial activities, but most of its compounds exhibit human toxicity and are classified as priority-controlled pollutants. Unlike traditional electrochemical methods that remove metallic pollutants via coagulation or precipitation, electrochemical hydride generation technology converts antimony (Sb) in wastewater into stibine gas (SbH3) for efficient removal. Furthermore, the generated SbH₃ can be decomposed thermally to partially recover metallic antimony.
View Article and Find Full Text PDFToxics
August 2025
Fujian Key Laboratory of Toxicant and Drug Toxicology, Medical College, Ningde Normal University, Ningde 352100, China.
Soil co-contamination with antimony (Sb) and arsenic (As) presents significant ecological and human health risks, demanding effective stabilization solutions. This study evaluated iron-manganese-modified hydrochar (FMHC) for synergistic Sb-As stabilization in contaminated smelter soils. Through 60-day natural aging and 30 accelerated aging cycles, we assessed stabilization performance using toxicity leaching tests (acid/water/TCLP), bioavailable fraction analysis, bioaccessibility assessment, and Wenzel sequential extraction.
View Article and Find Full Text PDFEnviron Geochem Health
August 2025
School of Ecology and Applied Meteorology, Nanjing University of Information Science & Technology, Nanjing, 210044, China.
China produces 48.2% of global antimony (Sb) annually, of which approximately 80% was produced in Southwest China in 2023. The distribution of high-Sb geological background areas in China overlaps with that of karst landforms.
View Article and Find Full Text PDFEnviron Geochem Health
August 2025
Hubei Key Laboratory of Petroleum Geochemistry and Environment, Yangtze University, Wuhan, 430100, Hubei, People's Republic of China.
Mine wastewater pollution, primarily caused by heavy metals and sulfates, poses a significant threat to ecosystems and water quality in mining-affected regions. Effective remediation is essential for mitigating these environmental impacts and ensuring sustainable water management. This study explores the potential of bio-modified coal gangue (MCG) as a sustainable solution for remediating mine wastewater.
View Article and Find Full Text PDFEnviron Monit Assess
August 2025
National Centre for Polar & Ocean Research, Ministry of Earth Sciences, Vasco Da Gama, Goa, India.
Antarctic ice cores provide past atmospheric composition beyond the timeframe of the instrumental records. Here, we examine the record of copper (Cu), a trace metal contaminant, from an ice core record spanning the past ~ 200 years (1809-2012 CE) from the coastal Dronning Maud Land (cDML), East Antarctica (71.5° S, 10.
View Article and Find Full Text PDF