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Iron-Based Nanomaterials Enhance Rice Growth and Limit Grain Arsenic Accumulation via Iron Plaque Formation and
Mengshan Tang1, Zhiyuan Lv2, Jiayi Wang1
1College of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, P. R. China.
Iron-based nanoparticles (NPs) effectively reduce arsenic (As) in rice by altering root iron plaque properties and promoting stable As forms. Nanoscale zero-valent iron (nZVI) showed the strongest As mitigation, enhancing soil and plant health.
Area of Science:
- Environmental Science
- Soil Science
- Nanotechnology
Background:
- Arsenic (As) contamination in paddy soils poses risks to rice safety and human health.
- Iron-based nanoparticles (NPs) are explored for their potential in mitigating soil contaminant bioavailability.
Purpose of the Study:
- To evaluate the impact of iron-based NPs (nZVI, Fe2O3 NPs, Fe3O4 NPs) and ionic iron fertilizers on rice growth, arsenic accumulation, and rhizosphere properties.
- To investigate the mechanisms by which iron amendments affect arsenic dynamics and speciation in paddy soil.
Main Methods:
- Short-term (40-day) and life-cycle (128-day) pot experiments with rice.
- Analysis of iron plaque formation, structural characteristics, and physicochemical properties.
- Assessment of arsenic concentrations, iron content in rice grains, and rhizosphere soil microbial gene abundance.
Main Results:
- All iron treatments increased rice grain yield and iron content while reducing arsenic concentration in grains.
- Nanoscale zero-valent iron (nZVI) demonstrated the most significant arsenic mitigation effect.
- Iron NPs altered root-associated iron plaque, increasing crystalline iron oxides and enhancing arsenic-iron colocalization, thereby improving arsenic immobilization.
Conclusions:
- Iron-based nanoparticles, particularly nZVI, are a promising strategy for reducing arsenic exposure risks in contaminated paddy soils.
- Fe NPs enhance arsenic immobilization by modifying iron plaque properties and promoting the transformation of labile arsenic into stable forms in the rhizosphere.
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