The NH4+-N adsorption performance regulated by the external surface of water storage clay: Particle size effect and path analysis.
- 2026-06
- Environmental research 300
- PubMed: 41974340
- DOI: 10.1016/j.envres.2026.124495
Study Design
- Methods
- CT scanning to reconstruct 3D structure, quantification of porosity, fractal dimension, mass specific surface area, volume specific surface area, adsorption kinetics experiments, path analysis
- Funding
- Unclear
Water storage clay is a new type of porous material with a stable structure that can be used as a soil conditioner to enhance the soil's ability to store and transport water and fertilizer. However, its effectiveness in adsorbing NH4+-N remains unclear. In order to clarify the adsorption capacity and mechanism of NH4+-N by the three-dimensional pore structure of water storage clay, this study employed CT scanning technology to reconstruct the three-dimensional structure of water storage clay of varying particle sizes. Furthermore, the study quantified porosity, fractal dimension, mass specific surface area, and volume specific surface area. The study also proposed a new parameter termed the area coefficient (AC). A systematic analysis was conducted of the influence of structural characterization parameters of water storage clay on its NH4+-N adsorption behavior, using adsorption kinetics experiments and path analysis. The results showed that the three-dimensional structural characteristic parameters of water storage clay varied significantly with particle size. Small particle size water storage clay has low porosity and fractal dimension, high specific surface area and area coefficient, and dense internal particle structure. Large-sized water storage clay features high porosity and fractal dimension, low specific surface area and area coefficient. Its internal particles are loose and porous, and the pore structure is complex. The adsorption behaviors of water storage clay with different particle sizes for NH4+-N all conform to the pseudo-second-order adsorption kinetic model, and the adsorption capacity significantly decreases with the increase of particle size. Path analysis further reveals that the pseudo-second-order kinetic rate constant (k2) is the main parameter influencing the adsorption capacity. The particle size indirectly regulates the adsorption performance through the volume specific surface area and the mass specific surface area. This study provides a theoretical basis and quantitative support for the application of water storage clay in agricultural nitrogen management.
Research Insights
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