高级检索+

生物炭结构异质特征改变土壤养分吸附能力的作用机制

Mechanisms of biochar structural heterogeneity in altering soil nutrient adsorption capacity

  • 摘要: 生物炭作为一种实现农业减排固碳与秸秆资源化利用的关键绿色技术,在提升耕地质量方面具有巨大潜力。然而,生物炭粒径结构的理化性质差异直接影响其对土壤养分的吸附与释放机制,导致在农业生产指导中存在不确定性。该研究旨在揭示不同粒径生物炭(毫米级MB、微米级UB、纳米级NB)改良土壤保肥性能的差异性机制。通过不同粒径生物炭结构表征与溶质吸附分析试验,系统比较了其对土壤固磷能力、团聚体水稳性及胶体稳定性的影响。结果表明:1)生物炭颗粒粒径从MB降低至NB,脂肪性基团逐渐消失而芳香性基团基本保留,芳香化程度更高。C-C和COOR等烃基和酯基化合物官能团的减少,C-O酚、醇类化合物官能团呈现增加趋势;2)生物炭颗粒的Zeta电位绝对值增加,胶体分散体系稳定性增强。在土壤结构方面,MB呈现疏松多孔结构,能提升土壤团聚体的结构稳定性(降低团聚体分形维数);而UB和NB则呈现纳米碎晶或片层结构,倾向于团聚或吸附于土壤颗粒表面,且随着施用量的增加,反而降低了团聚体的稳定性。3)在磷素吸附固持方面,Freundlich与Temkin模型能较好拟合磷的等温吸附过程。随着生物炭粒径减小,土壤最大吸磷量显著增加(NB达1.05 mg/g),磷吸持指数提高39.5%,且磷释放风险参数在NB处理中降低34%。相关分析表明,团聚体水稳性、分形维数及Zeta电位与固磷指标呈极显著正相关(P<0.01)。综上所述,减小生物炭粒径能通过提升胶体稳定性与优化表面化学性质,协同增强土壤对磷的化学吸附与物理固持。针对粉砂质壤土,当NB施加量为2.0%时,土壤的吸附磷肥的作用最优。以上研究成果为精准指导生物炭应用生产,提升旱作农田土壤保肥能力提供了理论参考依据。

     

    Abstract: Biochar has emerged as a pivotal green technology for agricultural emission reduction, carbon sequestration, and straw resource valorization, demonstrating considerable potential for enhancing arable land quality. However, variations in the physicochemical properties arising from differences in biochar particle size directly influence its mechanisms of soil nutrient adsorption and release, leading to uncertainties in agricultural application. This study investigates the differential mechanisms by which biochar of varying particle sizes (millimeter-scale (MB), micrometer-scale (UB), and nanometer-scale (NB)) enhances soil nutrient retention capacity. Through experiments analyzing biochar structures of different particle sizes and solute adsorption, the effects on soil phosphorus fixation capacity, aggregate water stability, and colloidal stability were systematically compared. Results indicated that the particle size of biochar decreased from MB to NB, and the fatty groups gradually disappeared while the aromatic groups were basically retained, resulting in a higher degree of aromatization. The functional groups of C-C and COOR alkyl and ester compounds decrease, while the functional groups of C-O phenols and alcohol compounds show an increasing trend; (2) The absolute value of Zeta potential of biochar particles increases, and the stability of the colloidal dispersion system is enhanced. In terms of soil structure, MB exhibits a loose and porous structure, which can enhance the structural stability of soil aggregates (reduce the fractal dimension of aggregates); However, UB and NB exhibit nano crystalline or layered structures, tending to aggregate or adsorb on the surface of soil particles, and with increasing application, the stability of aggregates is actually reduced. (3) In terms of phosphorus adsorption and fixation, the Freundlich and Temkin models can well fit the isothermal adsorption process of phosphorus. As the particle size of biochar decreases, the maximum phosphorus uptake (qmax) of soil significantly increases (NB reaches 1.05 mg/g), the phosphorus adsorption index PSI increases by 39.5%, and the phosphorus release risk parameter EPCo decreases by 34% in NB treatment. Relevant analysis shows that the water stability, fractal dimension, and Zeta potential of aggregates are significantly positively correlated with phosphorus fixation indicators (P<0.01). In summary, reducing the particle size of biochar can synergistically enhance the chemical adsorption and physical fixation of phosphorus in soil by improving colloid stability and optimizing surface chemical properties. For sandy loam soil, the optimal adsorption of phosphorus fertilizer is achieved when the application rate of NB is 2.0%. The above research results provide a theoretical reference for accurately guiding the application and production of biochar, and improving the nutrient retention capacity of dryland farmland soil.

     

/

返回文章
返回