碱与硫酸盐环境下赤泥基充填材料的强度演化及硅铝活化机制

Strength evolution and silico-aluminous activation mechanism of red mud-based backfill materials in alkali-sulfate environments

  • 摘要: 赤泥是有色金属工业中排放量最大的固废,其碱性强、粒度细、组成复杂且综合利用程度低,制备赤泥基采空区充填材料是实现其资源化低碳利用与绿色处置的一种高效技术路径。以拜耳法赤泥、粉煤灰与脱硫石膏为原料制备赤泥基复合胶凝充填材料,对不同配合比的充填体进行力学性能测试,并采用X射线衍射仪(XRD)与扫描电子显微镜(SEM)微观测试技术,分析材料之间的复合协同效应,揭示充填体的水化产物与微结构演变机制。粉煤灰中活性硅铝组分的溶出动力学行为是决定赤泥基充填材料力学性能的关键因素,通过溶出试验,利用电感耦合等离子体发射光谱仪(ICP-OES)与SEM测试技术,探究粉煤灰中活性SiO2与Al2O3组分在NaOH溶液及NaOH与Na2SO4复合溶液体系的溶出动力学行为,引入经典溶出速率模型,探究活性硅铝组分的溶出动力学行为。结果表明:随着脱硫石膏掺量的增加,充填体强度呈先增加后降低的趋势,m(赤泥)∶m(粉煤灰)∶m(脱硫石膏)为4∶6∶0.9时的抗压强度最佳,3、7和28 d时,抗压强度分别为0.53、1.29、1.91 MPa,在碱与硫酸盐的协同活化作用下,形成了方沸石、斜钙沸石、钙矾石与硅铝酸盐凝胶等主要水化产物,密实了材料间的孔隙结构;粉煤灰中活性SiO2、Al2O3组分在碱溶液体系中溶出特性呈阶段性差异,早期以Si为主,后期以Al为主,硫酸盐通过调控离子平衡和反应路径,强化了溶出差异效应;在NaOH与Na2SO4复合溶液中,1D-diffusion模型适用于活性SiO2的溶解反应,Jander和1D-diffusion模型更适用于活性Al2O3的溶解反应,并阐明了粉煤灰中活性硅铝在碱与硫酸盐协同活化作用下的溶出机理。研究成果为铝土矿绿色开采提供了一种新型充填材料的制备路径。

     

    Abstract: Red mud, the largest solid waste discharged from the non-ferrous metal industry, is characterized by high alkalinity, fine particle size, complex composition, and low comprehensive utilization rate. The preparation of red mud-based backfill materials for goaf represents an efficient technological pathway for its resource utilization, low-carbon application, and green disposal. This study used solid wastes such as Bayer red mud, fly ash, and desulfurization gypsum as raw materials to prepare red mud-based composite cementitious system backfill materials. Mechanical property tests were conducted on backfill specimens with different mix ratios. X-ray diffraction (XRD) and scanning electron microscopy (SEM) were employed to analyze the composite synergistic effects between materials and reveal the hydration products and microstructural evolution mechanisms of the backfill. The dissolution kinetics behavior of active silicon-aluminum components in fly ash are crucial factors determining the performance of red mud-based backfill materials. Through dissolution tests, using the Inductively Coupled Plasma Optical Emission Spectrometer (ICP-OES) and SEM testing techniques, the dissolution kinetic behaviors of the active SiO2 and Al2O3 components in fly ash were studied in an alkaline (NaOH) solution system and an alkaline-sulfate (NaOH-Na2SO4) composite solution system. By referencing classical dissolution kinetic reaction rate models, the kinetic processes of active silicon-aluminum component dissolution were analyzed. The results show that: with the increase of the dosage of desulfurized gypsum, the strength of the backfilling body exhibits a trend of increasing first and then decreasing. When mass ratio of red mud, fly ash and desulfurized gypsum is 4:6:0.9, the compressive strength reaches the optimum. The values of the compressive strength at 3, 7 and 28 days are 0.53, 1.29 and 1.91 MPa respectively. Under the synergistic activation of alkali and sulfate, the backfilling bodies generated main hydration products including analcime, xonotlite, ettringite, and aluminosilicate gel at 28 days of curing, filling the pore structures between materials. The dissolution kinetics behavior of reactive SiO2 and Al2O3 in fly ash exhibits stage-dependent differences in the alkaline solution system, with Si dissolution predominating in the early stage and Al dissolution becoming dominant in the later stage. In the NaOH-Na2SO4 composite solution, the 1D-diffusion model is applicable to the dissolution of reactive SiO2, while both the Jander model and 1D-diffusion model better describe the dissolution of reactive Al2O3, thereby elucidating the dissolution mechanism of silico-aluminous species in fly ash under the synergistic activation by alkali and sulfate. The dissolution mechanism of active silicon-aluminum in fly ash under the synergistic activation of alkali and sulfate was elucidated. The research results provide a preparation route for a new type of backfilling material for the green mining of bauxite under coal seams.

     

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