磷石膏胶结充填体强度特性及微观机理研究

Research on Strength Characteristics and Microscopic Mechanisms of Phosphogypsum Cemented Backfill

  • 摘要: 针对磷石膏作为单一骨料用于矿山充填的应用需求,采用室内力学实验结合XRD、TG−DSC、SEM等微观分析手段,研究了磷石膏胶结充填体在7~90 d龄期内的强度发展规律,深入解析了水化产物演变、微观结构特征及其与宏观力学性能的关联机制。研究结果表明:磷石膏充填体的抗压强度在7~56 d龄期内呈现稳定的线性增长趋势,7 d强度显著偏低,28 d强度仅为56 d强度的40%~50%,呈现“前期缓凝−中后期持续增长”强度发展特征。充填体强度发展受水化产物累积和微观结构演变协同调控:7 d龄期时,石膏及可溶性磷、氟等缓凝组分显著抑制水泥水化,钙矾石(AFt)呈细针状分散分布,C−S−H凝胶生成量少,导致孔隙率较高,早期强度发展缓慢;28 d龄期时,C3S和C2S等水泥矿物持续水化,AFt晶体由细针状发育为针棒状,与C−S−H凝胶交织形成网状骨架,孔隙结构得到改善;56~90 d龄期时,C3S消耗殆尽,C−S−H凝胶致密包裹AFt及二水石膏晶体,同时二水石膏重结晶细化填充孔隙,形成致密结构,抗压强度显著提升。该研究从微观尺度揭示了磷石膏胶结充填体的缓凝机制与结构致密化过程,为磷石膏在矿山充填工程中的规模化应用提供重要技术支撑。

     

    Abstract: To address the engineering requirements of utilizing phosphogypsum as the sole filling aggregate in mine backfilling, the strength development patterns and microscopic mechanisms of phosphogypsum cemented backfill over curing periods of 7−90 d were investigated through laboratory mechanical testing combined with microscopic analysis techniques including X−ray diffraction, thermogravimetric differential scanning calorimetry and scanning electron microscopy. This integrated methodology enabled detailed analysis of hydration product evolution, microstructural characteristics, and their correlation with macro−mechanical properties. Research results indicate that the compressive strength of phosphogypsum backfill increases linearly with curing age during the 7−56 d curing period, exhibiting notably low early−stage strength. The 28 d strength accounts for only 40%~50% of 90 d strength, demonstrating a “slow initial setting followed by continuous growth in the middle and later stages” development pattern. The strength development is governed by hydration product accumulation and microstructural evolution. At the age of 7 d, gypsum and soluble phosphorus, fluorine inhibit cement hydration, resulting in AFt being distributed in fine needles and a small amount of C−S−H gel formation. This results in high porosity and low early strength of phosphogypsum cemented backfill. At the age of 28 d, sustained hydration of cement minerals (C3S, C2S) promotes the growth of AFt crystals from fine needles to needle rods, interweaving with C−S−H gel to form a network skeleton, reducing porosity. At the age of 56−90 d, C3S is nearly depleted, and C−S−H gel densely encapsulates AFt and dihydrate gypsum crystals, while recrystallized dihydrate gypsum refines and fills pores, forming a compact structure that significantly enhances the backfill’s compressive strength. This study reveals the retardation mechanism and structural densification process of phosphogypsum cemented backfill at the microscale, providing crucial technical support for the large−scale application of phosphogypsum in mine backfill engineering.

     

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