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分級細尾砂膠結充填體早期水化放熱及強度演化特性

Early hydration heat release and strength evolution of cemented backfill with graded fine tailings

  • 摘要: 對分級細尾砂膠結充填體的早期水化反應及力學演化特性進行研究,對不同灰砂比充填體料漿進行水化放熱及電阻特性測試,并根據掃描電子顯微鏡對早期水化產物進行微觀形貌特征分析,最后在單軸壓縮力學試驗結果的基礎上,分析早期水化反應進程及產物對充填體強度演化的影響。研究表明,灰砂比越大,水化放熱速率及放熱量越大,生成水化產物越多,體積電阻率越大。同時水化反應速率直接決定了充填體自身強度形成的快慢,生成的Ca(OH)2減小了料漿體積電阻率,加快充填體自身強度的增長;隨后生成的鈣礬石(Aft)導致顆粒間孔隙更加致密,抑制了離子的溶解,減緩放出熱量速率,從而阻礙了充填體強度的增長;當水化反應進行14 d基本結束后,充填材料凝結固化成為一個整體,強度基本穩定。充填體強度的變化呈現先迅速增加隨后增加趨勢逐漸減小直至穩定的趨勢,為礦山采用分級細尾砂進行井下采空區充填、控制深部采場溫度提供理論支撐及科學指導。

     

    Abstract: In this work, the early hydration reaction and mechanical evolution characteristics of graded fine tailing cemented backfill are studied. The hydration exothermicity and electrical resistance characteristics of backfill slurry with different lime sand ratios are tested, and the microscopic morphology characteristics of early hydration products are analyzed according to scanning electron microscopy (SEM). Finally, on the basis of uniaxial compression mechanical test results, the early hydration reaction process and the effect of the products on the strength evolution of the backfill are analyzed. The results showed that the exothermic process of slurry hydration underwent rapid reaction stage I, induction stage II, acceleration stage III, deceleration stage IV, and stabilization stage V. The volume resistivity underwent increasing stage I, decreasing stage II, and accelerated increasing stages III. The slurry lime sand ratio affects the hydration heat release and volume resistivity. The larger ratio is, the greater the hydration heat release rate and heat release, the more hydration products are generated, and the greater the volume resistivity. An increase in the lime sand ratio prolongs the induction time of the hydration reaction and increases the rate of the hydration reaction during the induction period. At the same time, it retards the growth of volume resistivity. The larger the lime sand ratio is, the stronger the retarding effect and the larger the retarding effect on the growth of slurry volume resistivity. The rate of the hydration reaction directly determines the formation speed of the backfill strength. When the main components of the filling material, C3S and C3A, are dissolved rapidly in water, much heat is released. The generated Ca(OH)2 reduces the volume resistivity of the slurry and accelerates the growth of the backfill strength; the AFt generated subsequently compacts the pores between particles, blocks the dissolution of ions, decreases the rate of heat release, and prevents the growth of backfill strength. The backfill strength increases rapidly from 0–3 d and slowly from 3–7 d. When the hydration reaction is basically completed after 14 d, the filling material is solidified overall, and its strength is basically stable. The change in backfill strength first increases and then gradually decreases until stabilizing. These research conclusions provide theoretical support and scientific guidance for mining to adopt graded fine tailings to fill the underground goaf and control the temperature of the deep stope.

     

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