動載下磁鐵礦石鐵硅比對其動力學特性及能耗規律的影響
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河北鋼鐵集團沙河中關鐵礦有限公司

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河北省博士研究生創新資助項目(CXZZBS2024137)


The Influence of Iron Silicon Ratio on The Dynamic Characteristics and Energy Consumption of Magnetite under Dynamic Loading
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Shahe Zhongguan Iron Mine Co., Ltd.,Hebei Iron and Steel Group

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    摘要:

    為探明磁鐵礦石在沖擊載荷作用下的破碎特性及能量轉換規律,以不同鐵硅比的磁鐵礦石為研究對象,利用霍普金森壓桿對不同鐵硅比的磁鐵礦石進行沖擊破碎試驗,分析磁鐵礦石在不同入射幅值下的破壞變形特性、抗壓強度特性及能量轉換規律,并結合掃描電鏡技術揭示宏微觀破碎機理,結果表明:在沖擊載荷的作用下,不同鐵硅比的磁鐵礦石應力應變曲線并無壓密階段,直接進入線彈性階段,隨著鐵硅比的增大,彈性模量和峰值應力在不斷減小,磁鐵礦石的動態抗壓強度隨鐵硅比的增大而減小。在動載的作用下,三種鐵硅比的磁鐵礦石的耗散能隨鐵硅比及入射能的增大而增大,擬合曲線的斜率隨鐵硅比的增大而增大。隨著入射幅值的增大,礦石碎塊塊徑在不斷減小,當入射幅值相同時,鐵硅比大的礦石碎塊比鐵硅比小的碎塊塊徑小。隨入射幅值的增大,磁鐵礦石內部沿晶裂隙及穿晶裂隙在不斷增多,破碎形貌變得復雜,裂隙寬度及長度隨鐵硅比的增大而增大增寬。研究結果對于礦山破碎不同磁性鐵含量的磁鐵礦石有一定的指導意義,可以為礦山在一定程度上提高能量的利用率。

    Abstract:

    In order to investigate the crushing characteristics and energy conversion law of magnetite under impact load, we take magnetite with different Fe-Si ratios as the research object, and carry out impact crushing test on magnetite with different Fe-Si ratios by using Hopkinson"s compression rod to analyse the destructive deformation characteristics, compressive strength characteristics and energy conversion law of magnetite under different incident amplitudes, and combine with scanning electron microscope technology to reveal the macro-microcosmic crushing mechanism. The results show that under the impact load, the stress-strain curves of magnetite with different Fe-Si ratios do not have a compression-density phase, but directly enter the linear elasticity phase, and the modulus of elasticity and peak stress are decrease with the increase of Fe-Si ratio, and the dynamic compressive strength of magnetite decreases with the increase of Fe-Si ratio. Under the action of dynamic loading, the dissipation energy of magnetite stones with three iron-silicon ratios increases with the increase of iron-silicon ratio and incident energy, and the slopes of the fitted curves increase with the increase of iron-silicon ratio. With the increase of incident amplitude, the block size of the ore fragments is decreasing, and when the incident amplitude is the same, the block size of the ore fragments with large Fe-Si ratio is smaller than that of the fragments with small Fe-Si ratio. With the increase of the incident amplitude, the magnetite ore internal along the crystal cracks and through the crystal cracks are

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  • 收稿日期:2024-05-09
  • 最后修改日期:2024-06-24
  • 錄用日期:2024-06-26
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