Characters of anisotropy seepage in homogenous ore material
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摘要: 以德興銅礦礦石為實驗物料,采用均勻設計法確定散體滲流實驗方案,在自制多功能浸出實驗臺架上進行水平和垂直滲流實驗,實驗結果采用SPSS統計軟件進行回歸分析.結果表明:垂直向下的滲流系數最大,其次為水平方式,垂直向上的滲流系數最小;均質體各向異性系數變化范圍為1.38~6.73,平均值為4;粗粒含量P5在35%~60%之間以及含泥量在1%~5%之間,散體的滲流系數變化呈先升后降現象;滲流系數與孔隙率呈冪函數關系,隨孔隙率增大而上升;孔隙率隨0.1~0.2 mm的物料含量增加而下降,隨10~8 mm和8~4 mm含量之積增大而上升;滲流指數m與雷諾數Re之間存在冪函數關系,對于判定滲流狀態兩者是一致的;西源排土場水平滲流系數為3.68×10-2m·s-1,垂直滲流系數為1.51×10-2m·s-1.Abstract: Horizontal and vertical seepage experiments with granular material from Dexing Copper Mine were completed on a multifunctional experimental shelf. The experiment projects were homogenous designed and the data were analyzed in SPSS software. It is shown that the maximum seepage coefficient appears in clown-going flow, the smaller in horizontal flow and the minimum in up-going flow. All the anisotropy coefficients vary from 1.38 to 6.73 and their average value is 4. While the content of coarse grains is in the range of 35% to 60% and the content of mud is 1% to 5%, the seepage coefficient is initially uprising but latter down-going. The seepage coefficient is correlated with porosity in a power function and uprises with enlarging porosity. The porosity declines with increasing content of grains in the range of 0.1 to 0.2 mm and heightens with increasing content of grains in the ranges of 10 to 8 mm and 8 to 4 ram. The relation of seepage coefficient and Reynolds number could he expressed as a power equation and they are identical to determine seepage state. The horizontal and vertical seepage coefficients of Xiyuan dump are 3.68× 10-2 m·s-1 and 1.51 × 10-2 m·s-1, respectively.
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Key words:
- homogenous material /
- seepage /
- anisotropy coefficient /
- heap leaching /
- porosity
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