Experimental study on preferential solution flow during dump leaching of low-grade ores

Sheng-hua Yin , Ai-xiang Wu , Yong-ding Su , Jie Zhang

Journal of Central South University ›› 2007, Vol. 14 ›› Issue (4) : 584 -588.

PDF
Journal of Central South University ›› 2007, Vol. 14 ›› Issue (4) : 584 -588. DOI: 10.1007/s11771-007-0112-2
Article

Experimental study on preferential solution flow during dump leaching of low-grade ores

Author information +
History +
PDF

Abstract

The phenomenon of preferential solution flow during dump leaching of low-grade ores was studied. The formative mechanism of preferential solution flow was investigated through analyzing the relationship between permeability and ore diameter, and the relationship between surface tension and ore diameter. The preferential solution flow happened within the fine ore area when the dump was unsaturated. And it could happen within the coarse ore area when the dump became saturated. The results of experiment show that the outflow of coarse ore area increases sharply with higher applied rate. The outflow of fine ore area is greater than that of coarse ore area when the applied rate is below 3.2 L/min, and the preferential solution flow happens in fine ore area. But the preferential solution flow happens in coarse ore area when the applied rate is higher than 3.2 L/min. The result of the experiment is consistent with the mechanism analyzing.

Keywords

low-grade ore / preferential solution flow / permeability / surface tension / applied rate

Cite this article

Download citation ▾
Sheng-hua Yin, Ai-xiang Wu, Yong-ding Su, Jie Zhang. Experimental study on preferential solution flow during dump leaching of low-grade ores. Journal of Central South University, 2007, 14(4): 584-588 DOI:10.1007/s11771-007-0112-2

登录浏览全文

4963

注册一个新账户 忘记密码

References

[1]

ZHANG Guang-ji, FANG Zhao-heng. The contribution of direct and indirect actions in bioleaching of pentlandite[J]. Hydrometallergy, 2005(80): 59–66.

[2]

CRUNDWELL F K. How do bacteria interact with minerals[J]. Hydrometallergy, 2003(71): 75–81.

[3]

ZHOU Hong-ming, ZHENG Shi-li, ZHANG Yi. Leaching of a low-grade niobium-tantalum ore by highly concentrated caustic potash solution[J]. Hydrometallurgy, 2005(80): 83–89.

[4]

AcarSevket, BrierleyJames A., WanRong Yu. Conditions for bioleaching a covellite-bearing ore. Hydrometallurgy, 2005, 77(3-4): 239-246

[5]

NiY.-w., OuZ.-q.. Research advance of soil preferential flow and pollutant priority migrate[J]. Soil and Environment, 2000, 9(1): 60-63

[6]

WuA.-x., YinS.-h., LiuJ.-z., et al.. Formative mechanism of preferential solution flow during dump leaching[J]. Journal of Central South University of Technology, 2006, 13(5): 590-594

[7]

WuA.-x., WangH.-j., JiangH.-c.. Rule of oxygen transmission in dump leaching[J]. Journal of Central South University of Technology, 2006, 13(3): 295-299

[8]

ChenY.-p., ShiM.-h.. Determination of permeability for porous media using fractal theory[J]. Journal of Tsinghua University: Science and Technology, 2000, 40(42): 94-97

[9]

LiuX.-l., LiangB., XueQ.. Fractal description of porous media permeability[J]. Advances in Water Science, 2003, 14(6): 769-773

[10]

LiuJ.-r., QinJ.-s., WuX.-d.. Experimental study on relation between temperature and rocky permeability[J]. Journal of the University of Petroleum: Edition of Natural Science, 2001, 25(4): 51-53

[11]

ZouZ.-Y, YoungM.H, LiZ, WierengaP.J. Estimation of depth averaged unsaturated soil hydraulic properties from infiltration experiments. Journal of Hydrology, 2001, 242(1-2): 26-42

[12]

ŠimůnekJ., van GenuchtenM. T.. Estimating Unsaturated Soil Hydraulic Properties from Tension Disc Infiltrometer Data by Numerical Inversion. Water Resources Research, 1996, 32(9): 2683-2696

AI Summary AI Mindmap
PDF

147

Accesses

0

Citation

Detail

Sections
Recommended

AI思维导图

/