Evaluation of A Composite Soil Cover to Control Acid Waste Rock Pile Drainage

1994 ◽  
Vol 1994 (2) ◽  
pp. 113-121 ◽  
Author(s):  
A. V. Bell ◽  
M. D. Riley ◽  
E. K. Yanful
1993 ◽  
Vol 30 (4) ◽  
pp. 588-599 ◽  
Author(s):  
Ernest K. Yanful ◽  
Michael D. Riley ◽  
Mark R. Woyshner ◽  
Jim Duncan

A 130 cm thick composite soil cover was constructed on an experimental waste-rock pile at the Heath Steele mine site near Newcastle, New Brunswick. The cover consisted of a 30 cm thick sand base, a 60 cm thick compacted glacial till, a 30 cm thick granular layer, and a final 10 cm thick gravel layer for erosion protection. The till was compacted on the sand base in three finished lifts each of 20 cm thickness. Results of a preconstruction pad test indicated six passes of a 5-t vibratory compactor were required to attain the design specifications of 95% of the Modified Proctor maximum dry density at a moulding water content of 2–3% wet of the optimum. These compaction specifications also ensure that the till has a degree of water saturation of at least 95%, which is required to reduce oxygen and acid fluxes in the underlying pile. Quality control measures were taken during the construction to ensure the specifications were followed. Monitoring instrumentation was installed during the construction of the cover. Results indicate a reduction in gaseous oxygen concentrations in the pile from 20% before cover to about 3% after cover placement. The decreased oxygen penetration implies reduced oxygen flux and acid production. Volumetric water contents averaged about 32% in the till both immediately following cover installation and 7 months later. The water-content data are corroborated by soil-suction measurements. Temperatures in the pile have decreased following cover installation but appear to be more influenced by climatic variability than by a decrease in heat production and hence sulphide mineral oxidation. Observed discharge from two lysimeters, installed below the cover, indicates infiltration of 2–2.5% of precipitation during a 55-day period when rainfall was heavy. The quality of seepage from the pile has not changed since cover installation. Further monitoring will be required to confirm the reduction in acid production. Key words : waste-rock pile, acid generation, soil cover, suction, oxygen flux, percolation.


2020 ◽  
Vol 114 ◽  
pp. 104531
Author(s):  
Brayden J. McNeill ◽  
Eva Pakostova ◽  
Jeff G. Bain ◽  
W. Douglas Gould ◽  
Richard T. Amos ◽  
...  

2018 ◽  
Vol 17 (1) ◽  
pp. 180119 ◽  
Author(s):  
Bas Vriens ◽  
Mélanie St. Arnault ◽  
Laura Laurenzi ◽  
Leslie Smith ◽  
K. Ulrich Mayer ◽  
...  

2018 ◽  
Vol 150 ◽  
pp. 40-51 ◽  
Author(s):  
Christopher Power ◽  
Panagiotis Tsourlos ◽  
Murugan Ramasamy ◽  
Aristeidis Nivorlis ◽  
Martin Mkandawire

2015 ◽  
Vol 744-746 ◽  
pp. 1101-1108
Author(s):  
Meng Zhou Zhang ◽  
Zeng He Xu ◽  
Li Guo Jiang

As a long-term source of contaminant solutes, the flow of water within a waste rock pile containing reactive sulfide minerals significantly contributes to the solutes transportation. In this paper, a waste rock pile with the internal structures and grain size distribution from a typical waste dump is introduced as the geometric configuration. A numerical model is then applied to simulate unsaturated flow within a waste rock pile constructed with two primary materials. The simulations results show that the water movement within heterogeneous pile mainly depended on the internal structures. The flow of water can be controlled by the fine material layers within the coarse materials. These fine material layers form a capillary barrier which preventing the water infiltrate towards the centre of the pile. They can retain more water than coarse materials and form a ponding effect and/or percolation points within the pile.


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