Newmont Mining Company
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Waste Disposal Area
Newmont Home Operations Australia & New Zealand Waihi Gold, New Zealand Mining Waste Disposal Area Acid Drainage Control

It is important to manage the placement of PAF material within the embankments to ensure that acid drainage is controlled both during the short term while the tailings storage facilities are being constructed, and in the long term. NAF material must also be managed carefully as sufficient NAF material must be available for the cover, (zones G, H) and for the liner, (zone A).

Details of the short and long term controls on acid drainage follow. The design strategy is to prevent generation of acid leachate as far as possible and as a contingency to provide for containment, collection and monitoring of any leachate that might be generated.

a. Short Term Controls

While the embankments are being constructed, the most important issue is the water quality of the runoff from the embankment structure. The following controls are used to prevent a deterioration in water quality:

b. Long Term Controls

   
 
Above: Construction of the embankments requires the selective use and zoning of waste rock materials and the controlled placement of waste rock fill.

Controlling the rate of oxygen movement from the atmosphere to the reactive sulphides in the PAF rock is a key factor in controlling the oxidation of the sulphide minerals. Long term control of sulphide oxidation within the PAF material is achieved by the cap which has low porosity and maintains a high degree of saturation which limits oxygen movement into the embankment structure. T

he performance of the cover (the zone G cap, subsoil and topsoil) in limiting oxygen movement has been verified by field testing and from theoretical modelling. The SoilCover model has been used to evaluate performance by examining water movement and moisture concentrations within the cover itself. The SoilCover model was run for cases of an average rainfall year (2,183mm), a low rainfall year (1,424 mm) an extreme drought year (90mm) and a wet year (3,976 mm).

Main conclusions relating to the performance of the cover layer in providing long term oxidation control are:

Field measurements of oxygen movement in Zone H and Zone G have been collected over a number of years. These include measurements carried out in February of 1998, following a two month low rainfall period. The measurements show that the oxidation rates are very low and confirm the results of the SoilCover modelling work.

For further information see Rehabilitation.