HYDROGEOCHEMICAL
INVESTIGATION OF REACTIVE TAILINGS AT THE WAITE-AMULET TAILINGS
SITE, NORANDA, QUEBEC - 1985 PROGRAM
Mine Environment Neutral Drainage at CANMET-MMSL |
MEND Project
1.17.la
July 1986
EXECUTIVE
SUMMARY
Noranda Inc.
initiated a five-year research program in 1985 undertaken by Noranda
Research Centre to conduct a hydrogeochemical investigation of the
reactive Waite Amulet tailings area near Noranda, Quebec. This study
is part of the national Reactive Tailings Study (RATS) Program.
A jointly funded Noranda-CANMET $100,000 study for 1985 consisted
of a preliminary site reconnaissance and drilling program to provide
a baseline indication of the underlying geologic materials and their
variations, the tailings depth, water table, mineralogy, pore water
chemistry. pore water hydraulic conductivity and direction of flow.
Bacterial activity was also assessed.
The evaluation
of the hydrogeology and geochemistry of the Waite Amulet tailings
area will provide an indication of where the acid generation is
occurring and its regulating factors. This will assist in developing
control techniques which would eliminate the need for perpetual
maintenance and treatment of acid water from reactive tailings area.
The 1985 field
program indicated that the Waite Amulet tailings, which varies in
thickness from 2 to 15 m, is underlain by moderately regular clay
with thickness varying from 2 to 20 m. The water table is near surface
in the northern section and up to 5.5 m below surface in the southern
section. Hydraulic conductivity's range from 9 x 10-7 to 1.4 x 10-3
Cm/s. Porewater horizontal velocities within the tailings range
from 0.4 cm/y to 5 m/y. Velocities across the dam face are up to
35 m/y.
Below the water
table, pH is generally above pH 6, and in the unsaturated zone,
the pH ranges from 3 to 6. Thiobacillus ferrooxidans, are
present only above the water table and there was a minimal count
of sulphate-reducing bacteria below the water table.
The 1986 program
will: resolve the hydrogeological uncertainties concerning the site;
evaluate the geochemistry in the unsaturated zone and dam face;
assess oxidation control options for 1987-1989.
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