Mercury Distribution around Taconite Concentrators
2003-12-09
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Mercury Distribution around Taconite Concentrators
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2003-12-09
Publisher
University of Minnesota Duluth
Type
Technical Report
Abstract
Sources of mercury in the environment have become an area of concern for the various
regulatory agencies. Taconite production has been identified as one of the sources. Previous
programs have indicated that the majority of the mercury in the ore is rejected to the tailings
basins, but it appeared that some plants rejected a greater portion than other plants. The purpose
of this study was to determine if the differences in mercury rejection were ore related or
flowsheet related. Samples were taken around the various concentrator unit operations from
!spat-Inland, National Steel Pellet Company, Evtac, Hibtac, and Minntac. The sampling
program was not designed to provide definitive mercury balances around the concentrator, but
rather to provide a "snapshot" of what was happening with each unit operation. Each unit
operation was sampled so that the feed was taken first, followed quickly by simultaneous
sampling of the concentrate and tails. This sampling should provide a good balance around each
unit operation. The sampling protocol, potential error sources, and measures to minimize the
various potential errors are discussed.
All of the samples were analyzed for total iron, Satmagan iron, silica, alumina, calcium,
magnesium, manganese and sulfur at the Coleraine Minerals Research Laboratory (CMRL). A
split of each sample was sent to Frontier Geosciences for total mercury analyses and sequential
extraction mercury analyses on the feed, coarse tails, fine tails and concentrate samples from
each plant. The sequential extraction is supposed to give an indication of the mercury
compounds present. It was anticipated that the sequential extraction method could be used to
determine if different plants had different forms of mercury in their ore and if different mercury
compounds behaved differently during concentration. The first stage of extraction uses DI
water; the second stage uses a pH 2 solution; the third stage uses lN KOH; the fourth stage uses
12N nitric acid; and the fifth and final stage uses aqua regia.
The mercury content in the plant crude ore feeds ranged from a low of 9.44 ppb to 27.90
ppb. The plant concentrates ranged from a low of 6.19 ppb to a high of 16.10 ppb. There
appeared to be no relationship between the mercury in the feed and the mercury in the
concentrate. The standard Excel correlation program was run to relate the various elements to
the mercury analyses. For all plants the correlation coefficients for sulfur and mercury content
were greater than 0.8 and were greater than 0.9 for four of the five plants. As would be
expected, the mercury content correlated positively with the gangue elements and negatively
with the iron and magnetic iron analyses. This indicates a selective rejection of mercury to the
tails and suggests that the mercury is not associated with the magnetite.
The sequential extractions indicated no significant leaching of mercury in either the water
or pH 2 solution. This indicates that there is no easily solubilized mercury present in the ore and
that the mercury rejected to the tailings should not leach into the water. The sequential
extractions indicated no obvious differences in the feed to the five plants. There is some
question as to whether the sequential extraction is reflecting different mercury forms or is just
indicating the difficulty in extracting mercury from the mineral lattices. The sequential
extractions indicated no differences in plant performances.
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NRRI Technical Report;NRRI/TR-2003/30
CMRL Technical Report;CMRL/TR-03-10
CMRL Technical Report;CMRL/TR-03-10
Funding information
University of Minnesota Duluth, Natural Resources Research Institute, 5013 Miller Trunk Highway, Duluth, MN 55811-1442; Coleraine Minerals Research Laboratory, One Gayley Avenue, Box 188, Coleraine, MN 55722
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Benner, Blair R. (2003). Mercury Distribution around Taconite Concentrators. Retrieved from the University Digital Conservancy, https://hdl.handle.net/11299/188358.
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