Decant of sigma colliery
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Wessels, Lize
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University of the Free State
Abstract
Showing abstract in English
English: This study of Sigma Colliery was intended:
• To determine the water quality of each aquifer associated with the mining area.
• To determine the overall electrical conductivity profile of the mine to aid in the
overall management of the mine.
• To delineate possible decant positions with the help of water levels and to
determine what the water quality of the possible decanting water will be.
• To discuss the use of fly ash as a backfilling material in underground mines with
the help of case studies.
• To determine if ashfilling is a viable option for Sigma Colliery.
From the study of Sigma Colliery, the following conclusions and recommendations
could be made in this document:
• A total of 12 samples were obtained from the shallow aquifer, classified
according to the SANS 241 :2006 drinking water standards and discussed in this
document. Only sample WW024D was classed as above the maximum
allowable limit and not suitable for human consumption. Four samples were
classed within Class 2, suitable for human consumption for a limited duration
use only. A total of seven samples were classed as Class 1, suitable for human
consumption.
• A total of 23 samples were obtained from the intermediate aquifer, classified
according to the SANS 241 :2006 drinking water standards and discussed in this
document. Samples WW036, NW021, NW037 and UG001 were classed as
above the maximum allowable limit and not suitable for human consumption.
Three samples were classed as Class 2, suitable for human consumption for a
limited duration use only while 16 samples were classed as Class 1, suitable for
human consumption.
• A total of 21 samples were obtained from the deep aquifer system, classified
according to the SANS 241 :2006 drinking water standards and discussed in this
document. Samples NW006, NW036, NW040, NW041, NW042, NW044,
NW046, NW051, UG027D, UG071, UG072D and UG072M were classed as
above the maximum allowable limit and not suitable for human consumption.
Two samples were classed within Class 2, suitable for human consumption for a
limited duration use only and seven samples were classed as Class 1, suitable
for human consumption.
• A total of six samples were obtained from the disturbed aquifer system,
classified according to the SANS 241 :2006 drinking water standards and
discussed in this document. Samples UG014 and UG023 were classed as
above the maximum allowable limit and not suitable for human consumption.
Two samples were classed within Class 2, suitable for human consumption for a
limited duration use only and two samples were classed as Class 1, suitable for
human consumption.
• A total of 20 samples were obtained from the ashfill boreholes, classified
according to the SANS 241 :2006 drinking water standards and discussed in this
document. Samples UG033, UG034, UG044, UG069, 812/179, 812/1830,
812/183M and 812/183S were classed as above the maximum allowable limit
and not suitable for human consumption. Only one sample (sample C316/47)
was classed within Class 2, suitable for human consumption for a limited
duration use only and 11 samples were classed as Class 1, suitable for human
consumption.
• A total of 19 samples were obtained from the mine boreholes, classified
according to the SANS 241 :2006 drinking water standards and discussed in this
document. Samples UG0130, UG024, UG0370, UG046, 812/530 and
812/53S were classed as above the maximum allowable limit and not suitable
for human consumption. Five samples were classed within Class 2, suitable for
human consumption for a limited duration use only and eight samples were
classed as Class 1, suitable for human consumption.
• All 94 boreholes were profiled and a three-dimensional image of the whole area
was created with the use of the electrical conductivity profiles. From this image
created, varies possible decant areas were identified and the water quality of
these possible decant areas were discussed.
• The ashfilling used turned out to be a viable option when there was still mine
void space available before the mine was filled up with water from the flooding.
• Since the mine voids were filled with water and the fine ash slurry was pumped
into the mine voids, the conditions was disturbed in that the void space in the
mine was decreased with some volume of water.
• The storage of the strata above is not enough for the water that was pumped in
with the ash and the water is therefore forced to decant.
• The only place where decant and pollution of the shallow aquifer is evident is
where ashfilling has been done.
• The situation improves as soon as the ashfilling is ceased and this can be
substantiated by the water level and water quality behaviour of borehole
UG069. The water levels of borehole UG069 has been at decanting levels from
September 2009 to March 2012 (Figure 15-3) after which the water level started
to decrease again after the ashfilling was ceased. From the electrical
conductivity profiling done of borehole UG069 (Figure 15-2) (after the ashfilling
was ceased) the profile already indicates that the upper part of the water
column is of a better quality than deeper down.
• In this document it is therefore recommended that in the event that the company
would like to continue with the ashfilling, they should pump water out of the
mine to provide void space and prevent decant.
• The ash slurry should simultaneously be injected into the mine with the water
that is pumped out. This should be pumped in equal volumes, which will prevent
other problems such as the collapsing of the mine roof.