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The Use of Non-Invasive Geophysical Methods for Identifying Possible Karst
Induced Stability Problems in Holcim Inc. Quarry Near Holly Hill, South
Carolina
Funded by
Holcim Inc.
Project Description
Holcim Inc. operates a rock quarry near Holly
Hill, South Carolina in support of its cement manufacturing plant at the
same location. Recently, karst features have been discovered in the
vicinity of the quarrying operation. Holcim Inc. is concerned that the
unknowing encounter of a significant solution cave/channel could seriously
damage the bucket wheel excavation machine thereby risking worker safety
and jeopardizing quarry operations. Therefore, it seems prudent to first
identify and then apply investigative techniques that can “preview” areas
within the quarry for karst features prior to advancing the quarrying
equipment over suspect terrain.There are two primary
objectives for this project: 1) select a geophysical method or a
combination of methods to locate possible karst or subsurface anomalies
ahead of the mining with the sand and clay unit in place. Once the sand
and clay unit has been remove follow up with a GPR survey over areas where
suspected karst or geophysical anomalies were identified; and 2) develop a
routine schedule for conducting geophysical surveys to detect possible
stability problems on the upper bench and quarry floor prior to the mining
operations reaching suspected areas.
We propose using a scaled approach to accomplish the
objectives. Different geophysical methods have different resolution; with
resistivity and seismic refraction having coarse resolution and GPR having
the finest resolution. Based upon the results from previous studies
(Applied Geosciences, Inc) and completion of ongoing field testing of
different geophysical methods, the following methods have had positive
results. The results from the Applied Geosciences, Inc. surface
resistivity survey appear to have located possible karst or solution
features in the subsurface. The current study will follow up on the
results from Applied Geosciences using surface resistivity but with closer
electrode spacing to attempt to enhance both the vertical and spatial
resolution. Because the seismic refraction survey on the quarry floor was
successful, the technique will be tested along the same resistivity survey
lines to determine the effectiveness of locating karst features or
geophysical anomalies with the sand and clay unit in place. If karst
features or geophysical anomalies are identified either by resistivity or
seismic refraction or both, once the clay and sand unit has been remove a
follow up survey using high resolution GPR will be conducted over suspect
areas to confirm the presence or absence of these anomalous features.
Personnel
Michael Waddell: ESRI - USC
Camelia
C. Knapp: DOGS - USC
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