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Henok Kiflu
School of Geosciences, University of South Florida
David Harro
G3 Group Forensic Consulting
Sarah Kruse
School of Geosciences, University of South
Florida
sinkhole lakes
houses
Or worse…
Example sinkhole
Stewart & Parker,
1992
Sand
Example sinkhole
Stewart & Parker,
1992
sand
Clay
Example sinkhole
Stewart & Parker,
1992
sand
Weathered Limestone
Example sinkhole
Stewart & Parker,
1992
sand
Limestone
Stewart & Parker,
1992
sand
Example sinkhole
Stewart & Parker,
1992
sand
Clay
cavity
cavity
x x
houses
Survey length limited by size of
residential lot
Optimize geometry of readings
with ‘Compare R’ method of
Wilkinson and Loke
“Horizontal cross
borehole”-can use
lessons learned from
cross-borehole methods
15-30 min per electrode
works through asphalt
Leave deep electrodes
for time-lapse
monitoring
Surface array
Surface + buried
array(MERIT)
Must have buried electrodes within
depth of sensitivity of surface array
Surface
array
MERIT array
Recover
features
below
clay
Surface only
Surface and deep electrodes
Moderate clay-limestone resistivity
contrast
High clay-limestone resistivity
contrast
surface array
Surface and Deep Array
Urban site example
array length limited by access
Lake Mellon
Resistivityarray
surface
array
MERIT
Array
Improved
image of
limestone
Increased
extent of
imaging
5.3
m
2.3
m
0m
Kruse_NS_AP_resistivity
Kruse_NS_AP_resistivity

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Kruse_NS_AP_resistivity

Editor's Notes

  1. Not true in March 2013 in Seffner, where a man vanished into a sinkhole.
  2. Not true in March 2013 in Seffner, where a man vanished into a sinkhole.
  3. 15 minutes to install electrode to 8 m depth, leaves small footprint, can be reused, could be done inside structure. Much cheaper than cross-borehole because can be installed with geoprobe or direct push and doesn’t require conventional drilling techniques.
  4. 7 hours to install array
  5. 7 hours to install array