SLIDE 4 Hydrology Are the
influences
mining on
hydrology to reduce the protective layer of the aeration
zone
raise
the water
level
in
light
level
data
noted
by ADWR alter hydraulic gradients causing
changes
in
flow direction and speed
alter
natural retention
features and
create turbid ground
water due
to rock fracturing
To clarify
there will be no
underground mining
at the Florence
Copper
Project Curis proposes to recover
copper by injecting low pH
solution into the orebody and then
pumping
it out via
recovery wells
copper
minerals have dissolved into solution
Pumping
will draw
water from
injection wells to recovery wells and
prevent the movement
solutions
The area of groundwater affected by
this process
is restricted
to the project well field
Surrounding groundwater
will continue to flow around the orebody in
northwest
direction Hydrofracturing
will not be undertaken at the Florence
Copper
Project
Are discontinuities
such as faults
and fracturing encountered
more frequently
with the injection/recovery
system
Consequently when
fracture flow
does
it make it much
more
difficult
in underground
metals
mining to predict where
and
when
hydrologic impacts will occur
To clarify
there will be no
underground mining
at the Florence
Copper
Project The orebody
is
highly fractured
by nature which
is idealfor
the
in-situ
copper
recovery
ISCR process
The existing Underground Injection Control
UIC permit issued by the
EPA
prohibits hydrofracturing
at this site This means that no new fracturing will be allowed during the injection and recovery
process
Injected
fluids are expected
to flow along naturally
fractures
in the orebody
from
injection wells to recovery wells The faults that
exist
at the site are actually
fault zones
that consist
number of parallelfractures
in fairly
close proximity to
another
These fault zones do have higher hydraulic conductivity
than the surrounding
less fractured
rock
The location and extent
been thoroughly studied by previous
site owners
and Curis intends to add to this knowledge
base
Wells will be located so that they avoid
fault zones
The EPA UIC permit requires that hydraulic control
fluids is maintained
at all times
by creating and
sustaining localized hydraulic gradient that
draws
the injected
fluids to the
recovery wells
The water willflow
along the naturalfractures from
the injection wells to the recovery wells
but not beyond Are water-table
drawdown
predictions generally
based
the
assumption that
geologic materials transmit
water equally
in all
directions
isotropic and
that they are the same
great distance
homogenous
Could
formations as structural
features
such as faults
and fractures control
magnify
and
extend drawdown
in
selected directions Curis
water table drawdown
predictions will be based
actual geological characteristics that include naturally
variation anisotropic and heterogeneous On broad scale geologicalfeatures
will affect
drawdown
predictions
however
Curis UIC
permit requires
that
water drawdown
is managed
very
tightly in the injection
area Drawdown
effects
in the injection area will not extend more than
few tens of feet
in any direction outside
the injection
area regardless
heterogeneity and
anisotropy
CURlS RESOURCES ARIZONA INC
1575
Hunt Highway Florence
Arizona 85132
USA
florencecopperproj ect.com
SWVP-019245