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Document Description
Title
Experimental
and
numerical
study
of
solute
transport
through
saturated
fractured
porous
aquifer
Author
Amoah
,
Nelson
,
1958-
Description
Thesis
(Ph.D.)--Memorial
University
of
Newfoundland
,
1997.
Engineering
and
Applied
Science
Date
1997
Pagination
xvi, 284 leaves : col. ill., maps, graphs
Subject
Aquifers;
Groundwater
tracers;
Groundwater--Pollution
Degree
Ph.D.
Degree Grantor
Memorial University of Newfoundland. Faculty of Engineering and Applied Science
Discipline
Engineering and Applied Science
Language
Eng
Notes
Blbliography:
leaves
223-235.
Abstract
The
evaluation
of
groundwater
pollution
in
different
subsurface
media
has
always
been a
challenging
task.
The
knowledge
required
for the
conceptual
basis
for
analysis
is
often
insufficient.
Site
specific
data
are
usually
not
available.
In
fractured
formations
further
difficulties
arise
since
contaminant
migration
patterns
are
influenced
in a
complex
way
by the
variability
of
fracture
characteristics.
In
addition
many
numerical
models
have been
found
to be
inefficient
in
handling
the
equations
governing
subsurface
contaminant
transport.
This
means
that the
investigator
is
confronted
with
several
sources
of
uncertainties
arising
from
both
the
input
data
and the
numerical
model
itself.
--
This
thesis
presents
a
field
experiment
and
numerical
study
of
solute
transport
through
a
saturated
fractured
aquifer
located
in
St.
John's
,
Newfoundland
,
Canada.
The
aquifer
at the
test
site
consists
of a
thin
glacial
till
overlying
a
fractured
bedrock.
The
investigation
comprised
two
parts.
The
first
part
involved
several
months
of
groundwater
level
monitoring
, in
situ
tests
for
hydraulic
conductivity
and
study
of the
groundwater
chemistry.
High
spatial
variability
of
hydraulic
conductivity
in the
bedrock
aquifer
was
observed.
The
second
part
involved
two
natural
gradient
tracer
tests.
Experimental
results
indicate
that there
is
limited
hydraulic
communication
between
the
overlying
till
and the
fractured
bedrock.
Tracer
migration
patterns
in the
bedrock
suggest
a
dense
network
of
highly
interconnected
fractures
which
cannot
be
represented
on
individual
scale.
Tracer
migration
in the
bedrock
showed
no
evidence
of
flow
channeling.
The
concentration
distribution
has been
represented
by
breakthrough
curves.
--
Knowledge
from the
field
study
has been
used
to
develop
an
efficient
numerical
model
for
solute
transport
based
on the
advection-dispersion
equation.
The
numerical
model
was
based
on the
dual
reciprocity
boundary
element
method
(DRBEM).
A
new
approach
in the
application
of this
technique
to a
class
of
non-linear
,
nonhomogeneous
equations
has been
proposed.
Several
numerical
experiments
to
test
the
accuracy
and
efficiency
of the
new
model
have been
performed.
Numerical
results
showed
that the
new
approach
improves
the
accuracy
of the
DRBEM.
Good
agreement
was
obtained
between
model
results
and the
analytical
solutions
for
several
theoretical
test
problems.
The
ability
of the
DRBEM
to
handle
the
dual
nature
of the
advection-dispersion
equation
was also
recognized
by
achieving
accurate
results
at
high
Peclet
numbers.
The
efficiency
of the
DRBEM
compared
with
other
numerical
solution
techniques
was also
observed.
--
The
DRBEM
model
was
applied
to a
practical
field
situation
by
using
the
results
from a
tracer
test.
Numerically
simulated
breakthrough
curves
were
compared
with the
experimental
results
obtained
from the
tracer
test.
Aquifer
parameters
optimized
for a
reasonable
match
between
the
numerically
simulated
and the
experimental
results
have been
estimated.
Simulation
results
suggest
that the
advection-dispersion
model
is
highly
suitable
for
solute
transport
analysis
in this
aquifer.
Sensitivity
analysis
has been
performed
by
computing
sensitivity
coefficients
for the
various
aquifer
parameters.
The
field
experiment
and the
numerical
study
have
provided
considerable
insights
into the
processes
controlling
solute
transport
in this
fractured
aquifer.
Type
Text
Resource Type
Electronic
thesis
or
dissertation
Format
Image/jpeg;
Application/pdf
Source
Paper copy kept in the Centre for Newfoundland Studies, Memorial University Libraries
Local Identifier
a1228570
Rights
The author retains copyright ownership and moral rights in this thesis. Neither the thesis nor substantial extracts from it may be printed or otherwise reproduced without the author's permission.
Collection
Electronic
Theses
and
Dissertations
Scanning Status
Completed
PDF File
(32.30
MB)
--
http://collections.mun.ca/PDFs/theses/NelsonAmoah_1.pdf
CONTENTdm file name
46246.cpd