RENAL
STONES
Renal
calculi
are
common
and
typically
arise
within
the
collecting
system.
Plain
radiographs
and
intravenous
urography
are
the
traditional
investigations
for
renal
colic.
Ultrasound
has
the
advantage
of
demonstrating
non-opaque
calculi
and
hydronephrosis
in
comparison
with
the
plain
radiographs.
Ultrasound
has
the
potential
of
early
diagnosis
as
compared
with
intravenous
urography.
Most
renal
calculi
(about
80%)
are
calcified.
Sonographically,
stones
usually
appear
as
a
hyperechoic
foci
with
distal
acoustic
shadowing
(Picture1).
Gas
may
cause
a
similar
appearance
but
may
have
a
"dirty"
shadow
that
is
not
as
sharply
defined
as
would
occur
with
a
calculus.
There
may
be
associated
mucosal
edema
if
the
stone
is
impacted
or
if
there
is
secondary
inflammation
or
infection.
Hydronephrosis
and
hydrourether
may
also
be
present.
Tiny
calculi
may
not
cause
distal
shadowing
if
they
are
smaller
than
the
focal
zone
of
the
transducer.
When
there
is
no
shadowing,
it
may
be
difficult
to
distinguish
small
calculi
from
echogenic
foci
caused
by
fat
or
other
echogenic
reflectors
within
the
renal
sinus.

Picture1.
Two
stones
in
kidney.
Ultrasound
may
have
false-negative
results
with
small
calculi
and
suboptimal
studies
(e.g.,
obesity,
uncooperative
patient).
Ultrasound
may
have
false-positive
results
with
renal
parenchymal
calcification,
vascular
calcification,
and
uretheric
catheters.
Staghorn
calculi
often
appear
as
multiple,
disconnected
calculi
within
the
collecting
system
(Picture2).
Sonography
generally
underestimates
the
extent
and
size
of
stones
in
patients
with
staghorn
and
other
large
calculi.
The
presence
of
staghorn
calculi
may
make
it
difficult
to
diagnose
underlying
hydronephrosis,
because
of
strong
acoustic
shadowing
from
calculi.

Picture2.
Staghorn
calculi
Renal
calcification
also
occur
in
patients
with
medullary
sponge
kidney
and
in
patients
with
nephrocalcinosis.
REFERENCES:
[1]Abdominal
Ultrasound.
E.E.Sauerbrei,
K.T.Nguyen,
R.L.Nolan.
1992.
[2]Sonography
of
the
Abdomen.
R.B.Jeffrey,
P.W.Rolls.
1995
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