A New
Component
in
the
Radio
Continua
of
PNe
S.
Casassus
, L.-≈.
Nyman
Ü,
, T.J.
Pearson
á
and
A.C.
Readhead
á
Departamento
de
Astr
onomÌa,
Univer
sidad
de
Chile
, Santia
go,
Casilla
36-D,
Chile
Ü
Eur
opean
Southern
Observatory
, Alonso
de
Cor
dova
3107,
Casilla
19001,
Santia
go
19,
Chile
Onsala
Space
Observatory
, 439
92
Onsala,
Sweden
á
Owens
Valle
y Radio
Observatory
, California
Institute
of
Technolo
gy, Pasadena,
CA
91125
Abstract.
A byproduct
of
experiments
designed
to
map
the
CMB
is the
recent
detection
of
a new
component
of
fore
ground
galactic
emission.
The
anomalous
fore
ground
at 10-30
GHz,
une
xplained
by
traditional
emission
mechanisms,
correlates
with
100
mu
m
dust
emission,
and
is thus
presumably
due
to
dust.
Is the
anomalous
fore
ground
ubiquitous
in
the
Galaxy?
I will
present
evidence
obtained
with
the
CBI
and
SIMB
A+SEST
supporting
the
existence
of
the
new
component
in
the
ISM
at
lar
ge,
and
in
specic
objects,
in
the
form
of
a 31
GHz
excess
over
free-free
emission
in
PNe.
Keyw
ords:
planetary
neb
ulae:
indi
vidual
(NGC
7293,
NGC
7009,
NGC
6369),
radio
continuum:
ISM,
radiation
mechanisms:
general,
infrared:
ISM,
ISM:
dust
PACS:
98.38.L
y;
98.58.Li;
98.38.-j;
INTR
ODUCTION
The
RING
5
M
experiment
(Leitch
et al.
1997)
disco
vered
an
anomalous
component
of
Galactic
radio
emission
in
the
direction
of
translucent
clouds
about
the
North
celes-
tial
pole.
The
14-32
GHz
and
100
μ
m
intensities
corre-
late,
as
expected
from
dust
clouds
photoionised
by
the
dif
fuse
UV
eld.
But
the
corresponding
H
a
emission
is
absent.
An
explanation
in
terms
of
a hot
plasma
at
10
6
K,
heated
by
shocks,
is
discarded
by
Draine
&
Lazarian
(1998a)
on
ener
getic
grounds.
The
anomalous
emission,
also
called
`fore
ground
X',
is also
present
in
the
COBE
data
(K
ogut
et
al.
1996)
as
a
DMR
-
DIRBE
correlation
signal.
A band-by-band
linear
model
between
the
31.5,
53,
90
GHz
DMR
bands
and
the
100
μ
m,
140
μ
m
and
240
μ
m
DIRBE
bands
gives
a
tight
correlation
slope
at
31.5
GHz
(
>
6
s
), but
loose
at
90
GHz.
The
DMR
-
DIRBE
signal
has
a at
spectrum,
with
a
+
0
:
3
0
:
4 (with
I
n
μ n
a
in
Jy),
and
is
tentati
vely
interpreted
as
a mixture
of
traditional
dust
and
free-free
emission
by
Kogut
et al.
(1996).
The
radio-IR
correlations
in
the
dif
fuse
ISM
are
con-
rmed
by
de
Oli
veira-Costa
et
al.
(1999);
Finkbeiner
et
al.
(1999);
de
Oli
veira-Costa
et
al.
(2002);
Lagache
(2003);
Finkbeiner
et
al.
(2002);
Finkbeiner
(2004).
In
particular
Finkbeiner
et
al.
(1999)
report
that
the
radio-
IR
signal
is not
the
Rayleigh-Jeans
tail
of
the
ISM
dust:
the
DMR
-
DIRBE
signal
is at
higher
levels
than
predicted
from
the
far-IR
data,
by
factors
of
1.2,
2.4
and
90
at 90,
53,
and
31
GHz,
respecti
vely
. de
Oli
veira-Costa
et
al.
(2004)
dispro
ve the
synchrotron
interpretation
by
Ben-
nett
et al.
(2003)
of
the
radio-IR
correlation
as
a
WMAP
fore
ground.
The
idea
that
char
ged
very
small
grains
(
VSG
s)
may
rotate
at
frequencies
reaching
observ
able
radio
frequen-
cies
originated
with
Erickson
(1957)
and
Ho
yle
&
Wick-
ramasinghe
(1970),
and
was
revived
in an
accurate
model
by
Draine
&
Lazarian
(1998b)
to
explain
the
RING
5
M
experiment.
The
spectral
ener
gy
distrib
ution
(
SED
) of
spinning
dust
rises
steeply
with
frequenc
y (
a
3),
and
then
drops-of
f with
a Boltzmann
factor
. Draine
&
Lazar
-
ian
(1998b)
obtain
a peak
at
25ñ30
GHz
and
intensity
levels
slightly
short
of
the
anomalous
fore
ground
in
the
RING
5
M
experiment.
The
spinning
dust
emission
mechanism
may
be
un-
derstood
in
crude
terms
by
assuming
equipartition
in
the
rotational
degrees
of
freedom:
1
2
I
w
2
=
kT
. For
a spher
-
ical
and
homogeneous
grain,
with
I
=
2
5
mR
2
, a radius
R
=
N
10