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PROJECTS
Contact Information:
Prof. Massimiliano Galeazzi
P.O. Box 248043
Coral Gables, FL 33124
Tel: (305) 284-2326 x2
Fax: (305) 284-4222
galeazzi@physics.miami.edu
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Diffuse
X-Ray emission from the Local galaxy (DXL)
Massimiliano
Galeazzi
(PI),
Meng
Chiao, Michael R. Collier, Thomas Cravens, Dimitra
Koutroumpa, Kip Kuntz, Susan Lepri, Dan McCammon, F. Scott Porter, Ina
Robertson, Steve Snowden, and Youaraj Uprety
University
of
Miami,
NASA/Goddard
Space Flight Center, University of Michigan, Johns Hopkins
University, and University of
Kansas
The first detection of extrasolar X-rays
came in 1962 with the
presence of a diffuse X-ray flux identified by a series of three papers
in
1968-69. Subsequent investigations, primarily the Wisconsin rocket
survey and
the Rosat All Sky Survey (RASS) extensively studied the nature of the
diffuse
emission and its correlation with the neutral material in the Milky
Way. X-rays
observed in the 1/4 keV band in the direction of the Galactic plane
must
originate locally as they are easily absorbed by the neutral material
in the
Galactic disk and it is currently believed that a significant fraction
of the
1/4 keV emission originates in an irregularly shaped cavity in the
neutral
hydrogen of the Galactic disk which contains the Sun and has dubbed the
Local
Hot Bubble (LHB). Despite the “local” origin of the emission, there is
still a
significant uncertainty in its nature and characteristics. The reason
for this
uncertainty lies primarily in the nature of the emission, which is weak
and
diffuse, and its superimposition on emission from other sources of the
Diffuse
X-ray Background (DXB). In particular, it
has been essentially impossible to isolate the LHB contribution from
the
emission from Solar Wind Charge eXchange (SWCX) recombination. SWCX
emission is
generated when the highly ionized
solar wind interacts with neutral or near-neutral gas in the
exo-atmosphere and
in the interplanetary medium. An electron is captured from the neutral
atom (H
or He) into an outer orbital of the highly ionized species in a
quasi-resonant process
and cascades to the ground state of the ion, often emitting soft X-rays
in the
process. The SWCX spectrum is therefore dominated by characteristic
line
emission that is very difficult to separate from the presumably thermal
emission from the LHB.
It is, however, possible to separate the
foreground SWCX
emission from the extra-solar sources, such as the LHB, by looking at
its
spatial signature. The slowest time-varying, and thus most troublesome
component of the SWCX emission originates in the interplanetary medium
and should
show a significant geometric variation due to the focusing of
interplanetary
helium. Interstellar neutrals flow through the solar system due to the
motion
of the heliosphere through the local interstellar cloud. Gravity
significantly affects
helium trajectories which execute Keplarian orbits and form a “focusing
cone” downstream
of the Sun centered at ~ 6◦ below
the ecliptic plane. This results in a localized downstream enhancement
of
helium which has the direct effect of increasing the SWCX X-ray
emission. By
scanning the sky through the focusing cone, the spatial signature of
the SWCX
can be identified, allowing:
(a)
a
separation and subsequent investigation of LHB and SWCX emission, such
as the
distribution of the hot plasma within the LHB. Combining this
information
with the geometry of the local cavity derived from other wavelengths we
can
then derive the physical parameters of the plasma, that is, the
pressure and
density. Knowing the physical conditions of the plasma will lead to
more
accurate pictures of the solar neighborhood and the evolution of
bubbles of hot
gas produced by supernovae or stellar wind when they near the end of
their
existence;
(b)
an
estimate of the contribution of heliospheric SWCX to the University of
Wisconsin
and ROSAT all-sky maps of the soft x-ray background, and to every
current and
future investigation of extended sources.
Current and near-term satellite missions
have only a tiny
fraction of the grasp of the proposed payload and are thus not-suitable
for the
proposed investigation. In addition, the X-ray Quantum Calorimeter
(XQC)
sounding rocket program is currently studying the spectral signature of
the
soft x-ray background, including the SWCX and LHB contributions with a
high
resolution microcalorimeter. XQC has limited grasp and limited spatial
resolution and this investigation, by verifying our spatial models of
the SWCX
emission, is a critical complement to the XQC results.
DXL is
composed of two large area (500 cm2 each at 1 keV) thin
window
proportional counters that were used to produce the original UW all-sky
soft
X-ray maps. The large area of the proportional counters will provide
excellent
counting statistics when scanning the sky though the He focusing cone
in the
limited observing time of a sounding rocket flight. For the scan we
have chosen
a region sufficiently close to the galactic plane to absorb soft X-rays
produced outside the solar system and its local environment (within
~100 pc),
therefore minimizing the intensity and structure of the cosmic
background, as
indicated by the RASS. DXL will be launched from White Sands
Missile Range in New Mexico during the month of December 2013 to ensure
a
scanning path through the He focusing cone when the sun is close to the
maximum
of its 11 year cycle. Contrary
to what may be expected, a solar maximum corresponds to a lower SWCX
emission because the higher solar flux ionizes
the bulk of the H in the inner solar system, removing many of the
neutrals involved in the charge
exchange. The SWCX emission will still be significant to see its
spatial
signature, but won’t overshadow the LHB emission.
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