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The launch of the XMM-Newton and the Chandra X-ray observatories
with imaging capabilities at hard energies (2-10keV) has given new
impetus in studies of the nature of the sources that make up the
diffuse X-Ray Background (XRB). In the pre-Chandra and
XMM-Newton era models have been developed that re-constructed the
XRB by assuming a mix of obscured and unobscured AGN. The main
prediction of these models was a dominant population of heavily
obscured systems. This however, has not been confirmed by recent
XMM-Newton and Chandra surveys, suggesting that revision of the model
assumptions is required (see figure).
These surveys indicate that the fraction of obscured sources
(NH>1022cm-2) is not constant, as
the earlier versions of the XRB models assume (see figure), but
depends on X-ray luminosity: more powerful AGN comprise a smaller
fraction of obscured sources. For example wide angle shallow
surveys, probing mostly luminous QSOs (see figure; Georgantopoulos
et al. 2004; Akylas et al. 2006),
estimate an obscured AGN fraction of ~20-30%. On the contrary,
ultra-deep pencil-beam surveys, comprising many moderate luminosity
AGN, find this fraction to be close to 80% (see figure; Perola et
al. 2004; Treister et al. 2005), similar to the value determined in
the local Universe.
We have recently completed a deep Chandra survey in the Extended
Groth Strip region (Nandra et al. 2005). This consists of
8x200ks Chandra pointings covering a total area of
0.5deg2 and is
intermediate to ultra-deep and shallow samples, in terms
of both area and flux limit. Initial results confirm the rapid
change of obscured AGN fraction with luminosity (of flux; see
figure). The advantage of our sample is that it probes the flux
regime where the rapid change in the obscured AGN fraction occurs,
providing the opportunity to explore this in detail. Additionally,
the X-ray observations are part of the All-wavelength
Extended Groth strip International Survey (AEGIS), which provides
multiwavelength data, essential to understand the nature of
the sources responsible for the XRB. These include deep optical
spectroscopy from the DEEP2,
optical photometry from the CFHTLS,
near, mid and far-IR data.
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