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THE LYMAN-a FOREST AS A PROBE OF FUNDAMENTAL PHYSICS. MATTEO VIEL. Shanghai, 16 March 2005 ... Lya physics. z 6. dynamics. termodynamics. CMB Lyman a. Long ... – PowerPoint PPT presentation

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Title: Nessun titolo diapositiva


1
THE LYMAN-a FOREST AS A PROBE OF
FUNDAMENTAL PHYSICS
MATTEO VIEL
  • Cosmological significance of the Lyman-a forest
  • 2. LUQAS The observational sample
  • Hydro-dynamical simulations of the Lyman-a forest
  • Cosmological parameters Implications for
    inflation,
  • neutrinos, gravitinos, warm dark matter
    particles


With M. Haehnelt, J. Lesgourgues, S. Matarrese,
A. Riotto, V. Springel, J. Weller
Shanghai, 16 March 2005
2
GOAL the primordial dark matter power
spectrum
CMB physics z 1100 dynamics
Continuum fitting
Lya physics z lt 6 dynamics
termodynamics
Temperature, metals, noise
Tegmark Zaldarriaga 2002
CMB Lyman a
Long lever arm
Relation P FLUX (k) - P MATTER (k) ??
Constrain spectral index and shape
3
the WMAP era
before WMAP Croft et al. 2002
Tilt in the spectrum nlt1 ? Running
spectral index dn/dlnk lt 0 ?
WMAP Verde et al. 2003
4
Wm 0.26 WL 0.74 Wb0.0463 H 72 km/sec/Mpc
- 60 Mpc/h COSMOS computer DAMTP
(Cambridge)
DM
GAS
STARS
NEUTRAL HYDROGEN
5
The LUQAS sample -I
Large sample Uves Qso Absorption Spectra (LP-UVES
program P.I. J. Bergeron) high resolution 0.05
Angstrom, high S/N gt 50 low redshift, ltzgt2.25,
Dz 13.75
Nr. spectra
redshift
Kim, MV, Haehnelt, Carswell, Cristiani, 2004,
MNRAS, 347, 355
6
The LUQAS sample II systematic errors

Effective optical depth
Low resolution SDSS like spectra
High resolution UVES like spectra
ltFgt exp (- t eff) Power spectrum of
F/ltFgt
7
Hydro-simulations scalings
T T0 ( 1 d) g-1
P FLUX (k) b2(k) P MATTER (k)
Effective optical depth
Viel, Haehnelt, Springel, MNRAS, 2004, 354, 684
8
Hydro-simulations what have we learnt? Many
uncertainties which contribute more or less
equally (statistical error is not an issue!)
ERRORS
CONTRIBUTION TO
FLUCT. AMPL.
Statistical error 4
Systematic errors 15
t eff (z2.125)0.17 0.02 8
t eff (z2.72) 0.305 0.030 7
g 1.3 0.3 4
T0 15000 10000 K 3
Method 5
Numerical simulations 8
Further uncertainties 5
9
Cosmological implications combining the forest
data with CMB - I
MV, Haehnelt, Springel 2004
SDSS Seljak et al. 2004
n 1.01 0.02 0.06 s8 0.93 0.03
0.09
Systematic error
Statistical error
Note that the flux bispectrum analysis agrees
with these values MV, Matarrese, Heavens,
Haehnelt, Kim, Springel, Hernquist, 2004
10
Cosmological implications combining the forest
data with CMB - II
MV, Weller, Haehnelt, MNRAS, 2004, 355, L23
s8 0.93 0.07 n0.99 0.03
d ns/ d ln k
SDSS Seljak et al. 2004
s8 0.90 0.03 n0.98 0.02 nrun
-0.003 0.010 nrun-0.033 0.025
11
Cosmological implications constraints on
slow-roll inflation - III
MV, Weller, Haehnelt, MNRAS, 2004, 355, L23
V inflaton potential
T/S
r lt 0.45 (95 lim.)
r 0.50 0.30 No evidence for
gravity waves
SDSS Seljak et al. 2004
T/S
12
Cosmological implications Warm Dark Matter
particles-I
LCDM
WDM 0.5 keV
30 comoving Mpc/h z3
In general
if light gravitinos
k FS 5 Tv/Tx (m x/1keV) Mpc-1
k FS 1.5 (m x/100eV) h/Mpc
Set by relativistic degrees of freedom at
decoupling
MV, Lesgourgues, Haehnelt, Matarrese, Riotto,
PRD in press
13
Cosmological implications Warm Dark Matter
particles-II
LWDM
LCWDM (gravitino like)
W gravitino/ W DM
Scale of free streaming
Set limits on the scale of Supersymmetry
breaking L susy lt 260 TeV
m WDM gt 550 eV gt 2keV sterile
neutrino lt 16 eV gravitino
14
Cosmological implications constraints on
neutrinos
WMAP 2dF Lyman-a
S mn (eV) 0.33 0.27
15
HPM simulations of the forest
Full hydro 2003 part.
HPM PMGRID600 HPM
PMGRID400
FLUX POWER
16
HIGH RESOLUTION HIGH S/N vs
LOW RESOLUTION LOW S/N
17
LUQAS vs SDSS
18
SUMMARY
  • LUQAS a unique high resolution view on the
    Universe at z2.1
  • 2. Hydro-dynamical simulations of the Lyman-a
    forest. Systematic
  • Errors? Differences between hydro codes?
  • Cosmological parameters no fancy things going on
  • s8 0.93 n 1 no running
  • substantial agreement between SDSS and LUQAS but
    SDSS has
  • smaller error bars not because of the larger
    sample but because of
  • the different theoretical modelling
  • Constraints on inflationary models, neutrinos
    and WDM

19
HPM simulations of the forest-I
equation of motion for gas element
if T T0 ( 1 d) g-1
Gnedin Hui 1998
20
Feedback effects Galactic winds
No Feedback
Feedback
Density
Temperature

21
Feedback effects Galactic winds-III
Line widths distribution
Column density distribution function
22
Metal enrichment CIV systems at z3
Strong Feedback e1 ---- Role of the UV background
Mori, Ferrara, Madau 2000 Rauch, Haehnelt,
Steinmetz 1996 Schaye et al. 2003
Soft background ---- Role of different feedback
e0
e1
e0.1
23
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