measurements of thermal pressures for interstellar diffuse ... · diffuse intercloud medium (the...
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MeasurementsofThermalPressuresforInterstellarDiffuseGasintheLocalPartofourGalaxy
EdJenkins
PrincetonUniversityObservatory
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Fromtheamountoffine-structureexcita=onofCIineachcase,wehavederivedinforma=ononthethermalgaspressureswithinthediffuseclouds.Mostcloudshavep/kbetween103cm-3Kand104cm-3K,butwefoundthatatleast6%oftheCI-bearingmaterialisatp/k>104cm-3K,andone-thirdofthegashasupperlimitsforpressurebelow103cm-3K.
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Overall Average ISM Pressure in the Galactic Midplane
• Total pressure p/k ≈ 2.5 × 104 cm-3K – Arises from the weight of material in the Galactic
plane’s gravitational potential (Boulares & Cox 1990: ApJ, 365, 544)
• Many forms of pressure: – Thermal – Magnetic Fields – Dynamical (or Turbulent) – Cosmic Rays
pressure p/k only of order 4 × 103 cm-3K
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ClassicalPhaseDiagramforaNeutral,Sta'cISM
40 The Role of the Disk-Halo Interaction in Galaxy Evolution
Fig. 1. Left panel: thermal pressure corresponding to thermal equilibrium between heat-
ing and cooling for the atomic ISM. Figure from Vazquez-Semadeni et al. (2007), using
the (errata-free) fit to the cooling function by Koyama & Inutsuka (2002). The horizon-
tal dotted line indicates a mean pressure P0 that allows the medium to spontaneously
segregate into a diffuse, warm phase and a cold, dense one, indicated by the heavy dots.
Right panel: schematic illustration of the density probability density function (PDF) for
the two-phase model. The vertical axis is in arbitrary, non-normalized units, and the
relative amplitude of the peaks is meant to simply illustrate the fact that most of the
volume is occupied by the WNM.
due to the net heating and cooling processes to which the ISM is subject, the ther-mal pressure Peq corresponding to thermal balance between heating and cooling isa non-monotonic function of the density (Fig. 1, left panel). As is well known, thenegative-slope portion of this curve corresponds to a density range that is unstableunder the isobaric mode of the thermal instability (TI; Field 1965). Thus, if theambient pressure lies within the thermally unstable range, such as the pressure P0shown in Figure 1 (left panel), the medium would tend to naturally segregate intotwo stable phases2 at the same pressure, but very different densities and tempera-tures, indicated by the heavy dots in the figure, and which are commonly referredto as the warm and the cold neutral media (respectively, WNM and CNM). Thisis the well-known “two-phase” model of the ISM. In it, the final state of the insta-bility would be a collection of cold, dense clumps (the CNM) immersed in a warm,diffuse intercloud medium (the WNM), in thermal and pressure equilibrium. Thedensity contrast between the cold clumps and the WNM was expected to be ∼100.The initial sizes of the cloudlets were expected to be small, were assumed to formby merging (coagulation) of smaller cloudlets (e.g., Oort 1954; Field & Saslaw1965; Kwan 1979). In this scenario, the density and temperature probability den-sity functions (PDFs, or histograms) of the atomic ISM would consist of two Dirac
2Thermodynamically, a phase is region of space throughout which all physical properties ofa material are essentially uniform (e.g., Modell & Reid 1974). A phase transition is a boundarythat separates physically distinct phases, which differ in most thermodynamic variables exceptone (often the pressure).
T = 6500 K T = 50 K
Ther
mal
Pre
ssur
e
Diagram taken from Vázquez-Semadeni (2012) “Are there Phases in the ISM?”
Local Particle Density
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CoolingFunc=onNote:Thisisnottheconven=onalrepresenta=onintermsofergcm3s-1
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Hea=ngFunc=onPrimarysourceofheatisfromtheac=onofstarlightondustgrains,whichemitenerge=cphotoelectrons–cosmicrayhea=ngisminorbycomparison.
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BothFunc=onstheat = 5
2kT
Γ− n(H)Λ
tcool = 52
kTn(H)Λ−Γ
Isobarice-folding@me
Isobarice-folding@me
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CoolingandHea=ng
106107
105
108
104
104105106107108∞
Cooling=me(yr)Hea=ng=me(yr)
tcool = 52
kTn(H)Λ−Γ
; theat = 52
kTΓ− n(H)Λ
Fordetailsonphysicalprocessesthatleadtotheconstruc=onoftheequilibriumcurve,seeWolfireetal.(1995:ApJ,443,152,2003,ApJ,587,278).
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CoolingandHea=ng
106107
105
108
104
104105106107108∞
Cooling=me(yr)Hea=ng=me(yr)
WNM CNM
AverageISMpressure
Isobaricchangesintemperatureanddensity
Detailed,rigorousdevelopmentofthenatureofthethermalinstabilityintheISMwasofferedbyField(1965,ApJ,142,531),buildingonearlierdiscussionsbyParker,Zanstra,SpitzerandWeyman.
tcool = 52
kTn(H)Λ−Γ
; theat = 52
kTΓ− n(H)Λ
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106107
105
108
104
104105106107108∞
Cooling=me(yr)Hea=ng=me(yr)
pmin
pmax
PressureRangeforaSta=c,2-Phasemedium
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pmin
pmax
Toomuchmaterialcondensesintogravita=onallyboundclouds,whichincreasestherateofstarforma=on
Whathappenswhen
A principle outlined by Ostriker, McKee & Leroy 2010
Regula=onofstarforma=on
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pmin
pmax
Toomuchmaterialrevertstothediffusephases,whichinhibitstheforma=onofgravita=onallyboundcloudsandstars
Whathappenswhen
A principle outlined by Ostriker, McKee & Leroy 2010
Regula=onofstarforma=on
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Prediction by Jenkins, Jura & Loewenstein in 1983:
Jenkins & Tripp (2001, 2011) analyzed UV spectra of 89 stars recorded at a resolution of 1.5−3 km s-1 by the Space Telescope Imaging Spectrograph (STIS) on HST.
Reality about 18-28 years later:
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Nine C I absorption multiplets in the UV spectrum of λ Cep (Jenkins & Tripp
2001, ApJS, 137, 297)
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Fine-structure Levels in the Ground State of C I
3P0 (E = 0 cm-1, g = 1) 3P1 (E = 16.4 cm-1, g = 3)
3P2 (E = 43.4 cm-1, g = 5)
C I C I*
C I**
Upper Electronic Levels
Collisionally Induced Transitions
Optical Pumping (by Starlight) Spontaneous Radiative
Decays
E/k = 23.6 K
E/k = 62.4 K
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MostUsefulWaytoExpressFine-structurePopula=onRa=os
• n(CI)total=n(CI)+n(CI*)+n(CI**)• f1≡n(CI*)/n(CI)total• f2≡n(CI**)/n(CI)total
f1f2Thenconsidertheplot:
Collision partners at a given density and temperature are expected to yield specific values of f1 and f2
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n(H)=10cm-3
n(H)=100cm-3
n(H)=1000cm-3
n(H)=104cm-3
n(H)=105cm-3
CollisionalExcita@onbyNeutralH
T=100K
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TracksforDifferentTemperatures
n(H)=100cm-3
T=30K
T=60K
T=120K
T=240K
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TracksforDifferentTemperatures
T=30K
T=60K
T=120K
T=240K
p/k=104cm-3K
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Cloud1
Cloud2
ATheoremonhowtodealwithsuperposi=ons
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ATheoremonhowtodealwithsuperposi=ons
CI-weighted�CenterofMass�givesComposite
f1,f2
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Outcomesfrom89Sightlines
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MustCorrectforIoniza=onEquilibium
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N(CII)[cm
-2]
Logp/k
BestfitGaussianprofile:meanLog(p/k)=3.58,σLog(p/k)=0.175Tailsofthedistribu@onare
abovethatgivenbythebest-fitlog-normaldistribu@on–thisisbestseeninalog-logplot.
Jenkins & Tripp (2011: ApJ, 734, 65)
PressureDistribu=onFunc=on
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Logp/k
p min
p max
Jenkins & Tripp (2011: ApJ, 734, 65)
N(CII)[cm
-2]
PressureDistribu=onFunc=on
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HighPressureMaterial
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Fromtheamountoffine-structureexcita=onofCIineachcase,wehavederivedinforma=ononthethermalgaspressureswithinthediffuseclouds.Mostcloudshavep/kbetween103cm-3Kand104cm-3K,butwefoundthatatleast6%oftheCI-bearingmaterialisatp/k>104cm-3K,andone-thirdofthegashasupperlimitsforpressurebelow103cm-3K.
ForT=80K,about40%ofalltheCIwesawhadf1andf2consistentwith3.4≤logp/k≤3.8.Roughlyone-thirdoftheCIhaddefiniteupperlimitsforpressurebelowthisrange,andAround6%ofthematerialhadlowerlimitsabovetheinterval.
Abstract:
Text:
ConclusionfromJenkins&Tripp(2011):60%oftheCIIisfoundbetween3.3≤logp/k≤3.8,29%isbelowlogp/k=3.3and11%isabovelogp/k=3.8.