Yuki Kimura Tohoku Univ. - - PowerPoint PPT Presentation

yuki kimura tohoku univ katsuo tsukamoto tohoku univ
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Yuki Kimura Tohoku Univ. - - PowerPoint PPT Presentation

Yuki Kimura Tohoku Univ. Katsuo Tsukamoto Tohoku Univ. Hitoshi Miura Tohoku Univ. Takao Maki Olympus Corp. (7 ) GFWS/ CPS


slide-1
SLIDE 1

均質核形成によるダスト生成実験と 古典的核形成論

Yuki Kimura Tohoku Univ. Katsuo Tsukamoto Tohoku Univ. Hitoshi Miura Tohoku Univ. Takao Maki Olympus Corp.

(77) GFWS/ 銀河のダスト研究会、神戸CPS、Sep. 2, 2010.

slide-2
SLIDE 2

Why nucleation?

  • Number
  • Morphology
  • Habit
  • Size
  • Size distribution

Not only industrially, Nucleation is also important to know the formation process of Cosmic dust particles.

We need understand Nucleation!

Evolved Star Planetary Nebula

均質核形成によるダスト生成実 験と古典的核形成論

slide-3
SLIDE 3

99% gas, but 1% solid

Building block of Planetary system & Life nm sized particles

AGB star Planetary Nebula SN Rem nant

Credit of all photos: NASA/ JPL/ Space Science Institute

Star Form ing Region Molecular Cloud Planetary System

slide-4
SLIDE 4

Nozaw a, et al., 2 0 0 9 .

惑星系 惑星系

500 nm 500 nm

惑星状星雲

200 nm 200 nm

500 nm 500 nm 500 nm Molster et al. 2002 100 nm

99% gas, but 1% solid

Building block of Planetary system & Life nm sized particles

slide-5
SLIDE 5

Condensation temperature of major elements as a function of C/ O ratio.

ガスの温度が下がるにつれて 高融点物質から順に凝縮する。

  • Cor. Corundum, コランダム, Al2O3
  • Per. Periclase, ペリクレイス, MgO
  • Gehl. Gehlenite, ゲーレナイト, Ca2Al(AlSi)O7
  • Sp. Spinel, スピネル, MgAl2O4
  • For. Forsterite, フォルステライト, (Fe,Mg) 2SiO4

Fe Iron, 鉄, Fe

C/ O abundance ratio Total gas pressure Gas outflow velocity Stellar mass loss rate Condensation sequence Sizes of core-mantle

Croat et al., 2004 LPS, 1353. Lodders et al. Meteoritics 30 (1995) 661.

Constraints on the formation conditions and environment have been calculated.

(Lodders & Fegley 1995; Sharp & Wasserburg 1995; Chigai et al. 1999, 2002)

slide-6
SLIDE 6

Smoke generator

Nickname is now wanted! Nickname is now wanted!

slide-7
SLIDE 7

Smoke generator + Interferometer

slide-8
SLIDE 8

Smoke generator + Interferometer

200 nm

100 nm 100 nm 50 nm

slide-9
SLIDE 9

He/ Ne laser 900 mm 600 mm camera mirror beam splitter

  • bjective lens, pinhole, collimate lens

polarizer lens mirror mirror IR filter dichroic mirror camera band-pass filter pyrometer ND filter ND filter

632.8 nm

slide-10
SLIDE 10

He/ Ne laser 900 mm 600 mm camera mirror beam splitter

  • bjective lens, pinhole, collimate lens

polarizer lens mirror mirror IR filter dichroic mirror camera band-pass filter pyrometer ND filter ND filter

632.8 nm

slide-11
SLIDE 11

He/ Ne laser 900 mm 600 mm camera mirror beam splitter

  • bjective lens, pinhole, collimate lens

polarizer lens mirror mirror IR filter dichroic mirror camera band-pass filter pyrometer ND filter ND filter

70.0 mm W wire 0.3 mm

632.8 nm

slide-12
SLIDE 12

Interferogram

Temperature: 298 K (25oC) Gas: Ar 1×104 Pa Refractive index: 1.00002714 3 mm Temperature: 323 K (50oC) Gas: Ar 1×104 Pa Refractive index: 1.00002503 Heating W wire 0.3 mm

Difference of refractive index is only 2 ×1 0 - 6.

slide-13
SLIDE 13

Interferogram

W wire 0.3 mm 3 mm 3 mm

We can detect only a difference of 10-6-10-7 orders!!

Temperature: 298 K (25oC) Gas: Ar 1×104 Pa Refractive index: 1.00002714 Temperature: 323 K (50oC) Gas: Ar 1×104 Pa Refractive index: 1.00002503 Heating Thermo couple 0.1 mmΦ

pyrometer thermocouple

slide-14
SLIDE 14

Interferogram

3 mm Temperature : 298 K (25oC) Gas : Ar 9×103 Pa, O2 1×103 Pa Refractive index: 1.00002703 3 mm

Oxygen

Heating RT 1570 K Temperature: 298 K (25oC) Gas: Ar 1×104 Pa Refractive index: 1.00002714 Only Temperature Temperature & concentration

Temperature information is subtracted by oxygen free experiment.

slide-15
SLIDE 15

In-situ observation using interferometer

A tungsten wire (0.3 mm and 70 mm depth) is heated in a mixture gas

  • f Ar (9×103 Pa) and O2 (1×103 Pa).

1st, 2nd and 3rd fringes correspond to 320, 500 and 1150 K, respectively. 5 mm

  • 5
slide-16
SLIDE 16

In-situ observation using interferometer

870 K 1570 K 1150 K 500 K  WO3 particles are condensed 700 K lower than equilibrium T due to homogeneous nucleation!  Nucleation occurs below

the evaporation source.

 Degree of supersaturation is at least 1011!!

Evaporation Source Pe= 1.3×103 Pa at 1570 K Position of Smoke Pe= ~ 10-9 Pa at 870 K

slide-17
SLIDE 17

Convection current and Smoke

WO3 vapor Diffusion velocity: 95 cm s-1 Convection current

Flow velocity (cm s-1) 150 100 50 1.3 Gas pressure (103 Pa) 6.5 13 26 39

He gas T= 1873 K

Yatsuya et al. J. Cry. Growth 70 (1984) 536.

104 Pa  The heated source generated a high- temperature atmosphere and convection currents (~ 100 cm s-1).  Evaporated WO3 vapor diffuses in uniformly with 9.79 cm 2 s-1.

1570 K ~ 100 cm s-1

slide-18
SLIDE 18

Convection current and Smoke

WO3 vapor Diffusion velocity: 95 cm s-1 Convection current of ambient gas: ~ 100 cm s-1

 Since there is a strong convection current, rising vapor is accelerated and down flow is restrained.  As the result, concentration of WO3 vapor is getting higher below the evaporation source.

slide-19
SLIDE 19

Convection current and Smoke

WO3 vapor Diffusion velocity: 95 cm s-1 Convection current of ambient gas: ~ 100 cm s-1

 Finally, nucleation occurs at the highest supersaturation environment between convection current of ambient gas and evaporated WO3 vapor.  Nuclei follow the convection current and grow to make nanoparticles in smoke.

slide-20
SLIDE 20

Convection current and Smoke

WO3 vapor Diffusion velocity: 95 cm s-1 Convection current of ambient gas: ~ 100 cm s-1

 Finally, nucleation occurs at the highest supersaturation environment between convection current of ambient gas and evaporated WO3 vapor.  Nuclei follow the convection current and grow to make nanoparticles in smoke.  W e can derive a lot of inform ation from I nterferogram .

slide-21
SLIDE 21

Condensation temperature of major elements as a function of C/ O ratio.

ガスの温度が下がるにつれて 高融点物質から順に凝縮する。

  • Cor. Corundum, コランダム, Al2O3
  • Per. Periclase, ペリクレイス, MgO
  • Gehl. Gehlenite, ゲーレナイト, Ca2Al(AlSi)O7
  • Sp. Spinel, スピネル, MgAl2O4
  • For. Forsterite, フォルステライト, (Fe,Mg) 2SiO4

Fe Iron, 鉄, Fe

C/ O abundance ratio Total gas pressure Gas outflow velocity Stellar mass loss rate Condensation sequence Sizes of core-mantle

Croat et al., 2004 LPS, 1353. Lodders et al. Meteoritics 30 (1995) 661.

Constraints on the formation conditions and environment have been calculated.

(Lodders & Fegley 1995; Sharp & Wasserburg 1995; Chigai et al. 1999, 2002)

slide-22
SLIDE 22

Conclusion

 Temperature and concentration can be measured in-situ during smoke experiment.  Condensation occurs under very high supercooling (T= ~ 400-700K).  Nucleation takes place below evaporation source in smoke experiment.  Nucleation theory may be verified.