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CH(A→X ) geislun

CH(A→X ) geislun. 02.04.2014 Ragnheiður Guðbrandsdóttir Ingólfur Magnússon. Tækjabúnaður. Ljómunarróf frá súrefnisríkum gasloga. CH(A→X ) rófið. CH(A→X) rófið kemur aðallega fram vegna v ′ = 0 →v′′ = 0 tilfærslu

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CH(A→X ) geislun

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  1. CH(A→X) geislun 02.04.2014 Ragnheiður Guðbrandsdóttir Ingólfur Magnússon

  2. Tækjabúnaður

  3. Ljómunarróf frá súrefnisríkum gasloga

  4. CH(A→X) rófið • CH(A→X) rófiðkemuraðallegaframvegna v′ = 0 →v′′ = 0 tilfærslu • (1,1) og(2,2) tilfærslurkomaeinnigframogsýnanokkuðeinfaldat, nærrisamhverftsnúningsmynstursemsvipartil IR rófs

  5. CH(A→X) rófið við 3000 K

  6. Hermun við CH(A→X) 2500 K

  7. Hermun CH(A→X) við 3000 K

  8. Frank Condon Stuðlar • Frank-Condon stuðlar gefa að færslur með Δv=±0 eru þær einu sem koma til greina • Yfir 900 meðan aðrir eru undir 10 • Boltzmanndreifing gefur að það eru mjög fáar sameindir með v>2 • Minna en 1% í öðrum

  9. Heildarróf

  10. Stækkun á okkar toppi

  11. B’= 17,06 B’’=17,07

  12. B’= 16,87 B’’= 16,92

  13. B’= 17,01 B’= 16,73 B’’= 17,06 B’’= 16,78 NIST: B’ = 14,457 B’’ = 14,932

  14. Takk fyrir • Spurningar

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