Photochemistry can be dramatically different from ordinary chemistry
Photochemistry can be dramatically different from “ordinary” chemistry See example below
Cl Ar Cl
. Ar Cl Cl
Cl Ar Cl
+ Ar Cl Cl
Cl Ar Cl
Hvernig er efnafræði ósoneyðingarinnar? / Ozon depletion? O 3 Cl
Heildarloftstyrkur og ósonstyrkur yfir jörðu. / Concentration profiles for air and ozone in the Earth´s atmosphere.
20 km
Gleypni ósons á nær-útfjólubláa litrófssviðinu. Gleypnistuðull er í réttu hlutfalli við gleypni efnisins fyrir fastann efnisstyrk. Absorption cross section of ozone in the near UV spectral region.
20 km
20 km O 3 + O -> O 2+O 2
Chemistry and spectroscopy of the greenhouse effect/ Global warming effects(? )
Gegnskin og gleypni andrúmsloftsins ÚF SÝN . . IR. . . .
Gleypni O=C=O Bylgjulengd (mm)
Ultraviolet Visible Near-IR Infrared Far-Infrared Microwave
Organic photochemistry: photoisomerization
Stilben
Stilbene(2)
Astrochemistry
C 2 H 2 ? ? ? Big organic molecules : Life(? )
C 2 H 2 ? ? ? Big organic molecules : Life(? )
C 2 H 2 C CH 2 ? ? ? C 2 Big organic molecules : Life(? )
Ion yield LASER radiation of C 2 H 2+ Magn jóna C+ C 2+ H+ C 2 H + CH 2+ Mw Time of flight
Orka HCCH*: HCCH:
+ Orka C+2 HCCH*: C 2 H 2
Orka HCCH*:
Orka HCCH*: C CH 2
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