Photochemistry can be dramatically different from “ordinary” chemistry See example below
Ar Cl
Ar Cl...
Ar
Cl Ar + -
Cl Ar
O3 O3O3 Cl Hvernig er efnafræði ósoneyðingar- innar?/ Ozon depletion?
( ) 20 km ( )
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 SÝNSÝN IR
Bylgjulengd ( m) Gleypni O=C=OO=C=O
UltravioletVisibleNear-IRInfraredFar-InfraredMicrowave
Organic photochemistry: photoisomerization
Stilben e(1)
Stilbene(2)
Astrochemistry
C2H2C2H2 Big organic molecules : Life(?) ???
C2H2C2H2 Big organic molecules : Life(?) ???
C2H2C2H2 Big organic molecules : Life(?) ??? C2C2 C CH 2
H+H+ CH + CH 2 + C+C+ C2+C2+ C2H+C2H+ C2H2+C2H2+ Magn jóna Ion yield LASER radiation of C 2 H 2 Mw Time of flight
Orka HCCH: HCCH*:
Orka C2C2 H2H2 HCCH*: C2C2 + +
Orka HCCH*:
Orka HCCH*: CH 2 C
A + M ??? M 1 + M 2 ??? A + B C + D Reaction cross section:
A + M ??? M 1 + M 2 ??? A + B C + D Cross section = = 2 d But ions: Reaction cross section:
A + + B C + D But ions: F 1/r 2 Reaction cross section:
+ A + + B C + D But Ions: Reaction cross section:
A + + B C + D But ions: ++ Collision frequency much larger Reaction cross section:
A + M ??? M 1 + M 2 ??? A + B C + D d + Ions: Collision cross section = >> 2 Reaction cross section: