Predicting the rates of photolysis of organic compounds in natural waters i
s limited by several factors. For direct photolysis of dilute solutions of
organic compounds in surface waters, the product of the quantum yield (effi
ciency) and light absorption rate are needed, but can rarely be calculated
from structure activity relations (SARs); direct kinetic constants can be e
stimated reliably using measured quantum yields and solar models or simple
spread sheet data bases to calculate rates as a function of latitude and se
ason. Indirect photoreaction constants can be calculated from measured or e
stimated rate constants and the average transient photooxidant concentratio
n. SARs for photooxidant rate constants are available for some classes of c
ompounds. The overall indirect photolysis rate for a specific compound is t
he sum of all significant oxidation reactions for the compound. Quantitatio
n of the rate process requires that a reaction profile be developed for eac
h compound.