Laboratory experiments on three different source rock samples indicate
that pressure effects on generation kinetics are measurable but minor
. Pressure effects are quantified in terms of an activated volume whic
h is analogous to the use of activation energy to quantify temperature
effects. Although the three shales had slightly different activated v
olumes, a value of 27 cm3/mol is recommended as typical for the activa
ted volume of the transformation of kerogen to products. With this act
ivated volume, a 1380 bar pressure corresponds to about a 7-degrees-C
increase in generation temperature. Since generation commonly occurs a
t pressures less than 1380 bar, the effects of pressure on generation
timing appear minor and well within the range of uncertainty from othe
r causes.