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Migration by solution in water (view source)
Revision as of 18:24, 10 June 2014
, 18:24, 10 June 2014→True solution
==True solution==
==True solution==
[[file:migration-of-petroleum_fig7-4.png|thumb|{{figure number|1}}After McAuliffe.<ref name=ch07r6>McAuliffe, C., D., 1980, [http://archives.datapages.com/data/specpubs/geochem1/data/a029/a029/0001/0050/0089.htm Oil and gas migration: chemical and physical constraints], in Roberts, W., H., Cordell, R., J., eds., AAPG Studies in Geology no. 10, p. 89–107.</ref>]]
[[file:migration-of-petroleum_fig7-4.png|300px|thumb|{{figure number|1}}The aqueous solubility of normal alkanes and aromatics at 25°C. After McAuliffe.<ref name=ch07r6>McAuliffe, C., D., 1980, [http://archives.datapages.com/data/specpubs/geochem1/data/a029/a029/0001/0050/0089.htm Oil and gas migration: chemical and physical constraints], in Roberts, W., H., Cordell, R., J., eds., AAPG Studies in Geology no. 10, p. 89–107.</ref>]]
True solution is a function of pressure, temperature, salinity, molecular weight, and mixtures of components present. The aqueous solubility of normal alkanes and aromatics at [[temperature::25°C]] is shown in [[:file:migration-of-petroleum_fig7-4.png|Figure 1]].
True solution is a function of pressure, temperature, salinity, molecular weight, and mixtures of components present. The aqueous solubility of normal alkanes and aromatics at [[temperature::25°C]] is shown in [[:file:migration-of-petroleum_fig7-4.png|Figure 1]].