Evaluation of the Potential for Dissolved Oxygen Ingress into Deep Sedimentary Basins during a Glaciation Event

Table 1

Geochemical reactions considered in the illustrative sedimentary basin example.

		Ref.
Homogeneous reactions
Cation-exchange reactions
Dissolution/precipitation reactions	Enthalpy; kcal mol^−1

Equilibrium constant taken from Wolery and Daveler [17]. Selectivity coefficients taken Appelo and Postma [18]. Not controlled by equilibrium [2].